||Detailed Chronology of Late|
Holocene Climatic Change
James S. Aber
The following detailed chronology of late Holocene climatic and historic events is based primarily on Le Roy Ladurie (1971), Grove (1988), Savage (1995), Nesje and Dahl (2000), and other sources as noted.
Medieval climatic optimum
- 760-810: Multi-year droughts initiated first collapse phase of classical Mayan civilization in the Yucatán Peninsula of Mexico (Peterson and Haug 2005).
- 793: Viking raid at Lindisfarne, England. This was the beginning of major Viking expansions outward from Scandinavia—see Fig. 19-14.
- 800-1000s: Aletsch and Grindelwald glaciers (Switzerland) were much smaller than today.
- 835: Viking invasions of England, Scotland, Wales, Ireland, and France began in earnest. By the mid-9th century most of these areas were permanently
occupied by Vikings.
- 860: Second collapse phase of Mayan civilization caused by mulit-year drought (Peterson and Haug 2005).
- 870: Vikings have taken all of England, except for the Wessex region. England became an Anglo-Danish dominion by end of 9th century.
- 870: Settlement of Iceland began; Viking immigration from Norway as well as Viking colonies in Scotland, Isle of Man, Ireland, Orkneys, Faeroes, etc. Glaciers of Iceland much smaller than today.
- 880-1140: Radiocarbon dates on trees that grew in Canada far north of modern timberline.
- 880-1230: Warm and wet climate in the Lvliang Mountains of north-central China (Liu et al. 2014).
- 910: Final collapse phase of Mayan civilization caused by mulit-year drought (Peterson and Haug 2005).
- 911: Viking dukedom granted by France in the area of Normandy (= Norse land), with its center at Rouen—see Fig. 19-14. Normandy became one of the strongest of Viking dukedoms.
- 924: Aethelstan became king of Wessex and began a drive to force the Vikings out of southern England. During the mid-10th century, the Anglo-Saxon kindgom became dominant in southern England.
- 930: Iceland nation established as independent commonwealth; population estimates range from under 10,000 (Ross 2010) to as many as 40,000 inhabitants (Magnusson 1987).
- 950-1250: Low oxygen-isotope values in ostracods from lake sediment at El Gancho, Nicaragua indicate wetter conditions during the Medieval Climatic Optimum (Stansell et al. 2013).
- 985: Settlement of Greenland (from Iceland) began led by Eirík the Red.
- 1000: Peaceful acceptance of Christianity by Iceland (or in 999).
- 1000: Discovery of Vinland (Newfoundland) by Eirík's son, Leif the Lucky.
- 1007: Expedition to Vinland led by Thorfinn Karlsefni. Considerable portion of eastern North America was explored, and Thorfinn's son Snorri was born in Vinland. He was the immediate ancestor of several Icelandic bishops (Craigie 1913). However, the Norse attempt to settle in Newfoundland was thwarted by native resistance.
- 1000s: Low radiocarbon levels in tree rings indicate high solar output and presumably warmer temperatures.
- 1000s: Decline in Tiwanaku culture in Bolvian-Peruvian altiplano linked to prolonged drought conditions (Peterson and Haug 2005).
- 1000s: Tyndall Glacier (Mt. Kenya, Africa) begins to advance (Mahaney 1990).
- 1000s: Cattle and pigs gradually disappear from Icelandic farms; sheep and goats remain (Ross 2010).
- 1000-1200: Rapid population growth in Estonia based on cereal grains—barley, rye, wheat. Northernmost region for crop tillage as the primary means of subsistence. Population by early 13th century at least 150,000 people (Tannberg et al. 2000).
- 1000-1300: Frequent severe droughts in the Great Plains of the central United States (Miao et al. 2007).
- 1020-1200: Minimal sea-ice cover around Iceland.
- 1066: Norman invasion of England led by William the Conqueror. The Anglo-Saxon
kindgom was defeated, and William became king of England. The Norman (Viking) empire
included all of England, Normandy, and much of western France—see Fig. 19-15.
