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According to popular legend, ice cream was invented by the ancient Chinese, brought to Italy by Marco Polo, to France by Catherine de Medici, and thence to America by Thomas Jefferson. The truth, however, about summer’s favorite chilled dairy treat is a bit more difficult to pin down. Iced drinks and desserts have been around since at least 4000 B.C., when nobles along the Euphrates River built icehouses to take the edge off the Mesopotamian summer heat. Snow, likely used to cool wine, was sold in the streets of Athens in the fifth century B.C., while the Roman emperor Nero (37–67 A.D.) enjoyed iced refreshments laced with honey. Sources from the Tang dynasty in China describe a sweet drink made from iced, camphor-laced water buffalo milk.
Chilled refreshments were also popular in the Islamic world. The English word sherbet comes from the Turkish term for a broad category of sweetened drinks, often cooled with snow from storehouses. Faloodeh, a Persian treat of vermicelli noodles in chilled syrup, dates back centuries. In India, Mughal emperors savored kulfi, a quasi-ice cream made from condensed milk frozen in molds.
Indeed, the first verified records of kulfi are nearly contemporary with the earliest evidence of frozen sherbets and ice creams in Europe. In both cases what made this breakthrough possible was the knowledge (familiar to many in the Arab world since the 13th century) that ice mixed with salt set in motion an exothermic chemical reaction, which created a heat-sucking slurry with a far lower freezing point than typical water. Immersed in a bath of exothermic brine, ice crystals easily formed in various liquid concoctions. Stirred regularly to prevent large ice crystals from forming, a scoop-able frozen foam resulted.
READ MORE: Frozen History: The Story of the Popsicle
The first European ice creams and water ices (sherbets) were likely made in Italy during the early 1600s (a century after a teenaged Catherine de Medici departed Florence to become queen of France). Descriptions of water ice desserts date to the 1620s, and by midcentury they were a feature of banquets in Paris, Florence, Naples and Spain. In 1672 Englishman Elias Ashmole recorded that “one plate of ice cream” had been served to King Charles II at a banquet the previous year. In 1694 Antonio Latini, a Neapolitan steward, published a recipe for a milk sorbet laced with candied pumpkin.
Ice cream crossed the Atlantic with the European colonists, and was served by first lady of colonial Maryland as early as 1744. George Washington bought a mechanical ice cream maker for his estate at Mount Vernon in 1784, the same year Thomas Jefferson likely acquired a taste for French ice cream while serving as a diplomat in Paris. While president, Jefferson served ice cream in the executive mansion at least six times. In a lifetime of copious notes and writings, Jefferson only wrote out ten recipes, one of which was for French-style vanilla ice cream, fortified with egg yolks.
By the late-19th century, America was a hotbed of ice cream innovation. A Philadelphia pharmacist mixed the first ice cream soda in 1874. The ice cream sundae dates to 1881 (with several Midwestern towns claiming to be the site of its invention)—its name likely coming from “blue laws” that banned sale of soda drinks on Sundays. The first edible ice cream cups were patented in the 1880s, around the time that milkshakes—originally promoted as a health drink—became popular. The waffle cone rocketed to fame when introduced at the 1904 St. Louis World’s Fair, and the Popsicle was patented in 1923. Both Dairy Queen and the Carvel company claim to have developed the first soft-serve ice cream in the mid-1930s, while frozen yogurt was a latecomer, introduced in the 1970s.
Today ice cream and its frigid cousins are known and loved worldwide, even imported to Antarctica, where a Frosty Boy soft-serve machine is a famous focal point for the scientists who work at McMurdo Station.
READ MORE: Why Ice Cream Soared in Popularity During Prohibition
Learn The History & Science Of Your Fave Summer Snack With These Books
Does anything say summertime quite like a couple cold creamy scoops of ice cream and a stack of absorbing beach reads? I didn't think so, either, which is why I've rounded up some of the most delicious nonfiction books about ice cream. Fun and fascinating, they're perfect for pairing with a waffle cone of your favorite flavor.
It's no secret that Americans love their fair share of frozen desserts. In fact, the average American consumes 23 pounds of ice cream in any given year. Most of those sweet, delicious scoop up during the summer months, ice cream's undisputed season of enjoyment. After a long, hot day on the beach, by the pool, at the park, or, more likely, at work, who doesn't enjoy a double dish of cookie dough ice cream?
America's favorite dessert, ice cream has a long and interesting history in the United States, and around the world. With origins reaching as far back as the second B.C., ice cream has been delighting eaters for two thousand years, and in that time, it has changed and evolved alongside culture, science, and technology. In fact, the only thing sweeter than eating ice cream is learning how it came to be.
Ready to satisfy your cravings? Then here are nine books about ice cream that will hit the spot this summer.
Ice Cream for America
The first official account of ice cream in the New World comes from a letter written in 1744 by a guest of Maryland Governor William Bladen. The first advertisement for ice cream in this country appeared in the New York Gazette on May 12, 1777, when confectioner Philip Lenzi announced that ice cream was available "almost every day." Records kept by a Chatham Street, New York, merchant show that President George Washington spent approximately $200 for ice cream during the summer of 1790. Inventory records of Mount Vernon taken after Washington's death revealed "two pewter ice cream pots." President Thomas Jefferson was said to have a favorite 18-step recipe for an ice cream delicacy that resembled a modern-day Baked Alaska. Check out President Jefferson's vanilla ice cream recipe here. In 1813, Dolley Madison served a magnificent strawberry ice cream creation at President Madison's second inaugural banquet at the White House.
Until 1800, ice cream remained a rare and exotic dessert enjoyed mostly by the elite. Around 1800, insulated ice houses were invented. Manufacturing ice cream soon became an industry in America, pioneered in 1851 by a Baltimore milk dealer named Jacob Fussell. Like other American industries, ice cream production increased because of technological innovations, including steam power, mechanical refrigeration, the homogenizer, electric power and motors, packing machines, and new freezing processes and equipment. In addition, motorized delivery vehicles dramatically changed the industry. Due to ongoing technological advances, today's total frozen dairy annual production in the United States is more than 1.6 billion gallons.
Wide availability of ice cream in the late 19th century led to new creations. In 1874, the American soda fountain shop and the profession of the "soda jerk" emerged with the invention of the ice cream soda. In response to religious criticism for eating "sinfully" rich ice cream sodas on Sundays, ice cream merchants left out the carbonated water and invented the ice cream "Sunday" in the late 1890's. The name was eventually changed to "sundae" to remove any connection with the Sabbath.
Ice cream became an edible morale symbol during World War II. Each branch of the military tried to outdo the others in serving ice cream to its troops. In 1945, the first "floating ice cream parlor" was built for sailors in the western Pacific. When the war ended, and dairy product rationing was lifted, America celebrated its victory with ice cream. Americans consumed over 20 quarts of ice cream per person in 1946.
In the 1940s through the ‘70s, ice cream production was relatively constant in the United States. As more prepackaged ice cream was sold through supermarkets, traditional ice cream parlors and soda fountains started to disappear. Now, specialty ice cream stores and unique restaurants that feature ice cream dishes have surged in popularity. These stores and restaurants are popular with those who remember the ice cream shops and soda fountains of days past, as well as with new generations of ice cream fans.
Dataset 2 Today’s Antarctic Sea Ice Report
The white area surrounding Antarctica shows how much of the ocean is currently covered by sea ice. The ice naturally grows and shrinks every winter and summer (September has the most ice February, the least.)
The orange line shows the normal (median) ice coverage for that day, based on measurements from 1981–2010.
Based on microwave data gathered via satellite, this image shows the extent of the Southern Ocean around Antarctica that’s currently covered by ice at greater than 15% concentration. Source: National Snow and Ice Data Center, University of Colorado Boulder
The Opposite of Melting
In spite of climate change, Antarctic sea ice has been growing by about 1.8% per decade. Scientists aren’t sure why, but they think it may be caused by the frigid ocean current that surrounds Antarctica, and by the continent’s icy winds.
Sea Ice Growing, Land Ice Shrinking
Though Antarctic sea ice is growing, the ice sheets on the continent itself are shrinking—by an estimated 219 billion metric tons per year, as of 2018. This melting appears to be accelerating, and is contributing to sea level rise.
The Antarctic ice sheet has lost more than 1,000 gigatonnes of ice since 2002, according to ice mass measurements from NASA’s GRACE satellites.
Dataset A Frozen History of the Climate
Snow in Summer: A Global History of Frozen Treats - HISTORY
May 31, 2020
For nearly two centuries, homemade frozen treats served with a smile on the streets of America have remained one of our nation’s seasonal treasures. It all started in the early 1800s, when immigrant street vendors in New York began peddling home-country, family-recipe ice cream to the city’s sweltering urban masses. As sweet-tooth journalist Laura B. Weiss notes in her book Ice Cream: A Global History, “Italy and France was where ice cream was first truly developed and made delicious—in the U.S., they developed the business.”
Fresh out of Ellis Island, carrying little luggage and even fewer career skills, scores of eager European upstarts combined their culinary passions, national pride and business instincts to design unique ice cream parlors on wheels. Crafting cheap, hand-built wooden wagons to serve from allowed them to support their own families by sharing desserts perfected by their ancestors, a sales model that established a stellar profit margin by avoiding the steep rent and tax costs incurred by New York’s stationary ice cream parlors.
As word of these cool carts spread like wildfire throughout the city’s poor downtown areas, a win-win situation emerged for both the pushcart operators and Manhattan’s disenfranchised masses. Being that the vendors lived on the same minimum income level as most New Yorkers, they priced their ice cream accordingly, giving many a chance to enjoy treats that at the time were more commonly enjoyed by those with cleaner clothes. While storefront ice-cream rooms did remain open, many encountered large dips in their sales. Some even sought out street vendor recipes to win back customers who had fled to the streets.
Among the most popular frozen treats sold by street vendors was a Neapolitan-style snack nicknamed a “hokey-pokey”. A thick blend of condensed milk, sugar, vanilla, gelatin and cornstarch, hokey-pokeys were sliced into cubes and served wrapped in wax paper. Repeat visitors and kids of all nationalities, including those of Italian, Irish and Jewish backgrounds, gathered together along the Bowery, early New York’s avenue of the people, listening intently for the vendors’ familiar yell, the original ice cream truck melody—”Hokey-pokey, sweet and cold for a penny, new or old!”
