Little Ice Age


Global average temperatures show that the Little Ice Age was not a distinct planet-wide time period but the end of a long temperature decline, which preceded the recent global warming.[1]

The Little Ice Age (LIA) was a period of regional cooling, particularly pronounced in the North Atlantic region, that occurred after the Medieval Warm Period.[2] It was not a true ice age of global extent. The term was introduced into scientific literature by François E. Matthes in 1939.[3] The time period has been conventionally defined as extending from the 16th to the 19th centuries,[4][5][6] but some experts prefer an alternative timespan from about 1300[7] to about 1850.[8][9][10]

The NASA Earth Observatory notes three particularly cold intervals. One began about 1650, another about 1770, and the last in 1850, all of which were separated by intervals of slight warming.[6] The Intergovernmental Panel on Climate Change Third Assessment Report considered that the timing and the areas affected by the Little Ice Age suggested largely independent regional climate changes, rather than a globally synchronous increased glaciation. At most, there was modest cooling of the Northern Hemisphere during the period.[11]

Several causes have been proposed: cyclical lows in solar radiation, heightened volcanic activity (specifically the catastrophic Kaharoa eruption of Mount Tarawera in 1315[12]), changes in the ocean circulation, variations in Earth's orbit and axial tilt (orbital forcing), inherent variability in global climate, and decreases in the human population (such as from the Black Death and the epidemics emerging in the Americas upon European contact[13]).

Areas involved

The Intergovernmental Panel on Climate Change Third Assessment Report (TAR) of 2001 described the areas that were affected:

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.[11]

The IPCC Fourth Assessment Report (AR4) of 2007 discusses more recent research and gives 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.[14]


The last written records of the Norse Greenlanders are from a 1408 marriage at Hvalsey Church, which is now the best-preserved Norse ruins.

There is no consensus on when the Little Ice Age began,[15][16] 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 that were collected from beneath ice caps on Baffin Island and Iceland, Miller et al. (2012)[7] state that cold summers and ice growth began abruptly between 1275 and 1300, followed by "a substantial intensification" from 1430 to 1455.[7]

In contrast, a climate reconstruction based on glacial length[17][18] shows no great variation from 1600 to 1850 but a strong retreat thereafter.

Therefore, any of several dates ranging over 400 years may indicate the beginning of the Little Ice Age:

  • 1250 for when Atlantic pack ice began to grow, a cold period that was possibly triggered or enhanced by the massive eruption of Samalas volcano in 1257[19] and the associated volcanic winter.
  • 1275 to 1300 for when the radiocarbon dating of plants shows that they were killed by glaciation
  • 1300 for when warm summers stopped being dependable in Northern Europe
  • 1315 for when rains and the Great Famine of 1315–1317 occurred
  • 1560 to 1630 for when the worldwide glacial expansion, known as the Grindelwald Fluctuation,[20] began
  • 1650 for when the first climatic minimum occurred

The Little Ice Age ended in the latter half of the 19th century or in the early 20th century.[21][22][23]

The 6th report of the IPCC describes the coldest period in the last millenium as:[24]

"...a multi-centennial period of relatively low temperature beginning around the 15th century, with GMST averaging –0.03 [–0.30 to 0.06] °C between 1450 and 1850 relative to 1850–1900."


By region


The Frozen Thames, 1677

The Baltic Sea froze over twice, in 1303 and 1306–07, and years followed of "unseasonable cold, storms and rains, and a rise in the level of the Caspian Sea.”[25] 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.[26] Canals and rivers in Great Britain and the Netherlands were frequently frozen deeply enough to support ice skating and winter festivals.[26] 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 have affected the river's flow and depth and greatly diminish the possibility of further freezes.[27] 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 marched 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 and closed 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.[28] Iceland also suffered failures of cereal crops and people moved away from a grain-based diet.[29] The Norse colonies in Greenland had starved and vanished by the early 15th century because of crop failures and the inability for livestock to be maintained throughout increasingly-harsh winters. Greenland was largely cut off by ice from 1410 to the 1720s.[30]

Winter skating on the main canal of Pompenburg, Rotterdam in 1825, shortly before the minimum, by Bartholomeus Johannes van Hove

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."[31] In Lisbon, Portugal, snowstorms were much more frequent than today, and one winter in the 17th century produced eight snowstorms.[32] Many springs and summers were cold and wet but with great variability between years and groups of years. That was particularly evident during the "Grindelwald Fluctuation" (1560–1630); the rapid cooling phase was associated with more erratic weather, including increased storminess, unseasonal snowstorms, and droughts.[33] Crop practices throughout Europe had to be altered to adapt to the shortened and less reliable growing season, and there were many years of dearth and famine. One was the Great Famine of 1315–1317, but that may have been before the Little Ice Age.[34] 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."[35] Viticulture disappeared from some northern regions, and storms caused serious flooding and loss of life. Some of them resulted in the permanent loss of large areas of land from the Danish, German, and Dutch coasts.[31]

The violinmaker Antonio Stradivari produced his instruments during the Little Ice Age. The colder climate is proposed to have caused the wood that was used in his violins to be denser than in warmer periods and to contribute to the tone of his instruments.[36] According to the science historian James Burke, the period inspired such novelties in everyday life as the widespread use of buttons and button-holes, as well as knitting of custom-made undergarments for the better covering and insulating of the body. Chimneys were invented to replace open fires in the centre of communal halls to allow houses with multiple rooms to have the separation of masters from servants.[37]

The Little Ice Age, by the anthropologist Brian Fagan of the University of California at Santa Barbara, tells of the plight of European peasants from 1300 to 1850: 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."[38] Historian Wolfgang Behringer has linked intensive witch-hunting episodes in Europe to agricultural failures during the Little Ice Age.[39]

The Frigid Golden Age, by the environmental historian Dagomar Degroot of Georgetown University, in contrast, reveals that some societies thrived, but others faltered during the Little Ice Age. In particular, the Little Ice Age transformed environments around the Dutch Republic, the precursor to the Netherlands,  and made them 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 Dutch Republic therefore owed much to its people's flexibility in coping with the changing climate.[40]

Cultural responses

Historians have argued that cultural responses to the consequences of the Little Ice Age in Europe consisted of violent scapegoating.[41][42][43][39][44] The prolonged cold, dry periods brought drought upon many European communities and resulted in poor crop growth, poor livestock survival, and increased activity of pathogens and disease vectors.[45] Disease tends to intensify under the same conditions that unemployment and economic difficulties arise: prolonged cold, dry seasons. Disease and unemployment are outcomes that enhance each other and generate a lethal positive feedback loop.[45] Although the communities had some contingency plans, such as better crop mixes, emergency grain stocks, and international food trade, they did not always prove effective.[41] Communities often lashed out via violent crimes, including robbery and murder. Also, accusations of sexual offenses increased, such as adultery, bestiality, and rape.[42] Europeans sought explanations for the famine, disease, and social unrest that they were experiencing, and they blamed the innocent. Evidence from several studies indicate that increases in violent actions against marginalized groups, which were held responsible for the Little Ice Age, overlap with the years of particularly cold, dry weather.[43][39][41]

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). They argue that the resurgence was brought by the climatic decline. Prior to the Little Ice Age, "witchcraft" was considered an insignificant crime, and victims were rarely accused.[39] But beginning in the 1380s, just as the Little Ice Age began, European populations began to link magic and weather-making.[39] 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.[39] 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.[42] In general, the number of witchcraft trials rose as the temperature dropped, and trials decreased when temperature increased.[41][39] The peaks of witchcraft persecutions overlap with the hunger crises that occurred in 1570 and 1580, the latter lasting a decade.[39] The trials targeted primarily poor women, many of them widows. Not everybody agreed that witches should be persecuted for weather-making, but such arguments focused primarily not upon whether witches existed but upon whether witches had the capability to control the weather.[39][41] 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 people agreed with the idea that witches could control natural forces.[41]

Historians have argued that Jewish populations were also blamed for climatic deterioration during the Little Ice Age.[42][44] Christianity was the official religion in Western Europe, and its populations had a great degree of anti-Semitism.[42] There was no direct link made between Jews and weather conditions. Jews were blamed only for indirect consequences such as disease.[42] 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.[42] Rumors were spread that Jews were either poisoning wells themselves or conspiring against Christians by telling those with leprosy to poison the wells.[42] As a response to such violent scapegoating, Jewish communities sometimes converted to Christianity or migrated to the Ottoman Empire, Italy, or the Holy Roman Empire.[42]

Some populations blamed the cold periods and the resulting famine and disease during the Little Ice Age on a general divine displeasure.[43] Particular groups, however, took the brunt of the burden in attempts to cure it.[43] 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.[43] Other regulations affected the wider population, such as prohibiting dancing and sexual activities and moderating food and drink intake.[43]

In Ireland, Catholics blamed the Reformation for the bad weather. The Annals of Loch Cé, in its entry for 1588, describes a midsummer snowstorm as "a wild apple was not larger than each stone of it" and blames it on the presence of a "wicked, heretical, bishop in Oilfinn," the Protestant Bishop of Elphin, John Lynch.[46][47]