- 1080-1180: Favorable interval of mild winters and dry summers in western
Europe: England, France, Germany.
- 1100: Human population of Iceland reached an estimated peak of 70,000 inhabitants (Magnusson 1987).
- 1100s: Norse population in Greenland reached 5000 to 6500 in two well developed settlements in southwestern coastal region (McGovern 1981).
- 1100-1300: Warm and dry interval in west-central Asia based on lake sediment, north of the Tien Shan Mountains in northwestern China (Long et al. 2011).
- 1104: Hekla volcano erupted in Iceland following several centuries of quiescence. Rich farming region of
Thjórsárdalur was completely destroyed and abandoned (Bárdarson 1991). Hekla has since become one of the most active volcanoes in the world.
||Hekla, an active volcano in south-central Iceland. Following a long quiet
period, this volcano erupted in 1104 and has since been one of the world's
most active volcanoes. The barren scoria fields in the foreground attest
to the local effects of this volcano. Photo © J.S. Aber.
- 1125: Greenland obtained its own Catholic bishop through trading a live polar bear for the Norwegian bishop, Arnald (McGovern 1981).
- Late 1100s: Sharp fall in Camp Century ice-core 18O content
signals lower temperature in North Atlantic region.
- 1200: Foraminifera in deep Atlantic sediments show culmination of
warming trend of preceding few centuries.
- 1200: Beginning of increased sea ice in coastal waters of Iceland.
- 1200s: Glaciers began to advance in Iceland. Lack of local wood limited boat building and restricted trade and travel abroad (Ross 2010).
- 1215-1350: Glaciers began to advance in several parts of Europe.
- 1215: Oberriederin (irrigation canal) overrun by advance of
Aletsch glacier; radiocarbon dates on buried larch; canal head still
covered by modern Aletsch glacier.
- 1220-60: Age of the Sturlungs (civil unrest, violence, war) in Iceland (Ross 2000).
- 1227: Thick sea ice on the Baltic allowed a German army to march from the mainland of Estonia to the islands of Muhu and Saaremaa and to capture those islands (Tannberg et al. 2000).
- 1230-1880: Cold and dry climate in the Lvliang Mountains of north-central China (Liu et al. 2014).
- 1240: Radiocarbon date on large Inuit settlement in the northern hunting ground of western Greenland. From this time, Inuits migrated southward and came into increasing competition and conflict with Norse Greenlanders (McGovern 1981).
- 1240-1362: North Sea storms destroyed 60 Danish coastal parishes in Slesvig (now Schleswig, Germany) with much loss of life (Lamb 1981).
- 1250-1300: Irregular cooling followed by extreme inter-decadal fluctuations of the following century reduced seal hunting in southwestern Greenland. Growing shortage of seaworthy wooden boats also restricted travel and hunting (McGovern 1981).
- 1262-64: Icelandic chiefains swear allegiance to the King of Norway, Hákon Hákonarson, and his son Magnús (Ross 2010). Iceland commonwealth ends. Greenland also accepted sovereignty of the King of Norway.
- 1275: Initial expansion of perennial snow and ice cover on Baffin Island that killed and buried vegetation, which is just now beginning to emerge (Morton 2012).
- 1275-1300: Prolonged drought caused disappearance of cliff-dwelling Anasazi culture in southwestern U.S. (Peterson and Haug 2005).
- 1280: Radiocarbon date on wood (Pinus cembro) of forest buried by advance of Grindelwald glacier; forest does not again grow on site today.
- 1300s: Decline of vineyards in Germany; vineyards completely disappeared in England.
- 1300s: Primary period of textual production (writing) of Icelandic sagas from their oral traditions.
- 1300-1350: Fishing replaced cereal crops as main food resource in Iceland.
- 1315: Crop failure and starvation in northern Estonia (Tannberg et al. 2000).
- Mid-1300s: Old sea route from Iceland directly west to Greenland impassable due to southward expansion of sea ice; serious decline began in Greenland settlements.