Another frozen favorite of Manhattan’s labor class and their children was a “Penny Lick”, called such because of its cost and method of consumption. At the time, the ice cream cone had yet to be created, so vendors served their ice cream in standard glasses, which customers would lick down to the last drop before returning to the cart. To satisfy the next sweet tooth in line, the vendor would dunk a returned glass in a water bucket, scoop, serve, and start the process all over again. Some fatherly vendors were even known to let the neighborhood’s most troubled children keep their own glass and save their pennies, in exchange for spreading word about their carts.
As the modern descendants of early New York’s scrappy mobile dessert peddlers, Carousel’s Soft Serve Icery is filled with pride to be part of such an innovative, family-oriented American lineage of homemade, curbside refreshment, served fresh to people of all ages. We believe we share our brand character stalwarts—Happiness, Charity, Honesty, Togetherness and Love—with the vendors who worked their rickety carts down Old New York’s packed cobbled streets, and through programs like Carousel’s Cares, we dedicate our assets and energies to advancing the spirit of charity many of our dessert forefathers displayed.
But while our hearts are similar, Carousel’s distribution methods are just a bit more advanced than those of our mobile sweets predecessors—they’re even a few steps ahead of most of our modern dessert truck colleagues! Just like our soft serve ices, our iconic trucks are a remix of prized tradition and pure imagination, carefully designed to make your dessert experience even more immersive and refreshing. From the environment our truck puts forth, to our frozen ice dispersal methods, to the flavor and texture of our ice itself, Carousel’s has always kept it classic while changing the game.
Just like our namesake attraction at the center of an amusement park, you can’t miss a Carousel’s Soft Serve Icery truck. We’re one-of-a-kind, from our colors to our music, and from our sights to our smells—yes, our smells! Carousel’s practices “scent marketing”, an innovative method of drawing passersby towards our truck using a mechanism that emits an all-natural, mouthwatering aroma from the perimeter of the vehicle. It’s sure to awaken the taste buds, and if it draws you in we’ll help you get started—Old New York’s miniature “Hokey-Pokeys” cost a penny, but our bite-sized samples are on the house.
Equally as distinctive are our ice’s trademark texture and taste. You won’t find another flavored ice like this, literally—Carousel’s soft-serve ice machine is a special, custom proprietary model that produces a tidal wave swirl of smooth fruity flavor. Our ices never end up watery and bland, a common problem for dessert trucks whose premade ice has spent all day riding around town. Our custom machines also ensure Carousel’s frozen ices are always creamy and even-textured, never crunchy or freezer-burned. And if all that rich taste and smooth consistency isn’t enough, our soft serve ices have none of the fat, calories, gluten or dairy of other similar frozen treats, and are vegan as well. Feeling ready for Summer yet?
Interested in franchising information? Contact us here!
Be it soft-serve, gelato, frozen custard, Indian kulfi or Israeli glida, some form of cold, sweet ice cream treat can found throughout the world in restaurants and home freezers. Though ice cream was once considered a food for the elite, it has evolved into one of the most successful mass-market products ever developed.
In Ice Cream, food writer Laura B. Weiss takes the reader on a vibrant trip through the history of ice cream from ancient China to modern-day Tokyo in order to tell the lively story of how this delicious indulgence became a global sensation. Weiss tells of donkeys wooed with ice cream cones, Good Humor-loving World War II-era German diplomats, and sundaes with names such as “Over the Top” and “George Washington.” Her account is populated with Chinese emperors, English kings, former slaves, women inventors, shrewd entrepreneurs, Italian immigrant hokey-pokey ice cream vendors, and gourmand American First Ladies. Today American brands dominate the world ice cream market, but vibrant dessert cultures like Italy’s continue to thrive, and new ones, like Japan’s, flourish through unique variations.
Weiss connects this much-loved food with its place in history, making this a book sure to be enjoyed by all who are beckoned by the siren song of the ice cream truck.
Introduction: Everyone Loves Ice Cream
1. The Early Ice Cream Age
2. Confectioners and Colonists
3. Ice Cream for the Masses
4. Ice Cream’s Golden Age
5. Cones and Novel Ice Cream Treats
6. Ice Cream Goes Mass Market
7. The New Ice Cream Age
Websites and Associations
&ldquoIce Cream: A Global History is the place to turn if you want to know the backstory of everyone&rsquos favorite frozen treat!&rdquo
&ldquoIce Cream: A Global History . . . look[s] back at ice cream&rsquos enduring appeal to people around the globe&mdashfrom George Washington’s ice cream cravings to today’s upwardly mobile Chinese&mdashand celebrates the enormous popularity of a beloved treat that never goes out of style. It&rsquos a MUST read this summer . . . with ice-cream in-hand of course! :)&rdquo
&ldquoThe subject is captivating enough to keep the interest of students of cultural history as well as ice cream fanatics or foodie historians.&rdquo
&ldquoWe are quite taken with the short but engagingly readable Edibles series of handsome little books on basic, well, edibles, as in the cultural and global history of one type of food or beverage. Originating in England from Reaktion Books but written by foodie journalists or food science academics on both sides of the Atlantic, these spritely, much-illustrated books are a peruser&rsquos delight.&rdquo
&ldquoA fun, smartly written series appropriate for a popular audience that likes to eat . . . the Edible series books provide level-headed and enjoyable overviews of food culture . . . These will create a little library that any foodie will be proud to show off . . . aesthetically pleasing volumes with decent content that would make good presents.&rdquo
&ldquoLaura Weiss paints a compelling portrait of everyone s favorite dessert. She traces the transition of ice cream from a luxury reserved for the wealthy to an everyday treat accessible to the masses, while never allowing history to obscure a sense of pure pleasure.&rdquo
&ldquoAn informative and lighthearted book about ice cream of all varieties. The book is slender to the hand, but packed with history, facts, and stories.&rdquo
After this deep freeze, there were several “hothouse earth” periods when the temperature exceeded those we experience today. The warmest was probably the Paleocene-Eocene Thermal Maximum (PETM), which peaked about 55 million years ago. Global temperatures during this event may have warmed by 5°C to 8°C within a few thousand years, with the Arctic Ocean reaching a subtropical 23°C. Mass extinctions resulted.
The warming, which lasted 200,000 years, was caused by the release of massive amounts of methane or CO2. It was thought to have come from the thawing of methane clathrates in deep ocean sediments, but the latest theory is that it was caused by a massive volcanic eruption that heated up coal deposits. In other words, the PETM is an example of catastrophic global warming triggered by the build-up of greenhouse gases in the atmosphere.
Since then, the Earth has cooled. For the past million years or so, the climate has switched between ice ages and warmer interglacial periods with temperatures similar to those of the past few millennia. These periodic changes seem to be triggered by oscillations in the planet’s orbit and inclination that alter the amount of solar radiation reaching Earth.
However, it is clear that the orbital changes alone would not have produced large temperature changes and that there must have been some kind of feedback effect (see the section on Milankovitch cycles in this article).
Heavy snow fell in northern New England on June 7-8, with 18- to 20-inch high drifts. In Philadelphia, the ice was so bad "every green herb was killed and vegetables of every description very much injured," according to the book American Weather Stories.
Frozen birds dropped dead in the streets of Montreal, and lambs died from exposure in Vermont, the New England Historical Society said.
On July 4, one observer wrote that "several men were pitching quoits (a game) in the middle of the day with heavy overcoats on." A frost in Maine that month killed beans, cucumbers and squash, according to meteorologist Keith Heidorn. Ice covered lakes and rivers as far south as Pennsylvania, according to the Weather Underground.
By the time August rolled around, more severe frosts further damaged or killed crops in New England. People reportedly ate raccoons and pigeons for food, the New England Historical Society said.
Europe also suffered mightily: the cold and wet summer led to famine, food riots, the transformation of stable communities into wandering beggars and one of the worst typhus epidemics in history, according to The Year without Summer.
Scientists’ best estimate is that the global-average temperature cooled by almost 2 degrees in 1816 said Nicholas Klingaman, who is also a meteorologist at the University of Reading in the United Kingdom. Land temperatures cooled by about 3 degrees, he added.
Evidence from mountain glaciers does suggest increased glaciation in a number of widely spread regions outside Europe prior to the twentieth century, including Alaska, New Zealand and Patagonia. However, the timing of maximum glacial advances in these regions differs considerably, suggesting that they may represent largely independent regional climate changes, not a globally-synchronous increased glaciation. Thus current evidence does not support globally synchronous periods of anomalous cold or warmth over this interval, and the conventional terms of "Little Ice Age" and "Medieval Warm Period" appear to have limited utility in describing trends in hemispheric or global mean temperature changes in past centuries. [Viewed] hemispherically, the "Little Ice Age" can only be considered as a modest cooling of the Northern Hemisphere during this period of less than 1°C relative to late twentieth century levels. 
The IPCC Fourth Assessment Report (AR4) of 2007 discusses more recent research, giving particular attention to the Medieval Warm Period:
. when viewed together, the currently available reconstructions indicate generally greater variability in centennial time scale trends over the last 1 kyr than was apparent in the TAR. The result is a picture of relatively cool conditions in the seventeenth and early nineteenth centuries and warmth in the eleventh and early fifteenth centuries, but the warmest conditions are apparent in the twentieth century. Given that the confidence levels surrounding all of the reconstructions are wide, virtually all reconstructions are effectively encompassed within the uncertainty previously indicated in the TAR. The major differences between the various proxy reconstructions relate to the magnitude of past cool excursions, principally during the twelfth to fourteenth, seventeenth and nineteenth centuries. 
There is no consensus regarding the time when the Little Ice Age began,   but a series of events before the known climatic minima has often been referenced. In the 13th century, pack ice began advancing southwards in the North Atlantic, as did glaciers in Greenland. Anecdotal evidence suggests expanding glaciers almost worldwide. Based on radiocarbon dating of roughly 150 samples of dead plant material with roots intact, collected from beneath ice caps on Baffin Island and Iceland, Miller et al. (2012)  state that cold summers and ice growth began abruptly between 1275 and 1300, followed by "a substantial intensification" from 1430 to 1455. 