Depictions of winter in European painting

William James Burroughs analyses the depiction of winter in paintings, as does Hans Neuberger.[48] 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."[49] 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 that show 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 in 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, particularly stormy seascapes, became artistic genres in the Dutch Republic during the coldest and stormiest decades of the Little Ice Age. While the Little Ice Age was at its height, Dutch observations and reconstructions of similar past weather caused artists to paint local manifestations of a cooler, stormier climate consciously. That was a break from European conventions, as Dutch paintings and realistic landscapes depicted scenes from everyday life. Most modern scholars believe them to be full of symbolic messages and metaphors, which would have been clear to contemporary customers.[50]

All of the famous winter landscape paintings by Pieter Brueghel the Elder, such as The Hunters in the Snow, are 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...."[49][51]

Winter landscape with iceskaters, c. 1608, Hendrick Avercamp

Burroughs says that snowy subjects return to Dutch Golden Age painting with works by Hendrick Avercamp from 1609 onwards. There is a hiatus between 1627 and 1640, which is before the main period of such subjects from the 1640s to the 1660s. That 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.[49]

Neuberger analysed 12,000 paintings, held in American and European museums and dated between 1400 and 1967, for cloudiness and darkness.[48] His 1970 publication shows an increase in such depictions that corresponds to the Little Ice Age,[48] which peaks between 1600 and 1649.[52]

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.[53] For 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.[54]

General Crisis of the Seventeenth Century

The General Crisis of the Seventeenth Century in Europe was a period of inclement weather, crop failure, economic hardship, extreme intergroup 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).[55] The war started as a war of succession to the Bohemian throne. Animosity between Protestants and Catholics in the Holy Roman Empire (now Germany) added fuel to the fire. It soon escalated to a huge conflict that involved all of the major European powers and devastated much of Germany. When the war ended, some regions of the Holy Roman Empire had seen their population drop by as much as 70%.[56] However, 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. That paved 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) and made life even more comfortable.[57]

North America

"February" from the calendar of Les Très Riches Heures du duc de Berry, 1412–1416

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 meanwhile reported in the Jamestown, Virginia, settlement.[31] Native Americans formed leagues in response to food shortages.[30] 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.[58] In the winter of 1780, New York Harbor froze, which allowed 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.[59] In Glacier National Park, the last episode of glacier advance came in the late 18th and the early 19th centuries.[60] In 1879, the famed naturalist John Muir found that Glacier Bay ice had retreated 48 miles (77 km). In Chesapeake Bay, Maryland, large temperature excursions were possibly related to changes in the strength of North Atlantic thermohaline circulation.[61]

Because the Little Ice Age took place during the European colonization of the Americas, it threw off a lot of the early colonizers, who 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 in Europe. That effect was aggravated by the Little Ice Age, and unpreparedness led to the collapse of many early European settlements in North America.

When colonizers settled at Jamestown, historians agree it was one of the coldest time periods in the last 1000 years. Drought was also a huge problem in North America during the Little Ice Age, and the settlers arrived in Roanoke during 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. The times of drought also decreased the Native American populations and led to conflict because of food scarcity. English colonists at Roanoke forced Native Americans of Ossomocomuck to share their depleted supplies with them. That 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 parasites brought by Europeans in mosquitoes develop faster. That in turn led to many deaths among Native American populations from malaria.[62]

In 1642, Thomas Gorges wrote that between 1637 and 1645, colonists in Maine, then in Massachusetts, had horrendous weather conditions. In June 1637, it was so hot that European newcomers were dying in the heat, and travelers had to travel at night to stay cool enough. Gorges also wrote that the winter of 1641–1642 was “piercingly Intolerable” and that no Englishman or Native American had ever seen anything like it. He also stated that the Massachusetts Bay had frozen as far as one could see and that horse carriages now roamed where ships used to be. He stated that the summers of 1638 and 1639 were very short, cold, and wet, which compounded food scarcity for a few years. To make matters worse, creatures like caterpillars and pigeons fed on crops and devastated harvests. Every year about which Gorges wrote had unusual weather patterns noted, including high precipitation, drought, and extreme cold or extreme heat. All of them were byproducts of the Little Ice Age.[63]

Many of the people living in North America had their own theories for the weather being so poor. The colonist Ferdinando Gorges blamed the cold weather on cold ocean winds. Humphrey Gilbert tried to explain Newfoundland's extremely cold and foggy weather by saying that the Earth drew cold vapors from the ocean and drew them west. Dozens of others had their own theories for North America being so much colder than Europe, but their observations and hypotheses allow much to be known on the Little Ice Age’s effects in North America.[64]


An analysis of several climate proxies undertaken in Mexico's Yucatán Peninsula, which was 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.[65]

Another study conducted in several sites in Mesoamerica like Los Tuxtlas and Lake Pompal in Veracruz, Mexico show a decrease in human activity in the area during the Little Ice Age. That was proven by studying charcoal fragments and the amount of maize pollen taken from sedimentary samples by using a nonrotatory piston corer. The samples also showed volcanic activity which caused forest regeneration between 650 and 800. The instances of volcanic activity near Lake Pompal indicate varying temperatures, not a continuous coldness, during the Little Ice Age in Mesoamerica.[66]

Atlantic Ocean

In the North Atlantic, sediments accumulated since the end of the last ice age, which occurred 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 that recur every 1,500 years or so.[67] The most recent cooling event was the Little Ice Age. The same cooling events are detected in sediments accumulating off Africa, but the cooling events appear to be larger: 3–8 °C (6–14 °F).[68]


Although the original designation of a Little Ice Age referred to the reduced temperature of Europe and North America, there is some evidence of extended periods of cooling outside those regions although it is not clear whether they are related or independent events. Mann states:[4]

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.[69] 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).[70] Scholars have argued that one of the reasons for the fall of the Ming dynasty may have been the droughts and famines that were caused by the Little Ice Age.[71]

There are debates on the start date and the time periods of Little Ice Age's effects. Most scholars agree on categorizing the Little Ice Age period into three distinct cold periods: in 1458–1552, 1600–1720, and 1840–1880.[72] 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 to 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 from 1620 to 1749.[73]

The temperature changes was unprecedented for the farming communities in China. According to Dr. Coching Chu's 1972 study, the Little Ice Age from the end of the Ming dynasty to the start of the Qing dynasty (1650–1700) was one of the coldest periods in recorded Chinese history.[74] Many major droughts during the summer months were recorded, and significant freezing events occurred during the winter months. That greatly worsened the food supply during the Ming dynasty.

This period of Little Ice Age would correspond to the period's major historical events. The Jurchen people lived in Northern China and formed a tributary state to the Ming dynasty and its Wanli Emperor. From 1573 to 1620, Manchuria experienced famine caused by extreme snowfall, which depleted agriculture production and decimated the livestock population. Scholars have argued that it had been caused by the temperature drops during Little Ice Age. Despite the lack of food production, the Wanli Emperor ordered the Jurchens to pay the same amount of tribute each year. That led to anger and sowed seeds to the rebellion against the Ming dynasty. 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 dynasty's military such as during the 1618 Battle of Fushun.[75]

After the earlier defeats and the death of the Wanli Emperor, the Chongzhen Emperor took over China and continued the war effort. From 1632 to 1641, the Little Ice Age began to cause drastic climate changes in the Ming dynasty's territories. For example, rainfall in the Huabei region dropped by 11% to 47% from the historical average. Meanwhile, the Shaanbei region, along the Yellow River experienced six major floods, which ruined cities such as Yan’an. The climate factored heavily in weakening the government’s control over China and accelerated the fall of the Ming dynasty. In 1644, Li Zicheng led the Later Jin's forces into Beijing, overthrew the Ming dynasty, and established the Qing dynasty.[76]

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 the Kangxi Emperor (1661–1722), most Qing territories were still much colder than the historical average. However, the Kangxi Emperor pushed reforms and managed to increase the socio-economic recovery from the natural disasters. He benefited partly from the peacefulness of the early Qing dynasty. That essentially marked the end of the Little Ice Age in China and led to a more prosperous era of Chinese history that is known as the High Qing era.[77]

In the Himalayas, the general assumption is that the cooling events were synchronous with those in Europe during the Little Ice Age because of the characteristics of moraines. However, applications of Quaternary dating methods such as surface exposure dating have showed that glacial maxima occurred between 1300 and 1600, slightly earlier than the recorded coldest period in Northern Hemisphere. Many large Himalayan glacial debris fields have remained close to their limits since the Little Ice Age. The Himalayas also experienced an increase in snowfall at higher altitudes, which results 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.[78]

In Pakistan, the Balochistan is a province that became colder, and its native Baloch people started a mass migration and began to settle along the Indus River in Sindh and Punjab Provinces.[79]


The Little Ice Age has been clearly shown to have influenced the African climate from the 14th to the 19th centuries.[80] Despite variances throughout the continent, a general trend of declining temperatures in Africa led to an average cooling of 1 °C.[81]

In Ethiopia and North Africa, permanent snow was reported on mountain peaks at levels at which it does not occur today.[69] Timbuktu, an important city on the trans-Saharan caravan route, was flooded at least 13 times by the Niger River, but there are no records of similar flooding before or since that time.[69]

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, which "further support, and extend, the global expanse of the Little Ice Age."[82] 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."[83] The δ18O stalagmite record temperature reconstruction over a 350-year period (1690–1740) suggests that South Africa may have been the coldest region in Africa and have cooled by as much as 1.4 °C in summer.[84] Also, the solar magnetic and Niño-Southern Oscillation cycles 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.[85] Another archaeological reconstruction of South Africa reveals the rise of the Great Zimbabwe people because of ecological advantages from the increased rainfall over other competitor societies, such as the Mupungubwe people.[86]

Other than temperature variability, data from equatorial East Africa suggest impacts to the hydrologic cycle in the late 1700s. Historical data reconstructions from ten major African lakes indicate that an episode of “drought and desiccation” occurred throughout East Africa.[87] The period showed drastic reductions in the depths of lakes, which were transformed into desiccated puddles. It is very likely that locals could cross Lake Chad, among others, and that bouts of “intense droughts were ubiquitous.” That indicates local societies were probably launched into long migrations and warfare with neighboring tribes since agriculture was made virtually useless by the dry soil.