- 1340-50: Western (northern) settlement in Greenland abandoned and derelict.
- 1348: Black Death swept through England killing about one-third of the population. See Farringdon cemetery.
- 1350: Beginning of disasterous wind-blown sand drifting along northwestern coast of Denmark. Episodes of wind erosion and sand-dune migration occurred several times during the following centuries (Clemmensen and Andersen 1998).
- 1378: Death of Bishop Alf in Greenland; he was not replaced (McGovern 1981).
- 1380-1460: Minimal sea-ice cover around Iceland.
- 1397: Union of Kalmar joined Denmark, Sweden and Norway; Greenland and Iceland became colonies of the Danish Kingdom. Greenland remains part of Denmark to present.
- 1400-1700: 3‰ decline in 18O values for Inuit and Norse teeth in western Greenland implies significant climatic cooling—see Fig. 19-16.
||Norse skeletal remains from graves at Hvalsey church, Greenland.
18O values from tooth enamel indicate sharply colder
temperature during the Little Ice Age (Fricke et al. 1995).
Photo by Preben Jensen; reproduced by permission.|
- 1400-1750: Cold and wet interval in west-central Asia based on lake sediment, north of the Tien Shan Mountains in northwestern China (Long et al. 2011).
- 1408-10: Last reliable account of Norsemen still living in Greenland; all had perished by end of 15th century. All official contact with Norse Greenland ended after 1408 (McGovern 1981).
- early 1400s until mid-1600s: Reduced activity of El Nińo-Southern Oscillation (ENSO) recorded in fossil corals of Papua New Guinea in the western Pacific (Hereid et al. 2013).
- 1450: Further expansion of perennial snow and ice cover on Baffin Island that killed and buried vegetation, which is just now beginning to emerge (Morton 2012).
- 1450-present: High oxygen-isotope values in ostracods from lake sediment at El Gancho, Nicaragua indicate dry conditions during the Little Ice Age and since (Stansell et al. 2013).
- 1460: Increased sea ice in coastal waters of Iceland.
- 1460-1560: End of Medieval glaciation was followed by a century of relatively mild climate.
- 1510: German merchants visited Greenland and found Inuits living among ruins of Norse settlements.
- 1530-75: Chamonix/Mont Blanc glaciers (France) advanced, but caused no damages.
Little Ice Age
- 1550-1600: Significant cooling in Switzerland marked by reduced vine yields and narrow tree rings, especially for the intervals 1560-64, 1572-79 and 1585-97 (Pfister 1981). Mer de Glace, Grindelwald, and other glaciers began advancing in 1580s.
- 1570: Medieval gold mines of Hohe Tauern, Austria blocked by glacier ice; Icelandic glaciers much larger than today.
- 1585: First account of cave glacier from Jura region; a natural
cave filled with ice formations that persisted until 1910.
- 1588: Grindelwald glacier broke through its end moraine.
- 1594-98: Glaciers of Italian Alps advanced markedly.
- 1595: Gietroz glacier (Switzerland) advanced, dammed Dranse River, and
caused flooding of Bagnes with 70 deaths.
- 1600: Eruption of Huaynaputina volcano (Peru) caused the most severe short-term cooling event of the past 600 years in the northern hemisphere.
- 1600: Vernagt glacier (eastern Alps) advanced and blocked Rofenthal
causing lake to form; failure of ice dam led to destructive flooding.
- 1600: Dramatic increase in sea ice in coastal waters of Iceland which lasted until early 20th century.
- 1600-10: Advances by Chamonix glaciers accompanied by massive floods
entirely destroyed three villages--Bonnenuit, Le Chatelard and La
Bonneville--and severely damaged a fourth, La Rosiere. Oldest village (Le
Chatelard) dated from 1200s.
- 1600-1700: Western coast of Greenland began to submerge due to crustal
depression adjacent to thicker ice sheet; submergence continued.