In contrast, a climate reconstruction based on glacial length   shows no great variation from 1600 to 1850 but strong retreat thereafter.
Therefore, any of several dates ranging over 400 years may indicate the beginning of the Little Ice Age:
- 1250 for when Atlanticpack ice began to grow cold period possibly triggered or enhanced by the massive eruption of Samalas volcano in 1257 
- 1275 to 1300 based on the radiocarbon dating of plants killed by glaciation
- 1300 for when warm summers stopped being dependable in Northern Europe
- 1315 for the rains and Great Famine of 1315–1317
- 1560 to 1630 for beginning of worldwide glacial expansion known as the Grindelwald Fluctuation 
- 1650 for the first climatic minimum.
The Little Ice Age ended in the latter half of the 19th century or early in the 20th century.   
The Baltic Sea froze over twice, 1303 and 1306–07 years followed of "unseasonable cold, storms and rains, and a rise in the level of the Caspian Sea.”  The Little Ice Age brought colder winters to parts of Europe and North America. Farms and villages in the Swiss Alps were destroyed by encroaching glaciers during the mid-17th century.  Canals and rivers in Great Britain and the Netherlands were frequently frozen deeply enough to support ice skating and winter festivals.  The first River Thames frost fair was in 1608 and the last in 1814 changes to the bridges and the addition of the Thames Embankment affected the river flow and depth, greatly diminishing the possibility of further freezes.  In 1658, a Swedish army marched across the Great Belt to Denmark to attack Copenhagen. The winter of 1794–1795 was particularly harsh: the French invasion army under Pichegru was able to march on the frozen rivers of the Netherlands, and the Dutch fleet was locked in the ice in Den Helder harbour.
Sea ice surrounding Iceland extended for miles in every direction, closing harbors to shipping. The population of Iceland fell by half, but that may have been caused by skeletal fluorosis after the eruption of Laki in 1783.  Iceland also suffered failures of cereal crops and people moved away from a grain-based diet.  The Norse colonies in Greenland starved and vanished by the early 15th century, as crops failed and livestock could not be maintained through increasingly harsh winters. Greenland was largely cut off by ice from 1410 to the 1720s. 
In his 1995 book the early climatologist Hubert Lamb said that in many years, "snowfall was much heavier than recorded before or since, and the snow lay on the ground for many months longer than it does today."  In Lisbon, Portugal, snowstorms were much more frequent than today one winter in the 17th century produced eight snowstorms.  Many springs and summers were cold and wet but with great variability between years and groups of years. This was particularly evident during the 'Grindelwald Fluctuation' (1560-1630): a rapid cooling phase that was associated with more erratic weather - including increased storminess, unseasonal snow storms and droughts.  Crop practices throughout Europe had to be altered to adapt to the shortened, less reliable growing season, and there were many years of dearth and famine (such as the Great Famine of 1315–1317, but that may have been before the Little Ice Age).  According to Elizabeth Ewan and Janay Nugent, "Famines in France 1693–94, Norway 1695–96 and Sweden 1696–97 claimed roughly 10 percent of the population of each country. In Estonia and Finland in 1696–97, losses have been estimated at a fifth and a third of the national populations, respectively."  Viticulture disappeared from some northern regions and storms caused serious flooding and loss of life. Some of them resulted in permanent loss of large areas of land from the Danish, German, and Dutch coasts. 
The violin maker Antonio Stradivari produced his instruments during the Little Ice Age. The colder climate is proposed to have caused the wood used in his violins to be denser than in warmer periods, contributing to the tone of his instruments.  According to the science historian James Burke, the period inspired such novelties in everyday life as the widespread use of buttons and button-holes, and knitting of custom-made undergarments to better cover and insulate the body. Chimneys were invented to replace open fires in the centre of communal halls, so allowing houses with multiple rooms, separation of masters from servants. 
The Little Ice Age, by anthropologist Brian Fagan of the University of California at Santa Barbara, tells of the plight of European peasants during the 1300 to 1850 chill: famines, hypothermia, bread riots and the rise of despotic leaders brutalizing an increasingly dispirited peasantry. In the late 17th century, agriculture had dropped off dramatically: "Alpine villagers lived on bread made from ground nutshells mixed with barley and oat flour."  Historian Wolfgang Behringer has linked intensive witch-hunting episodes in Europe to agricultural failures during the Little Ice Age. 
The Frigid Golden Age, by environmental historian Dagomar Degroot of Georgetown University, by contrast, reveals that some societies thrived while others faltered during the Little Ice Age. In particular, the Little Ice Age transformed environments around the Dutch Republic — the precursor to the present-day Netherlands — so that they were easier to exploit in commerce and conflict. The Dutch were resilient, even adaptive, in the face of weather that devastated neighboring countries. Merchants exploited harvest failures, military commanders took advantage of shifting wind patterns, and inventors developed technologies that helped them profit from the cold. The 17th-century "Golden Age" of the Republic therefore owed much to the flexibility of the Dutch in coping with a changing climate. 
Cultural responses Edit
Historians have argued that cultural responses to the consequences of the Little Ice Age in Europe consisted of violent scapegoating.      The prolonged cold, dry periods brought drought upon many European communities, resulting in poor crop growth, poor livestock survival, and increased activity of pathogens and disease vectors.  Disease tends to intensify under the same conditions that unemployment and economic difficulties arise: prolonged, cold, dry seasons. Both of these outcomes – disease and unemployment – enhance each other, generating a lethal positive feedback loop.  Although these communities had some contingency plans, such as better crop mixes, emergency grain stocks, and international food trade, these did not always prove effective.  Communities often lashed out via violent crimes, including robbery and murder sexual offense accusations increased as well, such as adultery, bestiality, and rape.  Europeans sought explanations for the famine, disease, and social unrest that they were experiencing, and blamed the innocent. Evidence from several studies indicate that increases in violent actions against marginalized groups that were held responsible for the Little Ice Age overlap with years of particularly cold, dry weather.   
One example of the violent scapegoating occurring during the Little Ice Age was the resurgence of witchcraft trials, as argued by Oster (2004) and Behringer (1999). Oster and Behringer argue that this resurgence was brought upon by the climatic decline. Prior to the Little Ice Age, "witchcraft" was considered an insignificant crime and victims were rarely accused.  But beginning in the 1380s, just as the Little Ice Age began, European populations began to link magic and weather-making.  The first systematic witch hunts began in the 1430s, and by the 1480s it was widely believed that witches should be held accountable for poor weather.  Witches were blamed for direct and indirect consequences of the Little Ice Age: livestock epidemics, cows that gave too little milk, late frosts, and unknown diseases.  In general, as the temperature dropped, the number of witchcraft trials rose, and trials decreased when temperature increased.   The peaks of witchcraft persecutions overlap with hunger crises that occurred in 1570 and 1580, the latter lasting a decade.  These trials primarily targeted poor women, many of whom were widows. Not everybody agreed that witches should be persecuted for weather-making, but such arguments primarily focused not upon whether witches existed, but upon whether witches had the capability to control the weather.   The Catholic Church in the Early Middle Ages argued that witches could not control the weather because they were mortals, not God, but by the mid-13th-century most populations agreed with the idea that witches could control natural forces. 
Historians have argued that Jewish populations were also blamed for climatic deterioration during the Little Ice Age.   Christianity was the official religion of Western Europe, and within these populations there was a great degree of anti-Semitism.  There was no direct link made between Jews and weather conditions, they were only blamed for indirect consequences such as disease.  For example, outbreaks of the plague were often blamed on Jews in Western European cities during the 1300s Jewish populations were murdered in an attempt to stop the spread of the plague.  Rumors were spread that either Jews were poisoning wells themselves, or conspiring against Christians by telling those with leprosy to poison the wells.  As a response to such violent scapegoating, Jewish communities sometimes converted to Christianity or migrated to the Ottoman Empire, Italy, or to territories of the Holy Roman Empire. 
Some populations blamed the cold periods and the resulting famine and disease during the Little Ice Age on general divine displeasure.  Particular groups, however, took the brunt of the burden in attempts to cure it.  For example, in Germany, regulations were imposed upon activities such as gambling and drinking, which disproportionately affected the lower class, and women were forbidden from showing their knees.  Other regulations affected the wider population, such as prohibiting dancing and sexual activities, as well as moderating food and drink intake. 
In Ireland, Catholics blamed the Reformation for the bad weather. The Annals of Loch Cé, in its entry for the year 1588, describes a midsummer snowstorm: "a wild apple was not larger than each stone of it," blaming it on the presence of a "wicked, heretical, bishop in Oilfinn" that is, the Protestant Bishop of Elphin, John Lynch.  
Depictions of winter in European painting Edit
William James Burroughs analyses the depiction of winter in paintings, as does Hans Neuberger.  Burroughs asserts that it occurred almost entirely from 1565 to 1665 and was associated with the climatic decline from 1550 onwards. Burroughs claims that there had been almost no depictions of winter in art, and he "hypothesizes that the unusually harsh winter of 1565 inspired great artists to depict highly original images and that the decline in such paintings was a combination of the 'theme' having been fully explored and mild winters interrupting the flow of painting".  Wintry scenes, which entail technical difficulties in painting, have been regularly and well handled since the early 15th century by artists in illuminated manuscript cycles showing the Labours of the Months, typically placed on the calendar pages of books of hours. January and February are typically shown as snowy, as in February in the famous cycle in the Les Très Riches Heures du duc de Berry, painted 1412–1416 and illustrated below. Since landscape painting had not yet developed as an independent genre in art, the absence of other winter scenes is not remarkable. On the other hand, snowy winter landscapes and stormy seascapes in particular became artistic genres in the Dutch Republic during the coldest and stormiest decades of the Little Ice Age. At the time when the Little Ice Age was at its height, Dutch observations and reconstructions of similar weather in the past caused artists to consciously paint local manifestations of a cooler, stormier climate. This was a break from European conventions as Dutch paintings and realistic landscapes depicted scenes from everyday life, which most modern scholars believe that were full of symbolic messages and metaphors that would have been clear to contemporary customers. 