CO2 mixing ratios at Law Dome

Kreutz et al. (1997) compared results from studies of West Antarctic ice cores with the Greenland Ice Sheet Project Two GISP2; they suggested a synchronous global cooling.[88] An ocean sediment core from the eastern Bransfield Basin in the Antarctic Peninsula shows centennial events, which the authors link to the Little Ice Age and to the Medieval Warm Period.[89] The authors note that "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 Little Ice Age is the most dramatic climate event in the SD Holocene glaciochemical record.[90] 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.[91] Law Dome ice cores show lower levels of CO2 mixing ratios from 1550 to 1800, which Etheridge and Steele believe to be "probably as a result of colder global climate."[92]

Sediment cores in Bransfield Basin, Antarctic Peninsula, have neoglacial indicators by diatom and sea-ice taxa variations during the Little Ice Age.[93] Stable isotope records from the Mount Erebus Saddle ice core site suggests that the Ross Sea region experienced average temperatures 1.6 ± 1.4 °C cooler during the Little Ice Age than the last 150 years.[94]

Australia and New Zealand

Its location in the Southern Hemisphere made Australia not experience a regional cooling like that of Europe or North America. Instead, the Australian Little Ice Age was characterized by humid, rainy climates, which were followed by drying and aridification in the 19th century.[95]

As studied by Tibby et al. (2018), lake records from Victoria, New South Wales, and Queensland suggest that conditions in the east and the south-east of Australia were wet and unusually cool from the 16th to the early 19th centuries. That corresponds with the “peak” of the global Little Ice Age from 1594 to 1722. For example, the Swallow Lagoon rainfall record indicates that from c. 1500–1850, there was significant and consistent rainfall, which sometimes exceeded 300 mm.[95] The rainfalls significantly reduced after around 1890. Similarly, the hydrological records of Lake Surprise’s salinity levels reveal high humidity levels around from 1440 to 1880, and an increase in salinity from 1860 to 1880 points to a negative change to the once-humid climate.[96] The mid-19th century marked a notable change to eastern Australia’s rainfall and humidity patterns.

Tibby et al. (2018) note that in eastern Australia, the paleoclimatic changes of the Little Ice Age in the late 1800s coincided with the agricultural changes resulting from European colonization. After the 1788 establishment of British colonies in the Australia, which were concentrated primarily in the eastern regions and cities like Sydney and later Melbourne and Brisbane, the British introduced new agricultural practices like pastoralism.[95] Such practices required widespread deforestation and clearance of vegetation. Pastoralism and the clearing of land are captured in works of art such as the 1833 painting by the prominent landscape artist John Glover Patterdale Landscape with Cattle.

Patterdale Landscape with Cattle (1833) by John Glover depicts agricultural practices like pastoralism, which contributed to the aridification of Australia's late Little Ice Age.

Over the next century, the deforestation led to a loss of biodiversity, wind and water-based soil erosion, and soil salinity.[97] Furthermore, as argued by Gordan et al. (2003), such land and vegetation clearance in Australia resulted in a 10% reduction in the transport of water vapor to the atmosphere. That occurred in Western Australia as well, where 19th-century land clearing resulted in reduced rainfall over the region.[98] By 1850 to 1890, those human agricultural practices, which were concentrated in eastern Australia, had 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 rainfall similar to today but with less variability. A study that analyzed isotopes in Great Barrier Reef corals suggested that increased water vapor transport from the southern tropical oceans to the poles contributed to the Little Ice Age.[99] Borehole reconstructions from Australia suggest that over the last 500 years, the 17th century was the coldest on the continent.[100] 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, which further proves that Australia did not reach the same depths of cooling as the continents in 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. That was one of the few cases of a glacier thrusting into a rainforest.[101] 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.[102] 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 and 1730.[103]

Pacific Islands

Sea-level data for the Pacific Islands suggest that sea level in the region fell, possibly in two stages, between 1270 and 1475. That was associated with a 1.5 °C fall in temperature, as determined from oxygen-isotope analysis, and an observed increase in the frequency of El Niño.[104] Tropical Pacific coral records indicate the most frequent and intense El Niño-Southern Oscillation activity was in the mid-17th century.[105] Foraminiferald 18 O records indicate that the Indo-Pacific Warm Pool was warm and saline between 1000 and 1400, with temperatures approximating current conditions, but that it cooled from 1400 onwards and reached its lowest temperatures in 1700. That is consistent with the transition from the mid-Holocene warming to the Little Ice Age.[106] The nearby Southwestern Pacific, however, experienced warmer-than-average conditions over the course of the Little Ice Age, which is thought to be from the increased trade winds, which increased the evaporation and the salinity in the region. The dramatic temperature differences between the higher latitudes and the equator are thought to have resulted in drier conditions in the subtropics.[107] 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 that led to drought. The first occurred between 500 and 1200, and the second occurring during the Little Ice Age from 1570 to 1720.[108] In between both arid phases, the island enjoyed a humid period from 1200 to 1570. That coincided with the peak of the Rapa Nui civilization.[109]

South America

Tree-ring data from Patagonia show cold episodes from 1270 and 1380 and from 1520 to 1670, during the events in the Northern Hemisphere.[110][111] 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.[112] A 2009 paper details cooler and wetter conditions in southeastern South America between 1550 and 1800 by citing evidence obtained via several proxies and models.[113] 18O records from three Andean ice cores show a cool period from 1600 to 1800.[114]

Although it is only anecdotal evidence, the Antonio de Vea expedition entered San Rafael Lagoon in 1675 through Río Témpanos (Spanish for "Ice Floe River"). The Spanish mentioned no ice floe but stated 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 and noticed 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."[115] As of 2001, the borders of the glacier had significantly retreated from those of 1675.[115]

Possible causes

Scientists have tentatively identified seven possible causes of the Little Ice Age: orbital cycles, decreased solar activity, increased volcanic activity, altered ocean current flows,[116] fluctuations in the human population in different parts of the world causing reforestation or deforestation, and the inherent variability of global climate.

Orbital cycles

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, which continued through the Middle Ages and the Little Ice Age. The rate of Arctic cooling is roughly 0.02 °C per century.[117] That trend could be extrapolated to continue into the future and possibly lead to a full ice age, but the 20th-century instrumental temperature record shows a sudden reversal of that trend, with a rise in global temperatures attributed to greenhouse gas emissions.[117]

Solar activity

The Maunder minimum in a 400-year history of sunspot numbers
Solar activity events recorded in radiocarbon

Solar activity includes any sun disturbances like sunspots, solar flares, or prominences, and scientists can track those solar activities in the past by analyzing both the carbon-14 or beryllium-10 isotopes in items like tree rings. Those solar activities are not the most common or noticeable causes for the Little Ice Age, but they provide considerable evidence that they played a part in its formation and the increase in temperature after the period. From 1450 to 1850, there were very low recorded levels of solar activity in the Spörer, Maunder, and Dalton minima.

The Spörer minimum lasted from 1450 and 1550, when the Little Ice Age started. A study by Dmitri Mauquoy et al. found that at the beginning of Spörer, the percentage of change of carbon-14 skyrocketed to about 10%.[citation needed] That stayed quite common for the entire duration of the Spörer minimum, but around 1600, it dropped rapidly before the Maunder (1645–1715), when it rose again to a little under 10%. To put that into perspective, the change during standard periods of carbon-14 idles between -5% to 5% and so that is a considerable change. At the end of the Little Ice Age, which is also the Dalton minimum (1790–1830), the change was normal, at around -1%. Those changes in carbon-14 have a strong relationship with the temperature because during all three periods, an increase in the carbon-14 correlates with cold temperatures during the Little Ice Age.[118]

In a study by Judith Lean, she notes the relationship between the sun and the that helped form the Little Ice Age. Her research found that for a certain period, there was a 0.13% solar irradiance increased the temperature of the earth by 0.3 °C. That was around 1650–1790 and can help 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, they found an average coefficient of .79, which shows a strong relationship between the two components and is evidence that the Little Lce Age was considerably cold and had very low solar activity. Lean's team also formulated an equation in which the temperature Change is -168.802+Sx0.123426. That equals turns out to a 0.16 °C increase in temperature for every 0.1% increase in solar irradiance.[119]

In summary, the entire length of the Little Ice Age had a large change in carbon-14 and a low solar irradiance. Both show a strong relationship to the cold temperatures during the time. Solar activity remains important to the whole picture of climate change and affects the Earth even if the change is less than 1 °C over a few hundred years.