- 1640-50: General glacier advances throughout Alps. Fossil trees (P.
cembro) from high moraines in Mont Blanc vicinity radiocarbon dated to
- 1644: Chamonix glaciers advanced across Chamonix valley and threatened
to transform valley into lake. Swiss glaciers expanded to their maximum
Little Ice Age positions: 1644-53.
- 1650s: Some signs of moderation; Chamonix glaciers retreated slightly
from their terminal moraines.
- 1650-1700: Rapid rise in Black Sea chemocline corresponds to end of the peak bloom period of Emiliana huxleyi (coccolithophore) brought about by colder temperature, winter storms, and mixing surface and nutrient-rich deep water (Arnold et al. 2012).
- 1670-80s: No signs of significant waning. Maximum historical advances
achieved by glaciers in eastern Alps; Vernagt glacier again caused
flooding. Noticeable decline of human population by this time in areas
close to glaciers, whereas population elsewhere in Europe had risen.
- 1690s: Moderate withdrawal of many glaciers in Alps took place; Chamonix
glaciers retreated about 500 m. Norwegian glaciers experienced opposite
trend, however, with marked advances.
- Late 1600s: Recurrent famine in Scotland; 100,000 Scots had emigrated to
northern Ireland by 1691 (Oppenheimer and Boyle 1990).
- 1693: Hekla (Iceland) experienced enormous eruption, in which 22,000
km² of land was covered by tephra fall; 55 farms were ruined or badly
damaged in neighboring districts (Bárdarson 1991).
- 1695-97: Great Famine of Estonia. Climate was unfavorable for crops in 1694; summer of 1695 was cold and rainy, followed by an early autumn frost that destroyed the summer crops. Cold conditions continued during 1696, and rain fell throughout the summer. Peasants, orphans and the elderly began to die en masse of starvation. Melting of snow in spring 1697 revealed many corpses. Meanwhile, rich landlords and merchants exported grain to Finland and Sweden, where crops also had failed. 70,000 to 75,000 people died during the famine in Estonia, which did not end until 1698 (Tannberg et al. 2000).
- 1695-1709: Outlet glaciers of Drangajökull and Vatnajökull
(Iceland) advanced dramatically, approaching or destroying farms. One farm
at Fjallsjökull dated from AD 900 (Bárdarson 1991).
||Fjallsjökull, an outlet glacier of Vatnajökull ice cap on the southeastern
coast of Iceland. Advance of this glacier in the 1695-1710 period destroyed a farm that
dated from Viking settlement. Photo © J.S. Aber.|
- 1700-20: Glaciers maintained overall positions in Europe; some minor
advances and retreats took place.
- 1700-21: Great Northern War: crippled by the famine of late 1690s, Sweden was vulnerable to attack by Russia, Poland, and Denmark. Weakend by war, famine and plague, Swedish power over the Baltic region was broken.
- 1710: Nigardsbreen (Norway) was advancing at rate which averaged 100 m
per year over next 25 years.
- 1720: Engabreen (Norway) buried a farm; other glaciers threatened farms
- 1720-30s: Alpine glaciers maintained positions, much larger than today,
but did not experience major advances.
- 1732: Vatnajökull crushed ruins of Icelandic farm that had been
abandoned during earlier advance.
- 1735: Nigardsbreen destroyed pasture land and threatened a farm, which was completely destroyed by ice in 1743.
||Nigardsbreen, an outlet glacier of Jostedalsbreen, is visible at the valley
head in the distance. In the early 1700s, this glacier expanded dramatically
and destroyed a farm. The combination of glacier advances, melt-water floods,
and other disasters led to much human suffering in the vicinity.
Photo date © J.S. Aber.|
- 1740s: Glaciers advanced in all Alpine regions, including Chamonix
glaciers, Grindelwald and Vernagt glaciers.
- 1741: Drangajökull destroyed another farm in Iceland.