The famous winter landscape paintings by Pieter Brueghel the Elder, such as The Hunters in the Snow, are all thought to have been painted in 1565. His son Pieter Brueghel the Younger (1564–1638) also painted many snowy landscapes, but according to Burroughs, he "slavishly copied his father's designs. The derivative nature of so much of this work makes it difficult to draw any definite conclusions about the influence of the winters between 1570 and 1600. ".  
Burroughs says that snowy subjects return to Dutch Golden Age painting with works by Hendrick Avercamp from 1609 onwards. There is then a hiatus between 1627 and 1640, before the main period of such subjects from the 1640s to the 1660s, which relates well with climate records for the later period. The subjects are less popular after about 1660, but that does not match any recorded reduction in severity of winters and may reflect only changes in taste or fashion. In the later period between the 1780s and 1810s, snowy subjects again became popular. 
Neuberger analysed 12,000 paintings, held in American and European museums and dated between 1400 and 1967, for cloudiness and darkness.  His 1970 publication shows an increase in such depictions that corresponds to the Little Ice Age,  peaking between 1600 and 1649. 
Paintings and contemporary records in Scotland demonstrate that curling and ice skating were popular outdoor winter sports, with curling dating back to the 16th century and becoming widely popular in the mid-19th century.  As an example, an outdoor curling pond constructed in Gourock in the 1860s remained in use for almost a century, but increasing use of indoor facilities, problems of vandalism, and milder winters led to the pond being abandoned in 1963. 
General Crisis of the Seventeenth Century Edit
The General Crisis of the Seventeenth Century in Europe was a period of inclement weather, crop failure, economic hardship, extreme inter-group violence, and high mortality causally linked to the Little Ice Age. Episodes of social instability track the cooling with a time lapse of up to 15 years, and many developed into armed conflicts, such as the Thirty Years' War (1618–1648).  It started as a war of succession to the Bohemian throne. Animosity between Protestants and Catholics in the Holy Roman Empire (Germany today) added fuel to the fire. Soon, it escalated to a huge conflict involving all major European powers that devastated much of Germany. By the war's end, some regions of the Holy Roman Empire saw their population drop by as much as 70%.  But as global temperatures started to rise, the ecological stress faced by Europeans also began to fade. Mortality rates dropped and the level of violence fell, paving the way for a period known as Pax Britannica, which witnessed the emergence of a variety of innovations in technology (which enabled industrialization), medicine (which improved hygiene), and social welfare (such as the world's first welfare programs in Germany), making life even more comfortable. 
North America Edit
Early European explorers and settlers of North America reported exceptionally severe winters. For example, according to Lamb, Samuel Champlain reported bearing ice along the shores of Lake Superior in June 1608. Both Europeans and indigenous peoples suffered excess mortality in Maine during the winter of 1607–1608, and extreme frost was reported in the Jamestown, Virginia, settlement at the same time.  Native Americans formed leagues in response to food shortages.  The journal of Pierre de Troyes, Chevalier de Troyes, who led an expedition to James Bay in 1686, recorded that the bay was still littered with so much floating ice that he could hide behind it in his canoe on 1 July.  In the winter of 1780, New York Harbor froze, allowing people to walk from Manhattan Island to Staten Island.
The extent of mountain glaciers had been mapped by the late 19th century. In the north and the south temperate zones, Equilibrium Line Altitude (the boundaries separating zones of net accumulation from those of net ablation) were about 100 metres (330 ft) lower than they were in 1975.  In Glacier National Park, the last episode of glacier advance came in the late 18th and the early 19th centuries.  In 1879, famed naturalist John Muir found that Glacier Bay ice had retreated 48 miles.  In Chesapeake Bay, Maryland, large temperature excursions were possibly related to changes in the strength of North Atlantic thermohaline circulation. 
Because the Little Ice Age took place during the European colonization of the Americas, it threw off a lot of the early colonizers. The colonizers had expected the climate of North America to be similar to the climate of Europe at similar latitudes, however the climate of North America had hotter summers and colder winters than were expected by the Europeans. This was an effect aggravated by the Little Ice Age. This unpreparedness led to the collapse of many early European settlements in North America.
When colonizers settled at Jamestown, in modern day Virginia, historians agree it was one of the coldest time periods in the last 1000 years. Droughts were also a huge problem in North America during the Little Ice Age, settlers arriving in Roanoke were in the largest drought of the past 800 years. Tree ring studies done by the University of Arkansas discovered that many colonists arrived at the beginning of a seven year drought. These times of drought also decreased Native American populations and led to conflict due to food scarcity. English colonists at Roanoke forced Native Americans of Ossomocomuck to share their depleted supplies with them. This led to warfare between the two groups and Native American cities were destroyed. That cycle would repeat itself many times at Jamestown. The combination of fighting and cold weather led to the spread of diseases as well. The colder weather brought on by the Little Ice Age helped the Malaria parasites brought by Europeans in mosquitoes develop faster. This in turn led to many deaths among Native American populations. 
Cold winters made worse by the Little Ice Age were also an issue in North America for colonists. Anecdotal evidence shows that people who lived in North America suffered during this time. John Smith, who established Jamestown, Virginia, wrote of a winter so cold, not even the dogs could bear it. Another colonist, Francis Perkins, wrote in the Winter of 1607 that it got so cold that the river at his fort froze due to extremely cold weather. In 1642, Thomas Gorges wrote that between 1637 and 1645, colonists in Maine in Massachusetts had horrendous weather conditions. June of 1637 was so hot that European newcomers were dying in the heat and travelers had to travel at night to stay cool enough. He also wrote that the winter of 1641-1642 was “piercingly Intolerable” and that no Englishman nor Native American had ever seen anything like it. Stating that the Massachusetts bay had frozen as far as one could see and that horse carriages now roamed where ships used to be. The summers of 1638 and 1639 were very short, cold, and wet according to Gorges and this led to compounding food scarcity for a few years. To make matters worse, creatures like caterpillars and pigeons were feeding on crops and devastating harvests. Every year that Gorges writes about, he notes unusual weather patterns that include high precipitation, drought, and extreme cold or extreme heat. These all are byproducts of the Little Ice Age. 
While the Little Ice Age dropped global temperatures by an estimated 0.1 degrees celsius, it increased global weirding all over North America and the world. Summers got hotter and winters got colder. Floods ensued and so did droughts. The Little Ice age didn’t just cool places off a bit, it threw the climate into a weird unpredictable beast that made living in North America significantly harder for all of its inhabitants.
While nobody knows exactly what caused the Little Ice Age, one theory from Warren Ruddimen states that approximately 50% of the Little Ice Age originated in North America. This theory states that when European diseases wiped out 95 percent of Native Americans, the resulting effects led to global cooling. Approximately 55 million Native Americans died due to those diseases and the theory is that as a result of those deaths, 56 million hectares of land was abandoned and reforested. Ruddimen believes that this caused more oxygen to enter the air and then created a global cooling effect. 
Many of the people living in North America had their own theories as to why the weather was so poor. Colonist Ferdinando Gorges blamed the cold weather on cold ocean winds. Humphrey Gilbert tried to explain the extremely cold and foggy weather of Newfoundland by saying the earth drew cold vapors from the ocean and drew them west. Dozens of others had their own theories as to why North America was so much colder than Europe. But because of their observations and hypotheses, we know a lot about the Little Ice Age’s effect on North America. 
An analysis of several climate proxies undertaken in Mexico's Yucatán Peninsula, linked by its authors to Maya and Aztec chronicles relating periods of cold and drought, supports the existence of the Little Ice Age in the region. 
Another study conducted in several sites in Mesoamerica such as Los Tuxtlas and Lake Pompal in Veracruz, Mexico demonstrate a decrease in human activity in the area during the Little Ice Age. This was proven by studying charcoal fragments and the amount of maize pollen taken from sedimentary samples using a nonrotatory piston corer. The samples also showed volcanic activity which caused forest regeneration between 650 and 800 A.D. The instances of volcanic activity near Lake Pompal indicate varying temperatures, not a continuous coldness, during the Little Ice Age in Mesoamerica. 
Atlantic Ocean Edit
In the North Atlantic, sediments accumulated since the end of the last ice age, nearly 12,000 years ago, show regular increases in the amount of coarse sediment grains deposited from icebergs melting in the now open ocean, indicating a series of 1–2 °C (2–4 °F) cooling events recurring every 1,500 years or so.  The most recent of these cooling events was the Little Ice Age. These same cooling events are detected in sediments accumulating off Africa, but the cooling events appear to be larger, ranging between 3–8 °C (6–14 °F). 
Although the original designation of a Little Ice Age referred to reduced temperature of Europe and North America, there is some evidence of extended periods of cooling outside this region, but it is not clear whether they are related or independent events. Mann states: 
While there is evidence that many other regions outside Europe exhibited periods of cooler conditions, expanded glaciation, and significantly altered climate conditions, the timing and nature of these variations are highly variable from region to region, and the notion of the Little Ice Age as a globally synchronous cold period has all but been dismissed.
In China, warm-weather crops such as oranges were abandoned in Jiangxi Province, where they had been grown for centuries.  Also, the two periods of most frequent typhoon strikes in Guangdong coincide with two of the coldest and driest periods in northern and central China (1660–1680, 1850–1880).  Scholars have argued that the fall of the Ming dynasty may have been partially caused by the droughts and famines caused by the Little Ice Age. 
There are debates on the start date and time periods of Little Ice Age's effects. Most scholars agree on categorizing the Little Ice Age period into 3 distinct cold periods. 1458-1552, 1600-1720, and 1840-1880.  According to data from the National Oceanic and Atmospheric Administration, the Eastern Monsoon area of China was the earliest to experience the effects of Little Ice Age from 1560-1709. In the Western region of China surrounding the Tibetan Plateau, the effects of Little Ice Age lagged behind the Eastern region, with significant cold periods between 1620 and 1749. 
The temperature changes was unprecedented for the farming communities in China. According to Dr. Coching Chu's 1972 study, the Little Ice Age during the end of Ming Dynasty and start of Qing Dynasty (1650-1700) was one of the coldest periods in recorded Chinese history.  Many major droughts during summer months were recorded while significant freezing events occurred in Winter months, hurting the food supply significantly during Ming Dynasty.