Volcanic activity

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."[7]

Throughout the Little Ice Age, the world experienced heightened volcanic activity.[120] 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, which leads to worldwide cooling for up to two years after an eruption. Also emitted by eruptions is sulfur in the form of sulfur dioxide. When sulfur dioxide reaches the stratosphere, the gas turns into sulfuric acid particles, which reflect the sun's rays. That further reduces the amount of radiation reaching the 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. That may have caused the initial cooling, and the 1452–1453 eruption of Kuwae in Vanuatu triggered a second pulse of cooling.[7] 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 (c. 1580), Huaynaputina (1600), Mount Parker (1641), Long Island (Papua New Guinea) (ca. 1660), and Laki (1783).[26] The 1815 eruption of Tambora, also in Indonesia, blanketed the atmosphere with ash, and the following year came to be known as the Year Without a Summer,[121] when frost and snow were reported in June and July in both New England and Northern Europe.

Ocean circulation

Thermohaline circulation or Oceanic conveyor belt illustrated

Another possibility is that there was a slowing of thermohaline circulation.[59][116][122][123] The circulation could have been interrupted by the introduction of a large amount of fresh water into the North Atlantic and might have caused by a period of warming before the Little Ice Age that is known as the Medieval Warm Period.[38][124][125] There is some concern that a shutdown of thermohaline circulation could happen again as a result of the present warming period.[126][127]

Decreased human populations

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 that impact and led to a cooling trend.

The Black Death is estimated to have killed 30% to 60% of the European population.[128] In total, the plague may have reduced the world population from an estimated 475 million to 350–375 million in the 14th century.[129] It took 200 years for the world population to recover to its previous level.[130] William Ruddiman proposed that those large population reductions in Europe, East Asia, and the Middle East caused a decrease in agricultural activity. Ruddiman suggests reforestation took place and allowed 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 occurred in the 16th century could have had a similar effect.[131][132] Other researchers have supported depopulation in the Americas as a factor and have asserted that humans cleared considerable amounts of forest to support agriculture in the Americas before the arrival of Europeans brought on a population collapse.[133][134] 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 also that human-set fires played a central role in reducing biomass in Amazonian and Central American forests before the arrival of the Europeans and the concomitant spread of diseases during the Columbian exchange.[135][136][137] 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.[136] Brierley conjectured that the European arrival in the Americas caused mass deaths from epidemic disease, which caused much abandonment of farmland. That caused much forest to return, which sequestered greater levels of carbon dioxide.[13] 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.[138] The depopulation is linked to a drop in carbon dioxide levels observed at Law Dome, Antarctica.[133] 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 by allowing for the return of carbon-absorbing forest in cultivated land.[139][140]

Population increases at mid- to high-latitudes

It is suggested that during the Little Ice Age, increased deforestation had a significant enough effect on the Earth's albedo (reflectiveness) to cause regional and global temperatures decreases. Changes in albedo were caused by widespread deforestation at high latitude and so exposed more snow cover to and increased reflectiveness of the Earth's surface, as land was cleared for agricultural use. The 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.[141]

It has been proposed that the Land Use Intensification theory could explain the phenomenon. The theory was originally proposed by Ester Boserup and suggests that agriculture advances only as the population demands it.[142] Furthermore, there is evidence of rapid population and agricultural expansion, which 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 those regions. That has led to an inability to rely on data to explain sweeping changes or to 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.[143] That is, climate models have shown deforestation as neither a singular cause for climate change nor a reliable cause for the global temperature decrease.

Inherent variability of climate

Spontaneous fluctuations in global climate might explain the 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 the use of 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.[144] Two studies have concluded that the demonstrated inherent variability was not great enough to account for the Little Ice Age.[144][145] The severe winters of 1770 to 1772 in Europe, however, have been attributed to an anomaly in the North Atlantic oscillation.[146]