- 1748-50: Norwegian glaciers achieved their historical maximum Little Ice Age positions.
||Tuftebreen is a small outlet glacier of Jostedalsbreen. It is just visible
at top of the mountain side in this view. During the Little Ice Age this
glacier advanced and reached a maximum position about A.D. 1750. The maximum
limit is marked by the stony lateral moraine on the valley floor. The glacier
destroyed some pasture, but the local farm survived.
Photo © J.S. Aber.|
- 1760-90: Long-term "normality" of glacier expansion accepted; no real
sign of significant glacier retreats.
- 1775: Worst episode of sand-dune drifting in northwestern Denmark. Many farms, villages, and churches were destroyed during the late 1700s.
||St. Laurentii Church was partly buried by drifting sand dunes in 1775; the entrance could
be held open only by digging away sand during following years. In 1795, the church was
abandoned, and the walls were torn down in 1810 (Langberg 1971). Only the tower survives;
it was utilized as a lighthouse for some years. Photo © J.S. Aber.|
- 1780: New York Harbor froze over for the first recorded time allowing people to walk from Manhattan Island to Staten Island (Morton 2012).
- 1783-84: Huge fissure eruptions of Laki volcano in Iceland; greatest historical volcanic eruptions anywhere in world; possibly largest in all Holocene (Bárdarson 1991). Volcanic gas (SO2) killed vegetation, plus a severe winter resulted in mass starvation of livestock. The "haze famine" killed about one-quarter of Iceland's human population.
||Laki volcano erupted in Iceland in 1783-84. A tremendous volume of lava
poured from fissures and spread across the landscape as aa flows.
These flows are now covered by moss, as seen here. The Laki eruption was one
of the largest anywhere, and the resulting famine was the greatest natural
disaster in the history of Iceland. Photo © by J.S. Aber. |
- 1806-08: Crop failures and famine in Estonia (Tannberg et al. 2000).
- 1810-1819: Coldest decade of the last 1250 years in the French Alps, according to tree-ring data (Corona et al. 2011). Mean summer temperature was 3 °C lower than the warmest decades (810s and 1990s).
- 1812-1817: Cluster of bad years for agriculture in western Europe that led to high food prices and a subsitence crisis (Pfister 1981).
- 1814: Last London "frost fair" when the Thames River froze thick enough to host a large festival in February. January 1814 was the third coldest month (mean -2.9 °C) since London temperature recording began in 1659. Cold blamed on low sunspot activity and the North Atlantic Oscillation. See frost fair.
||1816: Coldest single year on record in many places in Europe and North America, following the 1815 eruption of Mount Tambora in Indonesia. U.S. postage stamp depicts ice cutting in winter. |
- 1816-25: New glacier offensive throughout Europe; all Alpine glaciers showed advances reaching positions slightly short of 17th century Alpine maximum limits.
- 1830-40s: Moderate retreat shown by many glaciers.
- 1840s: Introduction of potatoes in Estonia put an end to recurring famines (Tannberg et al. 2000).
- 1850-55: Fairly general glacier advances throughout Alps; some panic in
population, but no serious damages resulted.
- 1855: Signs of moderate retreats by Chamonix glaciers.
End of the Little Ice Age
- 1860-80s: Evidence of pronounced glacier withdrawal all over continental
Europe; many Alpine glaciers retreated >1 km by end of 19th century. Icelandic glaciers remained in advanced positions, however.
- 1870: Athabasca glacier of the Columbia Icefield (Alberta, Canada)
advanced to near its Little Ice Age maximum completely blocking Sunwapta
valley. Other glaciers in western Canada experienced major expansions.
- 1880 to present: Warm and wet climate in the Lvliang Mountains of north-central China (Liu et al. 2014).
- Late 1800s: Little Ice maximum in western Canada, which is contrary to general glacier retreat in most other part of the world—see Fig.
||View from crest of Little Ice Age recessional moraine looking
upvalley toward Hilda Glacier, Alberta, Canada. The glacier has wasted to a
very small size during this century. Photo © by J.S. Aber.|
||View downvalley, showing Little Ice Age moraines built by
Hilda Glacier. The outermost lateral moraine (left foreground) marks the
maximum Little Ice Age ice margin, 1870-90s. Some of the moraines retain a
core of stagnant ice that is insulated by the cover of sediment.