This period of Little Ice Age would correspond to major historical events of the period. The Jurchen people resided in Northern China and formed a tributary state to the Ming government and Wanli Emperor. From 1573 to 1620, the Manchurian land experienced famine experienced extreme snowfall, which depleted agriculture production and decimated the livestock population. Scholars argued that this was caused by the temperature drops during Little Ice Age. Despite the lack of food production, Wanli Emperor ordered the Jurchens to pay the same amount of tribute each year. This led to anger and sowed seeds to the rebellion against Ming China. In 1616, Jurchens established the Later Jin dynasty. Led by Hong Taiji and Nurhaci, the Later Jin dynasty moved South and achieved decisive victories in battles against the Ming military such as the Battle of Fushun in 1618. 
Following the earlier defeats and the death of Wanli Emperor, Chongzhen Emperor took the reign of China and continued the war effort. From 1632 to 1641, the Little Ice Age climate began to cause drastic climate changes in Ming territories. For example, rainfall in Huabei region dropped by 11%
47% compared to historical average. Meanwhile, the Shaanbei region along the Yellow River experienced six major floods that ruined cities such as Yan’an. The climate factored heavily in weakening the Imperial government’s control over China and accelerated the fall of Ming dynasty. In 1644, Li Zicheng led Later Jin forces into Beijing, overthrowing the Ming Dynasty, and establishing the Qing Dynasty. 
During the early years of the Qing Dynasty, the little ice age continued to have a significant impact on Chinese society. During the rule of Kangxi Emperor (1661-1722), majority of the Qing territories were still much colder than the historical average. However, Kangxi Emperor pushed reforms and managed to increase socioeconomic recovery from the natural disasters, partially benefiting from the peacefulness of the early Qing dynasty. This essentially marked the end of the Little Ice Age in China and led to a more affluent era of Chinese monarchial history known as the High Qing era. 
In the Himalayas, the general assumption is that the cooling events in the Himalayas were synchronous with cooling events in Europe during the Little Ice Age based on the characteristics of moraines. However, applications of Quaternary dating methods such as surface exposure dating demonstrated that glacial maxima occurred between 1300 and 1600 CE, which was slightly earlier than the recorded coldest period in Northern Hemisphere. Many large Himalayan glacial debris remained close to their limits from the Little Ice Age to present. The Himalayas also experienced increase in snowfall at higher altitudes, resulting in a southward shift in the Indian summer monsoon and an increase in precipitation. Overall, the increase in winter precipitation may have caused some glacial movements. 
In Pakistan, the Balochistan province became colder and the native Baloch people started mass migration and settled along the Indus River in Sindh and Punjab provinces. 
The influence of the Little Ice Age on African climate has been clearly demonstrated throughout the 14th-19th century.  Despite variances throughout the continent, a general trend of declining temperatures led to an average cooling of 1 °C in the continent. 
In Ethiopia and North Africa, permanent snow was reported on mountain peaks at levels where it does not occur today.  Timbuktu, an important city on the trans-Saharan caravan route, was flooded at least 13 times by the Niger River there are no records of similar flooding before or since. 
Several paleoclimatic studies of Southern Africa have suggested significant changes in relative changes in climate and environmental conditions. In Southern Africa, sediment cores retrieved from Lake Malawi show colder conditions between 1570 and 1820, suggesting the Lake Malawi records "further support, and extend, the global expanse of the Little Ice Age."  A novel 3,000-year temperature reconstruction method, based on the rate of stalagmite growth in a cold cave in South Africa, further suggests a cold period from 1500 to 1800 "characterizing the South African Little Ice age."  This δ18O stalagmite record temperature reconstruction over a 350-year period (1690-1740) suggests that South Africa may have been the coldest region in Africa, cooling as much as 1.4 °C in the Summer.  Further, solar magnetic and Niño-Southern Oscillation cycle may have been key drivers of climate variability in the subtropical region. Periglacial features in the eastern Lesotho Highlands might have been reactivated by the Little Ice Age.  Another archaeological reconstruction of South Africa reveals the rise of the Great Zimbabwe people society due to ecological advantages due to increased rainfall over other competitor societies’ such as the Mupungubwe people. 
Aside from temperature variability, data from equatorial East Africa suggests impacts to the hydrologic cycle in the late 1700s. Historical data reconstructions from ten major African lakes indicate an episode of “drought and desiccation” occurred throughout East Africa.  This period showed drastic reductions in lake depth as these were transformed into desiccated puddles. It is very likely that locals could traverse lake Chad, among others, and bouts of “intense droughts were ubiquitous”. These predictors indicate local societies were probably launched into long migrations and warfare with neighboring tribes as agriculture was rendered virtually useless by the arid soil conditions.
Kreutz et al. (1997) compared results from studies of West Antarctic ice cores with the Greenland Ice Sheet Project Two GISP2 and suggested a synchronous global cooling.  An ocean sediment core from the eastern Bransfield Basin in the Antarctic Peninsula shows centennial events that the authors link to the Little Ice Age and Medieval Warm Period.  The authors note "other unexplained climatic events comparable in duration and amplitude to the LIA and MWP events also appear."
The Siple Dome (SD) had a climate event with an onset time that is coincident with that of the Little Ice Age in the North Atlantic based on a correlation with the GISP2 record. The event is the most dramatic climate event in the SD Holocene glaciochemical record.  The Siple Dome ice core also contained its highest rate of melt layers (up to 8%) between 1550 and 1700, most likely because of warm summers.  Law Dome ice cores show lower levels of CO
2 mixing ratios from 1550 to 1800, which Etheridge and Steele conjecture are "probably as a result of colder global climate." 
Sediment cores in Bransfield Basin, Antarctic Peninsula, have neoglacial indicators by diatom and sea-ice taxa variations during the Little Ice Age.  Stable isotope records from the Mount Erebus Saddle ice core site suggests that the Ross Sea region experienced 1.6 ± 1.4 °C cooler average temperatures during the Little Ice Age, compared to the last 150 years. 
Australia and New Zealand Edit
Due to its location in the Southern Hemisphere, Australia did not experience a regional cooling as in Europe or North America. Instead, the Australian Little Ice Age was characterized by humid, rainy climates followed by drying and aridification in the nineteenth century. 
As studied by Tibby et al. (2018), lake records from Victoria, New South Wales, and Queensland suggest that conditions in the east and south-east of Australia were wet and unusually cool from the sixteenth to early nineteenth centuries. This corresponds with the “peak” of the global Little Ice Age from 1594-1722. For example, the Swallow Lagoon rainfall record indicates that from circa 1500-1850, there was significant and consistent rainfall, sometimes exceeding 300 millimeters.  These rainfalls significantly reduced after circa 1890. Similarly, the hydrological records of Lake Surprise’s salinity levels reveal high humidity levels from circa 1440-1880, while an increase in salinity between 1860-1880 point to a negative change to the once-humid climate.  The mid-nineteenth century marked a notable change to east Australia’s rainfall and humidity patterns.
As Tibby et al. (2018) note, in eastern Australia, these paleoclimatic changes of the Little Ice Age in the late 1800s coincided with the agricultural changes resulting from European colonization. Following the 1788 establishment of British colonies on the Australian continent—primarily concentrated in eastern regions and cities like Sydney, and later Melbourne and Brisbane—the British introduced new agricultural practices such as pastoralism.  Practices such as these required widespread deforestation and vegetation clearance. Pastoralism and land clearing is captured in works of art such as prominent landscape artist John Glover’s 1833 painting, Patterdale Landscape with Cattle.
Over the next century, such deforestation led to biodiversity loss, wind and water-based soil erosion, and soil salinity.  Furthermore, as argued by Gordan et al. (2003), such land and vegetation clearance in Australia resulted in a 10% reduction in water vapor transport to the atmosphere. This occurred in western Australia as well, in which nineteenth century land-clearing resulted in reduced rainfall over the region.  By 1850-1890, these human agricultural practices, concentrated in the eastern region of Australia, most likely amplified the drying and aridification that marked the end of the Little Ice Age.
In the north, evidence suggests fairly dry conditions, but coral cores from the Great Barrier Reef show similar rainfall as today but with less variability. A study that analyzed isotopes in Great Barrier Reef corals suggested that increased water vapor transport from southern tropical oceans to the poles contributed to the Little Ice Age.  Borehole reconstructions from Australia suggest that over the last 500 years, the 17th century was the coldest on the continent.  The borehole temperature reconstruction method further indicates that the warming of Australia over the past five centuries is only around half that of the warming experienced by the Northern Hemisphere, further proving that Australia did not reach the same depths of cooling as the continents to the north.
On the west coast of the Southern Alps of New Zealand, the Franz Josef glacier advanced rapidly during the Little Ice Age and reached its maximum extent in the early 18th century, in one of the few cases of a glacier thrusting into a rainforest.  Evidence suggests, corroborated by tree ring proxy data, that the glacier contributed to a -0.56 °C temperature anomaly over the course of the Little Ice Age in New Zealand.  Based on dating of a yellow-green lichen of the Rhizocarpon subgenus, the Mueller Glacier, on the eastern flank of the Southern Alps within Aoraki / Mount Cook National Park, is considered to have been at its maximum extent between 1725-1730. 
Pacific Islands Edit
Sea-level data for the Pacific Islands suggest that sea level in the region fell, possibly in two stages, between 1270 and 1475. This was associated with a 1.5 °C fall in temperature (determined from oxygen-isotope analysis) and an observed increase in El Niño frequency.  Tropical Pacific coral records indicate the most frequent, intense El Niño-Southern Oscillation activity in the mid-seventeenth century.  Foraminiferald 18 O records indicate that the Indo-Pacific Warm Pool was warm and saline between 1000 and 1400 CE, with temperatures approximating current conditions, but cooled from 1400 CE onwards, reaching its lowest temperatures in 1700, consistent with the transition from mid-Holocene warming to the Little Ice Age.  The nearby Southwestern Pacific, however, experienced warmer than average conditions over the course of the Little Ice Age, thought to be due to increased trade winds causing increased evaporation and higher salinity in the region, and that the dramatic temperature differences between the higher latitudes and the equator resulted in drier conditions in the subtropics.  Independent multiproxy analyses of Raraku Lake(sedimentology, mineralology, organic and inorganic geochemistry, etc) indicate that Easter Island was subject to two phases of arid climate leading to drought, with the first occurring between 500 and 1200 CE, and second occurring during the Little Ice Age, from 1570 to 1720.  In between these two arid phases, the island enjoyed a humid period, extending from 1200 CE to 1570, coinciding with the maximum development of the Rapanui civilization. 