See also


  1. ^ Hawkins, Ed (30 January 2020). "2019 years". Archived from the original on 2 February 2020. ("The data show that the modern period is very different to what occurred in the past. The often quoted Medieval Warm Period and Little Ice Age are real phenomena, but small compared to the recent changes.")
  2. ^ Ladurie, Emmanuel Le Roy (1971). Times of Feast, Times of Famine: a History of Climate Since the Year 1000. Barbara Bray. Garden City, NY: Doubleday. ISBN 978-0-374-52122-6. OCLC 164590.
  3. ^ Matthes, François E. (1939). "Report of Committee on Glaciers, April 1939". Transactions, American Geophysical Union. 20 (4): 518. Bibcode:1939TrAGU..20..518M. doi:10.1029/TR020i004p00518. Matthes described glaciers in the Sierra Nevada of California that he believed could not have survived the hypsithermal; his usage of "Little Ice Age" has been superseded by "Neoglaciation".
  4. ^ a b Mann, Michael (2003). "Little Ice Age" (PDF). In Michael C MacCracken; John S Perry (eds.). Encyclopedia of Global Environmental Change, Volume 1, The Earth System: Physical and Chemical Dimensions of Global Environmental Change. John Wiley & Sons. Retrieved 17 November 2012.
  5. ^ Lamb, HH (1972). "The cold Little Ice Age climate of about 1550 to 1800". Climate: present, past and future. London: Methuen. p. 107. CiteSeerX ISBN 978-0-416-11530-7. (noted in Grove 2004:4).
  6. ^ a b "Earth observatory Glossary L-N". NASA Goddard Space Flight Center, Green Belt MD: NASA. Retrieved 17 July 2015. Cite journal requires |journal= (help)
  7. ^ a b c d e Miller, Gifford H.; Geirsdóttir, Áslaug; Zhong, Yafang; Larsen, Darren J.; Otto-Bliesner, Bette L.; Holland, Marika M.; Bailey, David A.; Refsnider, Kurt A.; Lehman, Scott J.; Southon, John R.; Anderson, Chance; Björnsson, Helgi; Thordarson, Thorvaldur (2012). "Abrupt onset of the Little Ice Age triggered by volcanism and sustained by sea-ice/ocean feedbacks". Geophysical Research Letters. 39 (2): n/a. Bibcode:2012GeoRL..39.2708M. CiteSeerX doi:10.1029/2011GL050168. Lay summary – Science Daily (30 January 2012).
  8. ^ Grove, J.M., Little Ice Ages: Ancient and Modern, Routledge, London (2 volumes) 2004.
  9. ^ Matthews, John A.; Briffa, Keith R. (2005). "The 'little ice age': Re‐evaluation of an evolving concept". Geografiska Annaler: Series A, Physical Geography. 87: 17–36. doi:10.1111/j.0435-3676.2005.00242.x. S2CID 4832081.
  10. ^ "1.4.3 Solar Variability and the Total Solar Irradiance – AR4 WGI Chapter 1: Historical Overview of Climate Change Science". Retrieved 24 June 2013.
  11. ^ a b "Climate Change 2001: The Scientific Basis". UNEP/GRID-Arendal. Archived from the original on 29 May 2006. Retrieved 2 August 2007.
  12. ^ "New Zealand study reveals temperature could be key to predicting volcanic eruptions". NZ Herald. Retrieved 31 October 2021.
  13. ^ a b Koch, Alexander; Brierley, Chris; Maslin, Mark M.; Lewis, Simon L. (2019). "Earth system impacts of the European arrival and Great Dying in the Americas after 1492". Quaternary Science Reviews. 207: 13–36. Bibcode:2019QSRv..207...13K. doi:10.1016/j.quascirev.2018.12.004.
  14. ^ AR4 WG1 Section 6.6: The Last 2,000 Years, 2007.
  15. ^ Jones, Philip D. (2001). History and climate: memories of the future?. Springer. p. 154.[ISBN missing]
  16. ^ According to JM Lamb of Cambridge University, the Little Ice Age was already underway in Canada and Switzerland and in the wider North Atlantic region in the 13th and the 14th centuries.
  17. ^ "Worldwide glacier retreat". RealClimate. Retrieved 2 August 2007.
  18. ^ Oerlemans, J. (2005). "Extracting a Climate Signal from 169 Glacier Records". Science. 308 (5722): 675–77. Bibcode:2005Sci...308..675O. doi:10.1126/science.1107046. PMID 15746388. S2CID 26585604.
  19. ^ Jonathan Amos (30 September 2013). "Mystery 13th Century eruption traced to Lombok, Indonesia". BBC. The mystery event in 1257 was so large its chemical signature is recorded in the ice of both the Arctic and the Antarctic. European medieval texts talk of a sudden cooling of the climate, and of failed harvests.
  20. ^ Dagamar Degroot, 'Did the Spanish Empire Change Earth's Climate?' (2016)
  21. ^ Hendy, Erica J.; Gagan, Michael K.; Alibert, Chantal A.; McCulloch, Malcolm T.; Lough, Janice M.; Isdale, Peter J. (2002). "Abrupt Decrease in Tropical Pacific Sea Surface Salinity at End of Little Ice Age". Science. 295 (5559): 1511–14. Bibcode:2002Sci...295.1511H. doi:10.1126/science.1067693. PMID 11859191. S2CID 25698190.
  22. ^ Ogilvie, A.E.J.; Jónsson, T. (2001). "'Little Ice Age' Research: A Perspective from Iceland". Climatic Change. 48: 9–52. doi:10.1023/A:1005625729889. S2CID 189870320.
  23. ^ S.C. Porter. "Anout; Quaternary Science". INQUA. Archived from the original on 15 April 2010. Retrieved 6 May 2010.
  24. ^ "AR6 Climate Change 2021: The Physical Science Basis — IPCC".
  25. ^ Meacham, Jon (7 May 2020). "Pandemics of the Past". The New York Times. ISSN 0362-4331. Retrieved 8 May 2020.
  26. ^ a b c Jonathan Cowie (2007). Climate change: biological and human aspects. Cambridge University Press. p. 164. ISBN 978-0-521-69619-7.
  27. ^ Davies, Caroline (12 February 2021). "Part of River Thames freezes amid sub-zero temperatures". The Guardian. Retrieved 12 February 2021.
  28. ^ Stone, R. (2004). "Volcanology: Iceland's Doomsday Scenario?". Science. 306 (5700): 1278–81. doi:10.1126/science.306.5700.1278. PMID 15550636. S2CID 161557686.
  29. ^ "What Did They Eat? – Icelandic food from the Settlement through the Middle Ages". Archived from the original on 20 February 2012.
  30. ^ a b "SVS Science Story: Ice Age". NASA Scientific Visualization Studio. Retrieved 2 August 2007.
  31. ^ a b c Lamb, Hubert H. (1995). "The little ice age". Climate, history and the modern world. London: Routledge. pp. 211–41. ISBN 978-0-415-12734-9.
  32. ^ "Arquivo de eventos históricos – Página 4 – – Fórum de Meteorologia". 17 July 2012. Retrieved 24 June 2013.
  33. ^ Jones, Evan T.; Hewlett, Rose; Mackay, Anson W. (5 May 2021). "Weird weather in Bristol during the Grindelwald Fluctuation (1560–1630)". Weather. 76 (4): 104–10. Bibcode:2021Wthr...76..104J. doi:10.1002/wea.3846. S2CID 225239334 – via Wiley Online Library.
  34. ^ Cullen, Karen J. (2010). Famine in Scotland: The 'Ill Years' of The 1690s. Edinburgh University Press. p. 20. ISBN 978-0-7486-3887-1.
  35. ^ Ewanu, Elizabeth; Nugent, Janay (2008). Finding the Family in Medieval and Early Modern Scotland. Ashgate. p. 153. ISBN 978-0-7546-6049-1.
  36. ^ Whitehouse, David (17 December 2003). "Stradivarius' sound 'due to Sun'". BBC.
  37. ^ Burke, James (21 September 1978). "Thunder in the Skies". Connections. BBC.
  38. ^ a b Fagan 2001
  39. ^ a b c d e f g h i Behringer, Wolfgang (1999). "Climatic change and witch-hunting: the impact of the Little Ice Age on mentalities". Climatic Change. 43: 335–51. doi:10.1023/A:1005554519604. S2CID 189869470.
  40. ^ Dagomar Degroot, The Frigid Golden Age: Climate Change, the Little Ice Age, and the Dutch Republic, 1560–1720 (New York: Cambridge University Press, 2018) ISBN 978-1108419314[page needed]
  41. ^ a b c d e f Oster, Emily (2004). "Witchcraft, weather and economic growth in Renaissance Europe". The Journal of Economic Perspectives. 18 (1): 215–28. CiteSeerX doi:10.1257/089533004773563502. JSTOR 3216882. S2CID 22483025. SSRN 522403.
  42. ^ a b c d e f g h i Behringer, Wolfgang (2009). "Cultural Consequences of the Little Ice Age". A Cultural History of Climate. Wiley. pp. 121–67. ISBN 978-0-745-64529-2.
  43. ^ a b c d e f Parker, Geoffrey (2013). "The Little Ice Age". Global Crisis: War, Climate Change, & Catastrophe in the Seventeenth Century. Yale University Press. pp. 3–25. ISBN 978-0-300-20863-4.
  44. ^ a b Lehmann, Hartmut (1988). "The Persecution of Witches as Restoration of Order: The Case of Germany, 1590s–1650s". Central European History. 21 (2): 107–21. doi:10.1017/S000893890001270X.
  45. ^ a b Post, John D. (1984). "Climatic Variability and the European Mortality Wave of the Early 1740s". The Journal of Interdisciplinary History. 15 (1): 1–30. doi:10.2307/203592. JSTOR 203592. PMID 11617361.
  46. ^ "Part 12 of Annals of Loch Cé". Corpus of Electronic Texts. University College Cork.
  47. ^ Meigs, Samantha A. (1997). Reformations in Ireland: Tradition and Confessionalism, 1400–1690. Springer. ISBN 978-1349257102 – via Google Books.
  48. ^ a b c Macdougall, Douglas (2004). Frozen Earth: The Once and Future Story of Ice Ages. University of California Press. p. 225. ISBN 978-0-520-24824-3.
  49. ^ a b c Huddart, David; Stott, Tim (2010). Earth Environments: Past, Present and Future. Wiley. p. 863. ISBN 978-0-470-74960-9.
  50. ^ Dagomar Degroot (2018). The Frigid Golden Age: Climate Change, the Little Ice Age, and the Dutch Republic, 1560–1720. New York: Cambridge University Press. ISBN 978-1108419314.[page needed]
  51. ^ Burroughs, William (18 December 1980). "New Scientist". New Scientist Careers Guide : The Employer Contacts Book for Scientists. Reed Business Information: 768–. ISSN 0262-4079. 1980 article in the New Scientist
  52. ^ John E. Thornes; John Constable (1999). John Constable's skies: a fusion of art and science. Continuum International. p. 32. ISBN 978-1-902459-02-8.
  53. ^ "Kilsyth Curling". Retrieved 11 September 2010.
  54. ^ "The Story so Far!!!". Gourock Curling Club. 2009. Archived from the original on 25 April 2012. Retrieved 11 September 2010.
  55. ^ Zhang, David D.; Lee, Harry F.; Wang, Cong; Li, Baosheng; Pei, Qing; Zhang, Jane; An, Yulun (18 October 2011). "The causality analysis of climate change and large-scale human crisis". Proceedings of the National Academy of Sciences of the United States of America. 108 (42): 17296–301. doi:10.1073/pnas.1104268108. PMC 3198350. PMID 21969578.
  56. ^ National Geographic (2007). Essential Visual History of the World. National Geographic Society. pp. 190–91. ISBN 978-1-4262-0091-5.
  57. ^ Dutton, Edward; Woodley of Menie, Michael (2018). "Chapter 10: Does This Mean that Civilizations Always Rise and Fall?". At Our Wits' End: Why We're Becoming Less Intelligent and What It Means for the Future. Exeter, United Kingdom: Imprint Academic. ISBN 978-1845409852.
  58. ^ Kenyon W.A.; Turnbull J.R. (1971). The Battle for James Bay. Toronto: Macmillan Company of Canada Limited.
  59. ^ a b Broecker, Wallace S. (2000). "Was a change in thermohaline circulation responsible for the Little Ice Age?". Proceedings of the National Academy of Sciences. 97 (4): 1339–42. Bibcode:2000PNAS...97.1339B. doi:10.1073/pnas.97.4.1339. JSTOR 121471. PMC 34299. PMID 10677462.
  60. ^ "Ice Ages". National Park Service. Archived from the original on 12 April 2005.