Photo © J.S. Aber. |
- 1890: Eyjabakkajökull, an outlet glacier of Vatnajökull (Iceland), surged to its maximum historical limit.
- 1890: Approximate end of Little Ice Age climate in Svalbard based on lake sediments (Jiang et al. 2011).
- 1900: Sléttjökull, an outlet glacier of Mýrdalsjökull (Iceland), stood at its Little Ice Age maximum. Other Icelandic glaciers at or near their maxima.
||View from margin of Sléttjökull looking northward over the recently
deglaciated landscape. At the beginning of the 20th century, the margin of
Sléttjökull was located at the end moraine (yellow dots) in the
middle distance, about 2 km from the present ice margin.
Photo © by J.S. Aber. |
- Early 1900s: Rapid retreat by glaciers on Mt. Kenya, Africa—see Fig. 19-18.
- 1917: Iceland became an independent sovereign state; gained full independence from Denmark in 1944.
- 1920: Marked decrease in sea ice in coastal waters of Iceland. Summer temperature rises markedly in the French Alps (Corona et al. 2011).
- 1920-30s: Glaciers declined rapidly everywhere, except Antarctica; end of Little Ice Ages.
||During the 1930s, Nigardsbreen (Norway) retreated rapidly and uncovered a rock basin
in which this proglacial lake is ponded. A lateral moraine from an earlier retreat phase
is visible above the lake in the right foreground. Photo © J.S. Aber.|
||Wine harvests of|
Phenology is the study of seasonal dates of plant growth phenomena,
such as flowering or ripening in fruit trees or grape vines. The date at
which grapes ripen is mainly a function of summer temperature; warm, sunny
weather results in an early wine harvest, and vice versa. Good
historical records of the annual wine harvest have been compiled from towns
in western Europe (France and Switzerland) by historians interested in the
impact of climate on human activities (Le Roy Ladurie 1971).
The following chronology indicates a close correspondence between wine harvest dates and glacier advances during the Little Ice Age. Grape yield correlates most closely with mid-summer temperature. Early wine harvests generally coincided with glacier retreats; late harvests were times of glacier advances. However, glacier responses usually lagged 5-7 years behind the climatic changes indicated by wine harvest dates (Pfister 1981). Chronology of wine harvest dates and climatic conditions in western Europe is based on Le Roy Ladurie (1971).
- 1510-1559: Decidedly warm overall, average harvest date 26 Sept.
- 1560-1600: Definitely cooler, average harvest date 30 Sept. 1590s was coldest decade of 16th century.
- 1601-1616: Warm or average conditions, average harvest 25 Sept.
- 1617-1650: Outstanding cold episodes with low temperatures and late wine harvests.
- 1651-1686: Early wine harvest dates with drought episodes.
- 1687-1703: Late wine harvests, exceptionally cold spring/summer temperatures (thermometer readings). 1690s was coldest decade of 17th century, crop failures common.
- 1711-1717: Cold spring/summer weather, late wine harvests.
- 1718-1737: Warm spring/summer weather, early wine harvests.
- 1739-1752: Cold spring/summer weather, late wine harvests.
- 1757-1763: Warm spring/summer weather, early wine harvests.
- 1765-1777: Especially cold, wet spring/summer weather, low barometric
pressure, late wine harvests.
- 1778-1784: Warm spell throughout Europe, highest thermometer readings
recorded prior to 20th century.
- 1801-1811: Hot summers, early wine harvests.
- 1812-1817: Cold, wet spring/summer weather. 1816 coldest year on record, latest wine harvests ever known (early November), cereal crops failed.
- 1850-1856: Cold springs and cool summers, late wine harvests.
- post-1856: Warm, clear spring/summer weather, high air pressure, early
wine harvests, end of Little Ice Ages in western Europe.
Remember: send your comments and questions via e-mail to the instructor.
Glossary or references.