South America Edit
Tree-ring data from Patagonia show cold episodes between 1270 and 1380 and from 1520 to 1670, contemporary with the events in the Northern Hemisphere.   Eight sediment cores taken from Puyehue Lake have been interpreted as showing a humid period from 1470 to 1700, which the authors describe as a regional marker of the onset of the Little Ice Age.  A 2009 paper details cooler and wetter conditions in southeastern South America between 1550 and 1800, citing evidence obtained via several proxies and models.  18 O records from three Andean ice cores show a cool period from 1600 to 1800. 
Although only anecdotal evidence, in 1675 the Spanish Antonio de Vea expedition entered San Rafael Lagoon through Río Témpanos (Spanish for "Ice Floe River") without mentioning any ice floe but stating that the San Rafael Glacier did not reach far into the lagoon. In 1766, another expedition noticed that the glacier reached the lagoon and calved into large icebergs. Hans Steffen visited the area in 1898, noticing that the glacier penetrated far into the lagoon. Such historical records indicate a general cooling in the area between 1675 and 1898: "The recognition of the LIA in northern Patagonia, through the use of documentary sources, provides important, independent evidence for the occurrence of this phenomenon in the region."  As of 2001, the border of the glacier had significantly retreated as compared to the borders of 1675. 
Scientists have tentatively identified seven possible causes of the Little Ice Age: orbital cycles decreased solar activity increased volcanic activity altered ocean current flows  fluctuations in the human population in different parts of the world causing reforestation, or deforestation and the inherent variability of global climate.
Orbital cycles Edit
Orbital forcing from cycles in the earth's orbit around the sun has, for the past 2,000 years, caused a long-term northern hemisphere cooling trend that continued through the Middle Ages and the Little Ice Age. The rate of Arctic cooling is roughly 0.02 °C per century.  This trend could be extrapolated to continue into the future, possibly leading to a full ice age, but the twentieth-century instrumental temperature record shows a sudden reversal of this trend, with a rise in global temperatures attributed to greenhouse gas emissions. 
Solar activity Edit
Solar activity includes any sun disturbances like sunspots, solar flares, or prominences, and scientists can track these solar activities in the past by analyzing both the carbon 14 or Beryllium 10 isotopes in items like tree rings. These solar activities, while not the most common or noticeable causes for the little ice age, provide considerable evidence that they played a part in the formation of the little ice age and the increase in temperature after the period. During the time of the little ice age which ranged from 1450 to 1850, there were very low recorded levels of solar activity in the Spörer, Maunder, and Dalton minima.
The Spörer minimum was between 1450-1550 AD, when the little ice age started. A study by Dmitri Mauquoy and others found that at the beginning of Spörer, the percentage of change of carbon-14 skyrocketed to about 10%. [ citation needed ] This percentage stayed pretty common along with the entire duration of the Spörer minimum, then around 1600 dropped rapidly before the Maunder (1645-1715) where it rose again to a little under 10% change. To put this into perspective, during standard periods the percentage change in carbon-14 idles between -5 to 5 percent so this is a considerable change. At the end of the little ice age which is also the Dalton minimum (1790-1830), the percentage change is normal around -1%. These changes in the Carbon-14 have a strong relationship with the temperature because during these three periods as an increase in the carbon-14 does correlate with cold temperatures during the little ice age. 
In a study by Judith Lean, where she talked about the sun and climate relationships and the cause and effect relationship that helped form the little ice age. In her research, she found that during a certain time period there a .13% solar irradiance increased the temperature of the earth by .3 degree Celsius. This was around 1650-1790 and this information can help you formulate another idea of what happened during the little ice age. When they calculated correlation coefficients of the global temperature response to solar forcing over three different periods it comes out to an average coefficient of .79. This shows a strong relationship between the two components and helps the point that the little ice age was considerably cold with very low solar activity. Lean and your team also formulated an equation where Change in T is equal to -168.802+Sx0.123426. This equals turns out to a .16 increase in temperature for every .1% increase in solar irradiance. 
To summarize, the entire length of the little ice age had a high percentage change in carbon-14 and low social irradiance. Both of these show a strong relationship to the cold temperatures during the time and while the changes of solar activity actually have on the temperature of the earth compared to things like greenhouse gases is very minimal. Solar activity is still important to the whole picture of climate change and does affect the earth even if it’s just less than one Celsius over a few hundred years.
Volcanic activity Edit
In a 2012 paper, Miller et al. link the Little Ice Age to an "unusual 50-year-long episode with four large sulfur-rich explosive eruptions, each with global sulfate loading >60 Tg" and notes that "large changes in solar irradiance are not required." 
Throughout the Little Ice Age, the world experienced heightened volcanic activity.  When a volcano erupts, its ash reaches high into the atmosphere and can spread to cover the whole earth. The ash cloud blocks out some of the incoming solar radiation, leading to worldwide cooling that can last up to two years after an eruption. Also emitted by eruptions is sulfur, in the form of sulfur dioxide gas. When it reaches the stratosphere, it turns into sulfuric acid particles, which reflect the sun's rays, further reducing the amount of radiation reaching Earth's surface.
A recent study found that an especially massive tropical volcanic eruption in 1257, possibly of the now-extinct Mount Samalas near Mount Rinjani, both in Lombok, Indonesia, followed by three smaller eruptions in 1268, 1275, and 1284 did not allow the climate to recover. This may have caused the initial cooling, and the 1452–53 eruption of Kuwae in Vanuatu triggered a second pulse of cooling.  The cold summers can be maintained by sea-ice/ocean feedbacks long after volcanic aerosols are removed.
Other volcanoes that erupted during the era and may have contributed to the cooling include Billy Mitchell (ca. 1580), Huaynaputina (1600), Mount Parker (1641), Long Island (Papua New Guinea) (ca. 1660), and Laki (1783).  The 1815 eruption of Tambora, also in Indonesia, blanketed the atmosphere with ash the following year, 1816, came to be known as the Year Without a Summer,  when frost and snow were reported in June and July in both New England and Northern Europe.
Ocean circulation Edit
Another possibility is that there was a slowing of thermohaline circulation.     The circulation could have been interrupted by the introduction of a large amount of fresh water into the North Atlantic, possibly caused by a period of warming before the Little Ice Age known as the Medieval Warm Period.    There is some concern that a shutdown of thermohaline circulation could happen again as a result of the present warming period.  
Decreased human populations Edit
Some researchers have proposed that human influences on climate began earlier than is normally supposed (see Early anthropocene for more details) and that major population declines in Eurasia and the Americas reduced this impact, leading to a cooling trend.
The Black Death is estimated to have killed 30% to 60% of Europe's population.  In total, the plague may have reduced the world population from an estimated 475 million to 350–375 million in the 14th century.  It took 200 years for the world population to recover to its previous level.  William Ruddiman proposed that these large population reductions in Europe, East Asia, and the Middle East caused a decrease in agricultural activity. Ruddiman suggests reforestation took place, allowing more carbon dioxide uptake from the atmosphere, which may have been a factor in the cooling noted during the Little Ice Age. Ruddiman further hypothesized that a reduced population in the Americas after European contact in the 16th century could have had a similar effect.   Other researchers supported depopulation in the Americas as a factor, asserting that humans had cleared considerable amounts of forest to support agriculture in the Americas before the arrival of Europeans brought on a population collapse.   Richard Nevle, Robert Dull and colleagues further suggested that not only anthropogenic forest clearance played a role in reducing the amount of carbon sequestered in Neotropical forests, but that human-set fires played a central role in reducing biomass in Amazonian and Central American forests before the arrival of Europeans and the concomitant spread of diseases during the Columbian exchange.    Dull and Nevle calculated that reforestation in the tropical biomes of the Americas alone from 1500 to 1650 accounted for net carbon sequestration of 2-5 Pg.  Brierley conjectured that European arrival in the Americas caused mass deaths from epidemic disease, which caused much abandonment of farmland, which caused much return of forest, which sequestered greater levels of carbon dioxide.  A study of sediment cores and soil samples further suggests that carbon dioxide uptake via reforestation in the Americas could have contributed to the Little Ice Age.  The depopulation is linked to a drop in carbon dioxide levels observed at Law Dome, Antarctica.  A 2011 study by the Carnegie Institution's Department of Global Ecology asserts that the Mongol invasions and conquests, which lasted almost two centuries, contributed to global cooling by depopulating vast regions and allowing for the return of carbon absorbing forest over cultivated land.  
Population increases at mid- to high-latitudes Edit
During the Little Ice Age period, it is suggested that increased deforestation had a significant enough effect on albedo (reflectiveness of the Earth) to decrease regional and global temperatures. Changes in albedo were caused by widespread deforestation at high latitudes. In turn this exposed more snow cover to and increased reflectiveness of the Earth's surface as land was cleared for agricultural use. This theory implies that over the course of the Little Ice Age land was cleared to an extent that warranted deforestation as a cause for climate change. 
It has been proposed that Land Use Intensification theory could explain this phenomenon. This theory was originally proposed by Ester Boserup and suggests that agriculture is only advanced as the population demands it.  Furthermore, there is evidence of rapid population and agricultural expansion that could warrant some of the changes observed in the climate during this period.
This theory is still under speculation for multiple reasons. Primarily, the difficulty of recreating climate simulations outside of a narrow set of land in these regions. This has led to an inability to rely on data to explain sweeping changes, or account for the wide variety of other sources of climate change globally. As an extension of the first reason climate models including this time period have shown increases and decreases in temperature globally.  That is, climate models have not shown deforestation as a singular cause for climate change, nor as a reliable cause for global temperature decrease.