  61. ^ Cronin, T. M.; Dwyer, G. S.; Kamiya, T.; Schwede, S.; Willard, D. A. (2003). "Medieval Warm Period, Little Ice Age and 20th century temperature variability from Chesapeake Bay" (PDF). Global and Planetary Change. 36 (1): 17. Bibcode:2003GPC....36...17C. doi:10.1016/S0921-8181(02)00161-3. hdl:10161/6578.
  62. ^ Wolfe, Brendan (7 December 2020). "Little Ice Age and Colonial Virginia". The Encyclopedia Virginia. Retrieved 26 May 2021.
  63. ^ "Climate and Mastery of the Wilderness in Seventeenth-Century New England". Colonial Society of Massachusetts. Retrieved 26 May 2021.
  64. ^ White, Sam (2015). "Unpuzzling American Climate: New World Experience and the Foundations of a New Science". Isis. 106 (3): 544–66. doi:10.1086/683166. JSTOR 10.1086/683166. PMID 26685517. S2CID 37331690.
  65. ^ Hodell, David A.; Brenner, Mark; Curtis, Jason H.; Medina-González, Roger; Ildefonso-Chan Can, Enrique; Albornaz-Pat, Alma; Guilderson, Thomas P. (2005). "Climate change on the Yucatan Peninsula during the Little Ice Age". Quaternary Research. 63 (2): 109. Bibcode:2005QuRes..63..109H. doi:10.1016/j.yqres.2004.11.004. S2CID 129924750.
  66. ^ del Socorro Lozano-García, Ma.; Caballero, Margarita; Ortega, Beatriz; Rodríguez, Alejandro; Sosa, Susana (2007). "Tracing the effects of the Little Ice Age in the tropical lowlands of eastern Mesoamerica". Proceedings of the National Academy of Sciences. 104 (41): 16200–03. Bibcode:2007PNAS..10416200L. doi:10.1073/pnas.0707896104. PMC 2000453. PMID 17913875.
  67. ^ Bond et al., 1997[full citation needed]
  68. ^ "Abrupt Climate Changes Revisited: How Serious and How Likely?". USGCRP Seminar. US Global Change Research Program. 23 February 1998.
  69. ^ a b c Reiter, Paul (2000). "From Shakespeare to Defoe: Malaria in England in the Little Ice Age". Emerging Infectious Diseases. 6 (1): 1–11. doi:10.3201/eid0601.000101. PMC 2627969. PMID 10653562.
  70. ^ Liu, Kam-biu; Shen, Caiming; Louie, Kin-Sheun (2001). "A 1,000-Year History of Typhoon Landfalls in Guangdong, Southern China, Reconstructed from Chinese Historical Documentary Records". Annals of the Association of American Geographers. 91 (3): 453–64. doi:10.1111/0004-5608.00253. S2CID 53066209.
  71. ^ Fan, Ka-wai (2010). "Climatic change and dynastic cycles in Chinese history: A review essay". Climatic Change. 101 (3–4): 565–73. Bibcode:2010ClCh..101..565F. doi:10.1007/s10584-009-9702-3. S2CID 153997845.
  72. ^ Cai, Wenjuan; Yn, Shuyan (March 2009). "The freeze disasters in the Little Ice Age of Ming and Qing Dynasties in the Guanzhong Region". Journal of Arid Land Resources and Environment. College of Tourism and Environmental Sciences, Shaanxi Normal University. 23 (3): 119.
  73. ^ Zhang, Xian; Shao, Xiaohua; Wang, Tao (3 May 2013). "Regional Climate Characteristics in China during the Little Ice Age". Journal of Nanjing University of Information Science and Technology: Natural Science Edition. 4 (1): 317–25.
  74. ^ KeZhen, Zhu (January 1972). "中国近五千年来气候变迁的初步研究". Acta Archaeologica Sinica. 1 (1): 25.
  75. ^ Xiao, Jie; Zheng, Guozhang; Guo, Zhengsheng; Yan, Lisha (June 2018). "Climate change and social response during the heyday of the little ice age in the Ming and Qing dynasty". Journal of Arid Land Resources and Environment, College of Geography Science, Shanxi Normal University. 32 (6): 80. doi:10.13448/j.cnki.jalre.2018.176.
  76. ^ Yi, Shanming (May 2015). "明朝灭亡与"小冰期"". Journal of Social Science of the North China University of Water Conservancy and Electric Power. 1 (5): 3. Retrieved 5 May 2021.
  77. ^ Xiao, Lingbo, Xiuqi Fang, Jingyun Zheng, and Wanyi Zhao. “Famine, Migration and War: Comparison of Climate Change Impacts and Social Responses in North China between the Late Ming and Late Qing Dynasties.” Holocene 25, no. 6 (June 2015): 900–10. doi:10.1177/0959683615572851.
  78. ^ Rowan, Ann (1 February 2017). "The 'Little Ice Age' in the Himalaya: A review of glacier advance driven by Northern Hemisphere temperature change". The Holocene. 27 (2): 292–308. Bibcode:2017Holoc..27..292R. doi:10.1177/0959683616658530. S2CID 55253587. Retrieved 6 May 2021.
  79. ^ "From Zardaris to Makranis: How the Baloch came to Sindh". The Express Tribune. 28 March 2014.
  80. ^ Johnson, Thomas C.; Barry, Sylvia L.; Chan, Yvonne; Wilkinson, Paul (2001). <0083:drocvs>;2 "Decadal record of climate variability spanning the past 700 yr in the Southern Tropics of East Africa". Geology. 29 (1): 83. Bibcode:2001Geo....29...83J. doi:10.1130/0091-7613(2001)029<0083:drocvs>;2. ISSN 0091-7613.
  81. ^ Klein, Richard G. (December 2000). "The Earlier Stone Age of Southern Africa". The South African Archaeological Bulletin. 55 (172): 107–22. doi:10.2307/3888960. ISSN 0038-1969. JSTOR 3888960.
  82. ^ Johnson, Thomas C.; Barry, Sylvia L.; Chan, Yvonne; Wilkinson, Paul (2001). "Decadal record of climate variability spanning the past 700 yr in the Southern Tropics of East Africa". Geology. 29 (1): 83. Bibcode:2001Geo....29...83J. doi:10.1130/0091-7613(2001)029<0083:DROCVS>2.0.CO;2. S2CID 20364249.
  83. ^ Holmgren, K., Tyson, P.D., Moberg, A., Svanered, O. (2001). "A preliminary 3000-year regional temperature reconstruction for South Africa". South African Journal of Science. 97: 49–51. hdl:10520/EJC97278.CS1 maint: multiple names: authors list (link)
  84. ^ Sundqvist, H. S.; Holmgren, K.; Fohlmeister, J.; Zhang, Q.; Matthews, M. Bar; Spötl, C.; Körnich, H. (December 2013). "Evidence of a large cooling between 1690 and 1740 AD in southern Africa". Scientific Reports. 3 (1): 1767. Bibcode:2013NatSR...3E1767S. doi:10.1038/srep01767. ISSN 2045-2322. PMC 3642658.
  85. ^ MacKay, Anson W.; Bamford, Marion K.; Grab, Stefan W.; Fitchett, Jennifer M. (2016). "A multi-disciplinary review of late Quaternary palaeoclimates and environments for Lesotho". South African Journal of Science. 112. doi:10.17159/sajs.2016/20160045.
  86. ^ Huffman, Thomas N. (January 1996). "Archaeological evidence for climatic change during the last 2000 years in southern Africa". Quaternary International. 33: 55–60. Bibcode:1996QuInt..33...55H. doi:10.1016/1040-6182(95)00095-x. ISSN 1040-6182.
  87. ^ Nicholson, Sharon E.; Yin, Xungang (2001). "Rainfall Conditions in Equatorial East Africa during the Nineteenth Century as Inferred from the Record of Lake Victoria". Climatic Change. 48 (2/3): 387–98. doi:10.1023/a:1010736008362. ISSN 0165-0009. S2CID 130327434.
  88. ^ Kreutz, K. J. (1997). "Bipolar Changes in Atmospheric Circulation During the Little Ice Age". Science. 277 (5330): 1294–96. doi:10.1126/science.277.5330.1294. S2CID 129868172.
  89. ^ Khim, Boo-Keun; Yoon, Ho Il; Kang, Cheon Yun; Bahk, Jang Jun (2002). "Unstable Climate Oscillations during the Late Holocene in the Eastern Bransfield Basin, Antarctic Peninsula". Quaternary Research. 58 (3): 234. Bibcode:2002QuRes..58..234K. doi:10.1006/qres.2002.2371. S2CID 129384061.
  90. ^ "Siple Dome Glaciochemistry". Retrieved 4 October 2017.
  91. ^ Sarah B. Das; Richard B. Alley. "Clues to changing WAIS Holocene summer temperatures from variations in melt-layer frequency in the Siple Dome ice core". Archived from the original on 7 October 2006.
  92. ^ D.M. Etheridge; L.P. Steele; R.L. Langenfelds; R.J. Francey; J.-M. Barnola; V.I. Morgan. "Historical CO2 Records from the Law Dome DE08, DE08-2, and DSS Ice Cores". Carbon Dioxide Information Analysis Center. Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, Tenn. templatestyles stripmarker in |title= at position 33 (help)
  93. ^ Bárcena, M. Angeles; Gersonde, Rainer; Ledesma, Santiago; Fabrés, Joan; Calafat, Antonio M.; Canals, Miquel; Sierro, F. Javier; Flores, Jose A. (1998). "Record of Holocene glacial oscillations in Bransfield Basin as revealed by siliceous microfossil assemblages". Antarctic Science. 10 (3): 269. Bibcode:1998AntSc..10..269B. doi:10.1017/S0954102098000364.
  94. ^ Rhodes, R. H.; Bertler, N. A. N.; Baker, J. A.; Steen-Larsen, H. C.; Sneed, S. B.; Morgenstern, U.; Johnsen, S. J. (2012). "Little Ice Age climate and oceanic conditions of the Ross Sea, Antarctica from a coastal ice core record". Climate of the Past. 8 (4): 1223. Bibcode:2012CliPa...8.1223R. doi:10.5194/cp-8-1223-2012.
  95. ^ a b c Tibby, J; Tyler, JJ; Barr, C. “Post little ice age drying of eastern Australia conflates understanding of early settlement impacts.” Quaternary Science Reviews. Vol. 202 (15 December 2018): 45–54.
  96. ^ Mercer, D.; Marden, P. “Ecologically sustainable development in a 'quarry' economy: one step forward, two steps back.” Geogr. Res., 44 (2006): 183–202. doi:10.1111/j.1745-5871.2006.00376.x
  97. ^ Gordon, L; Dunlop, M; Foran, B. “Land cover change and water vapour flows: learning from Australia.” Phil. Trans. Biol. Sci., 385 (2003): 1973–84.
  98. ^ Nair, U.S; Wu, Y; Kala, J; Lyons, T.J; Peilke, R.A; Hacker, J.M. “The role of land use change on the development and evolution of the west coast trough, convective clouds, and precipitation in southwest Australia.” Journal of Geophysical Research: Atmospheres, 116 (2011): p. D7.
  99. ^ Hendy, Erica J.; Gagan, Michael K.; Alibert, Chantal A.; McCulloch, Malcolm T.; Lough, Janice M.; Isdale, Peter J. (2002). "Abrupt Decrease in Tropical Pacific Sea Surface Salinity at End of Little Ice Age." Science. 295 (5559): 1511–14. Bibcode:2002Sci...295.1511H. doi:10.1126/science.1067693. PMID 11859191. S2CID 25698190.
  100. ^ Pollack, Henry N.; Huang, Shaopeng; Smerdon, Jason E. (2006). "Five centuries of climate change in Australia: The view from underground". Journal of Quaternary Science. 21 (7): 701. Bibcode:2006JQS....21..701P. doi:10.1002/jqs.1060.
  101. ^ Fagan, Brian M. (2001). The Little Ice Age: How Climate Made History, 1300–1850. Basic Books. ISBN 978-0-465-02272-4.
  102. ^ Lorrey, Andrew; Fauchereau, Nicholas; Stanton, Craig; Pearce, Petra. “The Little Ice Age climate of New Zealand reconstructed from South Alps cirque glaciers: A synoptic type approach.” Climate Dynamics (June 2013): 11–12. doi:10.1007/s00382-013-1876-8.
  103. ^ Winkler, Stefan (2000). "The 'Little Ice Age' maximum in the Southern Alps, New Zealand: Preliminary results at Mueller Glacier". The Holocene. 10 (5): 643–47. Bibcode:2000Holoc..10..643W. doi:10.1191/095968300666087656. S2CID 131695554.
  104. ^ Nunn, Patrick D. (2000). "Environmental catastrophe in the Pacific Islands around A.D. 1300". Geoarchaeology. 15 (7): 715–40. doi:10.1002/1520-6548(200010)15:7<715::AID-GEA4>3.0.CO;2-L.
  105. ^ Kim M. Cobb; Chris Charles; Hai Cheng; R. Lawrence Edwards. "The Medieval Cool Period and the Little Warm Age in the Central Tropical Pacific? Fossil Coral Climate Records of the Last Millennium". Archived from the original on 20 November 2003.