Inherent variability of climate Edit
Spontaneous fluctuations in global climate might explain past variability. It is very difficult to know what the true level of variability from internal causes might be given the existence of other forces, as noted above, whose magnitude may not be known. One approach to evaluating internal variability is to use long integrations of coupled ocean-atmosphere global climate models. They have the advantage that the external forcing is known to be zero, but the disadvantage is that they may not fully reflect reality. The variations may result from chaos-driven changes in the oceans, the atmosphere, or interactions between the two.  Two studies have concluded that the demonstrated inherent variability is not great enough to account for the Little Ice Age.   The severe winters of 1770 to 1772 in Europe, however, have been attributed to an anomaly in the North Atlantic oscillation. 
Snow in Summer: A Global History of Frozen Treats - HISTORY
No specific person has officially been credited with inventing ice cream. Its origins date back as far as 200 B.C., when people in China created a dish of rice mixed with milk that was then frozen by being packed in snow. The Chinese King Tang of Shang is thought to have had over ninety “ice men” who mixed flour, camphor, and buffalo milk with ice. The Chinese are also credited with inventing the first “ice cream machine.” They had pots they filled with a syrupy mixture, which they then packed into a mixture of snow and salt.
Other early ice cream-like confectionery indulgers include Alexander the Great, who enjoyed eating snow flavoured with honey. Emperor Nero Claudius Caesar of Rome was said to have sent people up to the mountains to collect snow and ice which would then be flavoured with juice and fruit—kind of like a first century snow cone. These early “ice creams” were obviously a luxury indulged in by the rich, as not everyone had the ability to send servants up the mountains to collect snow for them.
One of the earliest forerunners of modern ice cream was a recipe brought back to Italy from China by Marco Polo. The recipe was very like what we would call sherbet. From there, it is thought that Catherine de Medici brought the dessert to France when she married King Henry II in 1533. In the 1600s, King Charles I of England was said to have enjoyed “cream ice” so much that he paid his chef to keep the recipe a secret from the public, believing it to be solely a royal treat. However, these two stories appeared for the first time in the 19 th century, many years after they were said to have taken place, so may or may not be true.
One of the first places to serve ice cream to the general public in Europe was Café Procope in France, which started serving it in the late 17th century. The ice cream was made from a combination of milk, cream, butter, and eggs. However, it was still primarily a treat for the elite and was not yet popular among every class.
The first mention of ice cream in America appeared in 1744, when a Scottish colonist visited the house of Maryland Governor Thomas Bladen wrote about the delicious strawberry ice cream he had while dining there. The first advertisement for ice cream in America appeared in 1777 in the New York Gazette, in which Philip Lenzi said ice cream was “available almost every day” at his shop.
Early American presidents loved ice cream, too. President George Washington purchased around $200 worth of ice cream (about $3,000 today) in the summer of 1790 and also owned two pewter ice cream pots. However, the “origin” story that his wife Martha once left sweet cream on the back porch one evening and returned in the morning to find ice cream is definitely not true. Thomas Jefferson created his own recipe for vanilla ice cream, and President Madison’s wife served strawberry ice cream at her husband’s second inaugural banquet.
Up until the 1800s, ice cream was mostly a treat reserved for special occasions as it couldn’t be stored for long due to the lack of insulated freezers. People would have ice cut from lakes in the winter and store it in the ground or brick ice houses, which were insulated with straw. Ice cream at this time was made using the “pot freezer” method, which involved placing a bowl of cream in a bucket of ice and salt (note: not mixing the ice and salt with the cream as many believe). In 1843, this method was replaced by the hand-cranked churn which was patented by Nancy Johnson. The churn created smoother ice cream faster than the pot freezer method.
Ice cream wasn’t big business until Jacob Fussell built an ice cream factory in Pennsylvania in 1851. Fussell was a milk dealer who bought dairy products from farmers in Pennsylvania and sold them in Baltimore. He found that an unstable demand often left him with a lot of extra milk and cream, which he then turned into ice cream. His business was so successful that he opened several other factories. Because mass production cut the cost of ice cream significantly, it became much more popular and a more viable treat for people of lower classes.
Ice cream received a further boost when, in the 1870s, Carl von Linde of Germany invented industrial refrigeration. This, along with other technological advances like steam power, motorized vehicles, and electric power, made ice cream that much easier to produce, transport, and store. Next time you grab an ice cream cone, you can thank the Industrial Revolution for your treat!
Due to its new, widespread availability in the late 1800s, additional ice cream recipes began to take form. Soda fountains emerged in 1874, and with them came the invention of the ice cream soda. Religious leaders condemned indulging in ice cream sodas on Sundays and set up “blue laws” banning their serving, which is thought by many to be how ice cream sundaes came about. Evidence seems to indicate that shop owners got around the problem by serving the ice cream with syrup and none of the carbonation and called them “ice cream Sundays.” According to the Oxford English Dictionary, they later modified the name to “sundae” to avoid association with the Sabbath. However, several cities take credit for being the home of the ice cream sundae and it can’t be proved that getting around blue laws was truly how the first person came up with the idea of an ice cream sundae, though it does seem plausible enough. But whatever the case, this seems to have been at least partially how the sundae was popularized.
Contrary to popular belief, the ever-popular ice cream cone was not invented at the 1904 World’s Fair. For instance, ice cream cones are mentioned in the 1888 Mrs. Marshall’s Cookbook and the idea of serving ice cream in cones is thought to have been in place long before that. However, the practice didn’t become popular until 1904. As to who specifically at the World’s Fair served the cones that popularized the treat, nobody knows exactly. The story goes that an ice cream vendor at the St. Louis World Fair ran out of cardboard cups in which to serve his ice cream. The stall beside him had waffles on offer, but due to the heat he wasn’t selling very many. Thus, and offer was made to roll up his waffles to make cones, and the resulting product was a hit. However, that may well just be a legend as there are no documented specifics, like the names of the vendors, to be able to verify the story and many ice cream vendors at that World’s Fair have claimed to be the ones to serve the cones there first. Whatever the case, it was the World’s Fair that popularized the cones and certainly some ice cream vendor or vendors were behind it, whether by happy accident as the story goes or because they planned it that way has been lost to history.
Ice cream was first sold in grocery stores in the 1930s. World War II further popularized the dessert as the treat was great for troop morale and became somewhat of a symbol of America at the time (so much so that Italy’s Mussolini banned ice cream to avoid the association). This war time ice cream resulted in the biggest producer of ice cream in America in 1943 being the United States Armed Forces.
Today, it is estimated that over 1.6 billion gallons of ice cream and related frozen dairy products are produced annually in the United States alone. In addition, U.S. citizens eat a whopping four gallons of ice cream per person each year on average.
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A Brief History of the Ice Cream Truck
It’s the sound of summer: a string of jangly notes cutting through the sticky-hot air. The response is Pavlovian. Mouths water. Parents reach for their wallets. Kids lace up their shoes and hit the pavement. For Ben Van Leeuwen, it was no different. Growing up in suburban Riverside, Conn., he’d race toward the siren song. The ice cream truck was coming.
In the sea of sweaty half-pints elbowing to place orders, Van Leeuwen always took his time. He’d inspect the full menu, pondering each offering, from cartoon-colored Popsicles to animal-shaped treats with gum balls for eyes. He’d imagine the flavors—Strawberry Shortcake, Choco Taco, King Cone. Then he’d pick what he always picked: a Reckless Rainbow Pop Up. “We were poor,” he laughs. The push pop was cheap.
Today, Van Leeuwen is an ice cream magnate. With six trucks and three storefronts in New York City, the company he runs with his brother, Pete, and business partner, Laura O’Neill, prides itself on its quality. Handcrafted recipes combine sustainably sourced ingredients from far-flung places: Michel Cluizel chocolate from France, pistachios from Sicily, Tahitian vanilla beans from Papua New Guinea. The flavors have put Van Leeuwen on the vanguard of an ice cream truck resurgence. In a single generation, the ice cream truck has moved upmarket.
The history of frozen street treats begins long before Van Leeuwen encountered his first push pop—it begins before even mechanical refrigeration. The very nature of the industry—taking something frozen and hawking it on sultry sidewalks—has always forced ice cream peddlers to innovate. That the cold treat had to come to America before it could move off kings’ tables and into the hands of common folk makes the story that much sweeter.
We All Scream for Ice Cream
It’s hard to imagine now, but for much of human history, Slurpees and Klondike bars and even the humble Reckless Rainbow would have been considered status symbols. Difficult to obtain and harder to store, ice itself was once a luxury. When the Roman Emperor Nero wanted Italian ice, he ordered it the old-fashioned way—dispatching his servants to fetch snow from mountain tops, wrap it in straw, and bring it back to mix with fruits and honey—a practice still popular with elites in Spain and Italy 1,500 years later. In the fourth century, the Japanese emperor Nintoku was so enamored with the frozen curiosity that he created an annual Day of Ice, during which he presented ice chips to palace guests in an elaborate ceremony. Around the world, monarchs in Turkey, India, and Arabia used flavored ices to punch up the extravagance at banquets, serving frosty bouquets flavored with fruit pulp, syrup, and flowers—often the grand finale at feasts intended to impress. But it wasn’t until the mid-16th century, when scientists in Italy discovered a process for on-demand freezing—placing a container of water in a bucket of snow mixed with saltpeter—that the ice cream renaissance truly began.
The innovation spread through European courts, and before long, royal chefs were whipping up red wine slushes, icy custards, and cold almond creams. Italian and French monarchs developed a taste for sorbets. And cooks experimented with every exotic ingredient in their arsenal: violets, saffron, rose petals. But while the excitement for ice cream grew, the treats were clearly reserved for the elite. The dessert needed a trip across the pond and a few more centuries of innovation before it could trickle down to the masses.
Ice cream came to America with the first colonists. British settlers brought recipes with them, and the treat found space at the Founding Fathers’ tables. George Washington loved it. Thomas Jefferson was such a fan that he studied the art of ice cream making in France and returned with a machine so he could churn his own flavors at Monticello. But even in this monarch-free land, the frosty desserts were an extravagance. Vanilla and sugar were expensive, and access to ice was limited. To serve the dessert year-round, Jefferson built himself an icehouse, refrigerated with wagonloads of ice harvested from the nearby Rivanna River. Still, even with all the means and materials, the road to producing ice cream was rocky.
As food historian Mark McWilliams explains in The Story Behind the Dish, making a scoop was laborious. Cooks had to extract the iced mixture from a frozen pewter bucket, churn and blend it with cream by hand, and place the concoction back into the bucket for additional freezing. To get the desired silky texture, this churning had to be repeated multiple times over days. McWilliams writes, “the process was long and taxing, and thus generally managed by servants or slaves.” Still, there was a market for the product. According to McWilliams, “The labor-intensive process may have restricted ice cream to the wealthy, but it also measured how strongly ice cream was desired.” Everyone wanted a taste. And now, as a new wave of immigrants began looking for something novel to peddle on city streets, working-class people were about to take their licks.
The Ice Age
In the 1800s, the ice delivery industry exploded. Companies began harvesting frozen rivers and transporting ice to homes at affordable prices. Meanwhile, the technology for hand-crank ice cream makers advanced, making it far easier to scoop sundaes at home. Before long, ice cream was regularly served in parlors and tea gardens across the country. By the 1830s, ice cream’s role as an Independence Day treat was well established. But for the poor urban populations who couldn’t afford July 4th ices or the fresh ingredients to make ice cream at home, immigrant street vendors came to the rescue. Fresh off the boat and with limited job prospects, these innovators used their culinary talents to grasp at the American dream, selling frozen treats from carts chilled with ice.
“Italy and France was where ice cream was first truly developed they made it delicious,” says food writer Laura B. Weiss, author of Ice Cream: A Global History. “In the U.S., they developed the business.” The cheap wooden wagons let proprietors avoid rent and taxes that came with setting up a store. And demand for their wares was always high.
One popular treat, called hokey-pokey, was a Neapolitan-striped confection. Made with condensed milk, sugar, vanilla extract, cornstarch, and gelatin, all cut into two-inch squares and wrapped in paper, the bite-sized dessert was the perfect street food. According to Anne Cooper Funderburg’s Chocolate, Strawberry, and Vanilla: A History of American Ice Cream, young children of all ethnicities—Jewish, Irish, Italian—would gather on the cobbled streets of Park Row and the Bowery, heeding the vendors’ melodic call: “Hokey-pokey, sweet and cold for a penny, new or old.” (“Hokey-pokey” is a mangling of the Italian phrase O che poco, or “Oh, how little.”)
Penny licks were also popular among New York’s children and the working class. Before the invention of the ice cream cone, vendors scooped ice cream into a regular glass, which a customer would lick clean. Then they returned the glass to the peddler, who would swish it in a pail before refilling it for the next customer. It was an entirely unsanitary practice. “The mix-ins were bacteria, not chocolate chips,” says Weiss.
But it was the ice cream sandwich that truly melted the social boundaries, as blue and white collars alike huddled around pushcarts on hot summer days. According to an article in the August 19, 1900 edition of The Sun, “[Wall Street] brokers themselves got to buying ice cream sandwiches and eating them in a democratic fashion side by side on the sidewalk with the messengers and the office boys.” In fact, by the mid-1800s, ice cream had become such a common indulgence that Ralph Waldo Emerson warned about America’s bent toward materialism and gluttony, hailing ice cream as a chief example. And he was right: In the 1860s, thousands of New York City peddlers were selling penny licks and ice cream sandwiches to ravenous crowds. “They were really the first ice cream trucks,” says Weiss. “They started ice cream as a street food. It was a walk-around food—you’d stand up and eat it.” Ice cream had become a staple of the American diet—not just for the rich and powerful, but for everybody—and it was about to get even more mobile.
On a winter evening in 1920, candy maker Harry Burt was puttering around his ice cream shop in Youngstown, Ohio. Burt had made a name for himself by sticking a wooden handle on a ball of candy to create the Jolly Boy Sucker—a newfangled lollipop. Ready for a bigger challenge, he set out to create an ice cream novelty. He started by mixing coconut oil and cocoa butter to seal a smooth block of vanilla ice cream in the silky chocolate coating. The treat looked good, but it was messy. When his daughter Ruth grabbed for the bar, more of the chocolate coating ended up on her hands than her mouth. So Harry Jr., Burt’s 21-year-old son, came up with a better idea: Why not use the sticks from the lollipops as handles? And with that, the Good Humor bar was born. But Burt wasn’t done innovating yet.
A visionary, Burt was intrigued by the era’s technological advances. Prohibition had helped soda fountains and ice cream shops proliferate in place of bars. Fast food like burgers and hot dogs had infiltrated the menus in America’s swelling suburbs. Meanwhile, the Henry Ford–led automobile industry was exploding. To Burt, combining these national trends—fast food and cars—was a no-brainer. He just needed to figure out how to get his portable treat into the hands of hungry kids. In 1920, Burt invested in 12 refrigerator trucks for distribution around the city. He made sure they were pristine white and put professional-looking drivers in signature white uniforms to signify cleanliness and safety to parents. Then he crafted a scheme for luring the kids. “He promised to follow a specified route so families would know when to expect the truck to come by,” says Nick Soukas, director of ice cream for Unilever, which now owns the Good Humor brand. “A bell, which came from Harry Jr.’s bobsled, chimed so everyone would know they could come out and purchase Good Humor bars.” At first, all that ringing drew curious children into the streets to see what the fuss was about, but before long, the sound was synonymous with the ice cream man.
From the 1920s to the ’60s, thousands of Good Humor men patrolled the nation’s neighborhoods, becoming part of the communities they served. Good Humor men inspired a children’s Little Golden Book. In 1965, Time reported, “To the young, he has become better known than the fire chief, more welcome than the mailman, more respected than the corner cop.” When a Westchester County, N.Y., Good Humor man switched routes, 500 neighborhood children signed a petition for his return.
But Burt’s truck wasn’t the only game in town. In the 1950s, two brothers from Philadelphia, William and James Conway, were busy dreaming up their own version of a mobile ice cream unit. At the time, soft-serve machines had become popular in soda shops, and the Conways saw no reason they couldn’t go mobile. So they bolted a soft-serve machine to the floor of a truck. On St. Patrick’s Day in 1956, the brothers took their Mister Softee truck on its maiden voyage, handing out green ice cream to excited kids on West Philadelphia streets. “That didn’t really work too well,” says Jim Conway, son of James and current president of Mister Softee.
The heat and power of the condensers, generator, and gas engines overwhelmed the early trucks, and the electricity often puttered out. “You’d be in the middle of making someone’s cone, and everything would shut down,” Conway says. “You’d have to open the back doors and wait for the thing to cool.”
Perfecting the vehicle proved to be a challenge. The Conways had to experiment with airflow and mitigating heat, using fans and different generators. (Decades later, the company would customize its trucks with innovative rust-free aluminum, General Motors Vortec engines, and high-efficiency Electro Freeze soft-serve machines.) By 1958, the company had become so successful that the brothers began to franchise. Before long, the trademark sailboat-blue and white ice cream trucks were being sold to vendors all over the Northeast and mid-Atlantic. The Conways even one-upped the Good Humor bell, hiring Grey Advertising to pen a jingle for the company. By 1960, the “Mister Softee (Jingle and Chimes)” was playing from trucks on a drum-and-spindle contraption, like a roaming music box. A modern day “Hokey Pokey,” Mister Softee’s never-ending ditty became the siren call to a new generation.
Chasing down the ice cream man on hot summer days wasn’t Ben Van Leeuwen’s only formative experience with ice cream trucks. In 2005, while Van Leeuwen was attending Skidmore College, he rented a retired Good Humor truck and sold the treats with his brother to wealthy Connecticut residents. But Van Leeuwen found that the allure of the treats had faded. “I hated the way they tasted,” he says. The brothers did, however, appreciate the independence of the job. And with organic farmer’s markets blooming all over New York City and the food truck itself enjoying a gourmet reinvention, the brothers saw a modern ice cream market developing. People were increasingly interested in their food’s origins just as they were clamoring for exotic epicurean adventures. In 2008, the brothers rolled out their first truck, painted a vintage faded yellow, after spending a few months developing their first batch of flavors. They were initially too rushed to outfit their truck with speakers. When they realized the silence helped them stand out from Mister Softee’s insistent jingle, they decided to remain music-free.
Today, there’s no shortage of entrepreneurs in the ice cream truck market. In San Jose, Calif., Ryan and Christine Sebastian created Treatbot, “a karaoke ice cream truck from the future” that allows customers to eat scoops of Eastside Horchata ice cream while singing Michael Jackson’s “Beat It.” In Tacoma, Cool Cycles Ice Cream Company sells motorcycles with a sidecar freezer that holds 600 ice cream bars. And in New York City, Doug Quint, a classically trained bassoonist, turned a retired Mister Softee truck into the Big Gay Ice Cream Truck, which spun off into a storefront that pairs classic soft serve with toppings like sriracha hot sauce and pumpkin butter.
But classicists need not fear. The traditional soft serve truck is in no danger. Although Good Humor phased out its trucks in the late ’70s, today there are more than 400 Mister Softee franchises employing more than 700 trucks across 15 states. Except for the trucks’ tune technology—the jingle is now blasted loud and clear through electronic circuits—they’re unchanged, right down to the classic soft serve menu on the side. “For close to 50 years, that menu board has changed only four times,” Conway says. Keeping tradition close is a big part of the Mister Softee ideal.
Whether they’re vintage or modern, classic or creative, ice cream trucks have a seductive allure that’s about more than just ice cream. They summon a particular kind of nostalgia—the sense of freedom and possibility that comes from long, carefree summer days and the particular thrill of having a dollar in your pocket and a long list of treats from which to choose. The ice cream man has basically been doing the same thing for hundreds of years now—exciting crowds by delivering something utterly familiar wrapped in different packages. But there’s comfort in that. Van Leeuwen’s quick to point out that the fan favorite among his elaborately refined offerings isn’t its sweet sticky black rice flavor or its luscious strawberry-beet creation, but vanilla, plain and simple. And as the upper-class crowd packs into the Van Leeuwen shop to sample the gourmet scoops, just one neighborhood over it’s evident how little ice cream has changed. Standing by the Red Hook ball fields, you’ll find immigrants rolling tiny pushcarts filled with flavored ices, chasing their dreams the way so many new Americans have, hawking a dessert of kings at nickel-and-dime prices.