  106. ^ Field, Julie, S; Lape, Peter, V (March 2010). "Paleoclimates and the emergence of fortifications in the tropical Pacific islands". Journal of Anthropological Archaeology. Elsevier Inc. 29 (1): 113–24. doi:10.1016/j.jaa.2009.11.001 – via Elsevier Science Direct.
  107. ^ Hendy, E. J. (22 February 2002). "Abrupt Decrease in Tropical Pacific Sea Surface Salinity at End of Little Ice Age". Science. 295 (5559): 1511–14. Bibcode:2002Sci...295.1511H. doi:10.1126/science.1067693. ISSN 0036-8075. PMID 11859191. S2CID 25698190.
  108. ^ Rull, Valenti (5 January 2020). "Drought, freshwater availability and cultural resilience on Easter Island (SE Pacific) during the Little Ice Age". The Holocene. Sage Publications. 30 (5): 774–80. Bibcode:2020Holoc..30..774R. doi:10.1177/0959683619895587. S2CID 214564573 – via GeoRef In Process.
  109. ^ Fischer, Steven Roger (2005). Island at the End of the World: The Turbulent History of Easter Island. London: Reaktion Books. ISBN 1861892829.
  110. ^ Villalba, Ricardo (1990). "Climatic fluctuations in northern Patagonia during the last 1000 years as inferred from tree-ring records". Quaternary Research. 34 (3): 346–60. Bibcode:1990QuRes..34..346V. doi:10.1016/0033-5894(90)90046-N.
  111. ^ Villalba, Ricardo (1994). "Tree-ring and glacial evidence for the medieval warm epoch and the little ice age in southern South America". Climatic Change. 26 (2–3): 183–97. Bibcode:1994ClCh...26..183V. doi:10.1007/BF01092413. S2CID 189877440.
  112. ^ Bertrand, Sébastien; Boës, Xavier; Castiaux, Julie; Charlet, François; Urrutia, Roberto; Espinoza, Cristian; Lepoint, Gilles; Charlier, Bernard; Fagel, Nathalie (2005). "Temporal evolution of sediment supply in Lago Puyehue (Southern Chile) during the last 600 yr and its climatic significance". Quaternary Research. 64 (2): 163. Bibcode:2005QuRes..64..163B. doi:10.1016/j.yqres.2005.06.005. hdl:2268/24732. S2CID 20090174.
  113. ^ Meyer, Inka; Wagner, Sebastian (2009). "The Little Ice Age in Southern South America: Proxy and Model Based Evidence". Past Climate Variability in South America and Surrounding Regions. Developments in Paleoenvironmental Research. 14. pp. 395–412. doi:10.1007/978-90-481-2672-9_16. ISBN 978-90-481-2671-2.
  114. ^ Thompson, L. G.; Mosley-Thompson, E.; Davis, M. E.; Lin, P. N.; Henderson, K.; Mashiotta, T. A. (2003). "Tropical Glacier and Ice Core Evidence of Climate Change on Annual to Millennial Time Scales". Climate Variability and Change in High Elevation Regions: Past, Present & Future. Advances in Global Change Research. 15. p. 137. doi:10.1007/978-94-015-1252-7_8. ISBN 978-90-481-6322-9.
  115. ^ a b Araneda, Alberto; Torrejón, Fernando; Aguayo, Mauricio; Torres, Laura; Cruces, Fabiola; Cisternas, Marco; Urrutia, Roberto (2007). "Historical records of San Rafael glacier advances (North Patagonian Icefield): Another clue to 'Little Ice Age' timing in southern Chile?". The Holocene. 17 (7): 987. Bibcode:2007Holoc..17..987A. doi:10.1177/0959683607082414. hdl:10533/178477. S2CID 128826804.
  116. ^ a b Wanamaker, Alan D.; Butler, Paul G.; Scourse, James D.; Heinemeier, Jan; Eiríksson, Jón; Knudsen, Karen Luise; Richardson, Christopher A. (2012). "Surface changes in the North Atlantic meridional overturning circulation during the last millennium". Nature Communications. 3: 899. Bibcode:2012NatCo...3..899W. doi:10.1038/ncomms1901. PMC 3621426. PMID 22692542.
  117. ^ a b Kaufman, D. S.; Schneider, D. P.; McKay, N. P.; Ammann, C. M.; Bradley, R. S.; Briffa, K. R.; Miller, G. H.; Otto-Bliesner, B. L.; Overpeck, J. T.; Vinther, B. M.; Abbott, M.; Axford, M.; Bird, Y.; Birks, B.; Bjune, H. J. B.; Briner, A. E.; Cook, J.; Chipman, T.; Francus, M.; Gajewski, P.; Geirsdottir, K.; Hu, A.; Kutchko, F. S.; Lamoureux, B.; Loso, S.; MacDonald, M.; Peros, G.; Porinchu, M.; Schiff, D.; Seppa, C.; Seppa, H.; Arctic Lakes 2k Project Members (2009). "Recent Warming Reverses Long-Term Arctic Cooling" (PDF). Science. 325 (5945): 1236–39. Bibcode:2009Sci...325.1236K. CiteSeerX doi:10.1126/science.1173983. PMID 19729653. S2CID 23844037.
    "Arctic Warming Overtakes 2,000 Years of Natural Cooling". UCAR. 3 September 2009. Archived from the original on 27 April 2011. Retrieved 19 May 2011.
    Bello, David (4 September 2009). "Global Warming Reverses Long-Term Arctic Cooling". Scientific American. Retrieved 19 May 2011.
  118. ^ Mauquoy, Dmitri; van Geel, Bas; Blaauw, Maarten; van der Plicht, Johannes (1 January 2002). "Evidence from northwest European bogs shows 'Little Ice Age' climatic changes driven by variations in solar activity". The Holocene. 12 (1): 1–6. Bibcode:2002Holoc..12....1M. doi:10.1191/0959683602hl514rr. ISSN 0959-6836. S2CID 131513256.
  119. ^ Lean, Judith; Rind, David (1 January 1999). "Evaluating sun–climate relationships since the Little Ice Age". Journal of Atmospheric and Solar-Terrestrial Physics. 61 (1–2): 25–36. Bibcode:1999JASTP..61...25L. doi:10.1016/S1364-6826(98)00113-8. ISSN 1364-6826.
  120. ^ Robock, Alan (1979). "The "Little Ice Age": Northern Hemisphere Average Observations and Model Calculations". Science. 206 (4425): 1402–04. Bibcode:1979Sci...206.1402R. doi:10.1126/science.206.4425.1402. PMID 17739301. S2CID 43754672.
  121. ^ "Is the Meghalayan Event a Tipping Point in Geology?". The Wire.
  122. ^ "A Chilling Possibility – NASA Science". Archived from the original on 17 March 2010. Retrieved 24 June 2013.
  123. ^ Hopkin, Michael (29 November 2006). "Gulf Stream weakened in 'Little Ice Age'". BioEd Online. Retrieved 1 February 2019.
  124. ^ Villanueva, John Carl (19 October 2009). "Little Ice Age". Universe Today. Retrieved 22 September 2010.
  125. ^ Pittenger, Richard F.; Gagosian, Robert B. (October 2003). "Global Warming Could Have a Chilling Effect on the Military" (PDF). Defense Horizons. 33. Retrieved 22 September 2010.
  126. ^ Leake, Jonathan (8 May 2005). "Britain faces big chill as ocean current slows". The Times. London. Archived from the original on 8 February 2007. Retrieved 11 May 2010.
  127. ^ "Little Ice Age, on season 15, episode 5". Scientific American Frontiers. Chedd-Angier Production Company. 2005. PBS. Archived from the original on 2006.
  128. ^ Austin Alchon, Suzanne (2003). A pest in the land: new world epidemics in a global perspective. University of New Mexico Press. p. 21. ISBN 978-0-8263-2871-7.
  129. ^ "Historical Estimates of World Population". Retrieved 28 April 2019.
  130. ^ Jay, Peter (17 July 2000). "A Distant Mirror". TIME Europe. 156 (3). Archived from the original on 25 July 2008. Retrieved 25 January 2018.
  131. ^ Ravilious, Kate (27 February 2006). "Europe's chill linked to disease". BBC.
  132. ^ Ruddiman, William F. (2003). "The Anthropogenic Greenhouse Era Began Thousands of Years Ago". Climatic Change. 61 (3): 261–93. CiteSeerX doi:10.1023/B:CLIM.0000004577.17928.fa. S2CID 2501894.
  133. ^ a b Faust, Franz X.; Gnecco, Cristóbal; Mannstein, Hermann; Stamm, Jörg (2006). "Evidence for the Postconquest Demographic Collapse of the Americas in Historical CO2 Levels" (PDF). Earth Interactions. 10 (11): 1. Bibcode:2006EaInt..10k...1F. doi:10.1175/EI157.1.
  134. ^ R.J. Nevle et al., "Ecological-hydrological effects of reduced biomass burning in the neotropics after A.D. 1500," Geological Society of America Meeting, Minneapolis MN, 11 October 2011. abstract. Popular summary: "Columbus' arrival linked to carbon dioxide drop: Depopulation of Americas may have cooled climate," Science News, 5 November 2011. (access date 2 January 2012)
  135. ^ Nevle, Richard J.; Bird, Dennis K. (7 July 2008). "Effects of syn-pandemic fire reduction and reforestation in the tropical Americas on atmospheric CO2 during European conquest". Palaeogeography, Palaeoclimatology, Palaeoecology. 264 (1): 25–38. Bibcode:2008PPP...264...25N. doi:10.1016/j.palaeo.2008.03.008. ISSN 0031-0182.
  136. ^ a b Dull, Robert A.; Nevle, Richard J.; Woods, William I.; Bird, Dennis K.; Avnery, Shiri; Denevan, William M. (31 August 2010). "The Columbian Encounter and the Little Ice Age: Abrupt Land Use Change, Fire, and Greenhouse Forcing". Annals of the Association of American Geographers. 100 (4): 755–71. doi:10.1080/00045608.2010.502432. ISSN 0004-5608. S2CID 129862702.
  137. ^ Nevle, R.J.; Bird, D.K.; Ruddiman, W.F.; Dull, R.A. (1 August 2011). "Neotropical human–landscape interactions, fire, and atmospheric CO2 during European conquest". The Holocene. 21 (5): 853–64. Bibcode:2011Holoc..21..853N. doi:10.1177/0959683611404578. ISSN 0959-6836. S2CID 128896863.
  138. ^ Bergeron, Louis (17 December 2008). "Reforestation helped trigger Little Ice Age, researchers say". Stanford News Service.
  139. ^ "War, Plague No Match For Deforestation In Driving CO2 Buildup". Carnegie Institution for Science. 20 January 2011. Retrieved 8 December 2019.
  140. ^ Julia Pongratz; Ken Caldeira; Christian H. Reick; Martin Claussen (20 January 2011). "Coupled climate–carbon simulations indicate minor global effects of wars and epidemics on atmospheric CO2 between ad 800 and 1850". The Holocene. 21 (5): 843–851. doi:10.1177/0959683610386981. ISSN 0959-6836. Wikidata Q106515792.
  141. ^ Ellis, Erle C.; Kaplan, Jed O.; Fuller, Dorian Q.; Vavrus, Steve; Klein Goldewijk, Kees; Verburg, Peter H. (2013). "Used planet: A global history". Proceedings of the National Academy of Sciences. 110 (20): 7978–85. Bibcode:2013PNAS..110.7978E. doi:10.1073/pnas.1217241110. PMC 3657770. PMID 23630271.
  142. ^ Turner, B. L.; Fischer-Kowalski, Marina (2010). "Ester Boserup: An interdisciplinary visionary relevant for sustainability". Proceedings of the National Academy of Sciences of the United States of America. 107 (51): 21963–65. Bibcode:2010PNAS..10721963T. doi:10.1073/pnas.1013972108. PMC 3009765. PMID 21135227.
  143. ^ Pitman, A.J.; Noblet-Ducoudre, N.; Cruz, F.T.; Davin, E.L.; Bonan, G.B.; Brovkn, V.; Claussen, M.; Delire, C.; Ganzeveld, L.; Gayler, V.; Can den Hurk, B.J.J.M.; Lawrence, P.J.; van der Molen, M.K.; Muller, C.; Reick, C.H.; Seneviratne, S.I.; Strengers, B.J.; Voldoire, A. (2009). "Uncertainties in climate responses to past land cover change: First results from the LUCID intercomparison study". Geophysical Research Letters. 36 (L14814): L14814. Bibcode:2009GeoRL..3614814P. doi:10.1029/2009GL039076.
  144. ^ a b Free, Melissa; Robock, Alan (1999). "Global warming in the context of the Little Ice Age". Journal of Geophysical Research. 104 (D16): 19, 057. Bibcode:1999JGR...10419057F. doi:10.1029/1999JD900233.
  145. ^ Hunt, B. G. (2006). "The Medieval Warm Period, the Little Ice Age and simulated climatic variability". Climate Dynamics. 27 (7–8): 677–94. Bibcode:2006ClDy...27..677H. doi:10.1007/s00382-006-0153-5. S2CID 128890550.
  146. ^ Collet, Dominik (2020). "Hungern und handeln". Damals (in German). No. 6. pp. 72–76.

Further reading

  • Fagan, Brian M. (2001). The Little Ice Age: How Climate Made History, 1300–1850. Basic Books. ISBN 978-0-465-02272-4.
  • Parker, Geoffrey (2013). Global Crisis: War, Climate Change and Catastrophe in the Seventeenth Century. New Haven, Conn.: Yale University Press. ISBN 978-0-300-15323-1.
  • White, Sam (2017). A Cold Welcome: The Little Ice Age and Europe's Encounter with North America. Cambridge, Mass.: Harvard University Press. ISBN 978-0-674-97192-9.

External links

  • Abrupt Climate Change Information from the Ocean & Climate Change Institute, links to Woods Hole Oceanographic Institution articles
  • "The Next Ice Age". Discover. September 2002. (discussion of Woods Hole research)
  • "Huascaran (Peru) Ice Core Data". NOAA/NGDC Paleoclimatology Program. 1995.
  • Dansgaard cycles and the Little Ice Age (LIA) (It is not easy to see a LIA in the graphs.)
  • Tyson, P.D.; Karlen, W.; Holmgren, K.; Heiss, G.A. (2000). "The Little Ice Age and Medieval Warming in South Africa" (PDF). South African Journal of Science. 96 (3): 121–26.
  • Was El Niño unaffected by the Little Ice Age? (2002)
  • Evidence for the Little Ice Age in Spain, c. 2003
  • The Little Ice Age in Europe, updated 2009
  • "The Little Ice Age, Ca. 1300–1870". Timeline of European Environmental History. undated review article
  • What's wrong with the sun? (Nothing) (2008)
  •, links, resources, and feature articles on the Little Ice Age and its present-day relevance.
  • Climate History Network, association of historical climatologists and climate historians, many of whom study the Little Ice Age and its social consequences.