Northern hemisphere temperature reconstructions for the past 2,000 years.
The
Medieval Warm Period (
MWP),
Medieval Climate Optimum, or
Medieval Climatic Anomaly was a time of warm
climate in the
North Atlantic region that may also have been related to other
climate events around the world during that time, including in
China[1] and other countries,
[2][3][3][4][5][6][7] lasting from about AD 950 to 1250.
[8] It was followed by a cooler period in the
North Atlantic termed the
Little Ice Age. Some refer to the event as the Medieval Climatic Anomaly as this term emphasizes that effects other than temperature were important.
[9][10]
Despite substantial uncertainties, especially for the period prior to 1600 for which data are scarce, the warmest period of the last 2,000 years prior to the 20th century very likely occurred between 950 and 1100, but temperatures were probably between 0.1 °C and 0.2 °C below the 1961 to 1990 mean and significantly below the level shown by instrumental data after 1980. Proxy records from different regions show peak warmth at different times during the Medieval Warm Period, indicating the heterogeneous nature of climate at the time.
[11] Temperatures in some regions matched or exceeded recent temperatures in these regions, but globally the Medieval Warm Period was cooler than recent global temperatures.
[8]
Initial research
The Medieval Warm Period (MWP) is generally thought to have occurred from about AD 950–1250, during the
European Middle Ages.
[8] In 1965
Hubert Lamb, one of the first
paleoclimatologists, published research based on data from
botany, historical document research and meteorology combined with records indicating prevailing temperature and rainfall in England around 1200 and around 1600. He proposed that "Evidence has been accumulating in many fields of investigation pointing to a notably warm climate in many parts of the world, that lasted a few centuries around A.D. 1000–1200, and was followed by a decline of temperature levels till between 1500 and 1700 the coldest phase since the last ice age occurred."
[12]
The warm period became known as the MWP, and the cold period was called the
Little Ice Age (LIA). However, this view was questioned by other researchers; the
IPCC First Assessment Report of 1990 discussed the "Medieval Warm Period around 1000 AD (which may not have been global) and the Little Ice Age which ended only in the middle to late nineteenth century."
[13] The
IPCC Third Assessment Report from 2001 summarised research at that time, saying "…current evidence does not support globally synchronous periods of anomalous cold or warmth over this time frame, 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".
[14] Global
temperature records taken from ice cores, tree rings, and lake deposits, have shown that, taken globally, the Earth may have been slightly cooler (by 0.03 degrees Celsius) during the 'Medieval Warm Period' than in the early and mid-20th century.
[15][16]
Palaeoclimatologists developing region-specific climate reconstructions of past centuries conventionally label their coldest interval as "LIA" and their warmest interval as the "MWP".
[15][17] Others follow the convention and when a significant climate event is found in the "LIA" or "MWP" time frames, associate their events to the period. Some "MWP" events are thus wet events or cold events rather than strictly warm events, particularly in central
Antarctica where climate patterns opposite to the North Atlantic area have been noticed.
By world region
Evidence exists across the world, often very sparsely, for changes in climatic conditions over time. Some of the "warm period" events documented below are actually "dry periods" or "wet periods."
[18]
Globally
A 2009 study by
Michael Mann et al. examining spatial patterns of surface temperatures shown in
multi-proxy reconstructions finds that the MWP shows "warmth that matches or exceeds that of the past decade in some regions, but which falls well below recent levels globally."
[8] Their reconstruction of MWP pattern is characterised by warmth over large part of North
Atlantic, Southern
Greenland, the Eurasian
Arctic, and parts of
North America which appears to substantially exceed that of the late 20th century (1961–1990) baseline and is comparable or exceeds that of the past one-to-two decades in some regions. Certain regions such as central
Eurasia, northwestern North America, and (with less confidence) parts of the South Atlantic, exhibit anomalous coolness.
North Atlantic
The last written records of the
Norse Greenlanders are from a 1408 marriage in the church of
Hvalsey — today the best-preserved of the Norse ruins.
A
radiocarbon-dated
box core in the
Sargasso Sea shows that the sea surface temperature was approximately 1 °C (1.8 °F) cooler than today approximately 400 years ago (the Little Ice Age) and 1700 years ago, and approximately 1 °C warmer than today 1000 years ago (the Medieval Warm Period).
[5]
Using sediment samples from
Puerto Rico, the
Gulf Coast and the Atlantic Coast from
Florida to
New England, Mann
et al. (2009) found consistent evidence of a peak in
North Atlantic tropical cyclone activity during the Medieval Warm Period followed by a subsequent lull in activity.
[19]
Through retrieval and isotope analysis of marine cores and examination of mollusc growth patterns from
Iceland, Patterson
et al were able to reconstruct a mollusc growth record at a decadal resolution from the
Roman Warm Period through the Medieval Warm Period and into the Little Ice Age.
[20]
North America
1690 copy of the 1570
Skálholt map, based on documentary information about earlier Norse sites in America.
The 2009
Mann et al. study found warmth exceeding 1961–1990 levels in Southern
Greenland and parts of North America during the Medieval climate anomaly (defined for this purpose as 950 to 1250) with warmth in some regions exceeding temperatures of the 1990–2010 period. Much of the Northern hemisphere showed significant cooling during the
Little Ice Age (defined for the purpose as 1400 to 1700) but
Labrador and isolated parts of the United States appeared to be approximately as warm as during the 1961–1990 period.
[8]
Norse colonization of the Americas has been associated with warmer periods. The
Vikings took advantage of ice-free seas to colonize areas in Greenland and other outlying lands of the far north.
[21]
From around 1,000 AD Vikings formed settlements in two areas located near the southern tip of Greenland at a similar
latitude to
Iceland, the
Eastern Settlement at the southern tip, and the
Western Settlement to its north. A smaller group of farms between them has been identified by archaeologists as the
"Middle Settlement". At that time they farmed cattle and pigs, with around a quarter of their diet from seafood, but after the climate became colder and stormier around 1250 smaller farms gradually changed to farming sheep and goats rather than cows. Around 1300 they abandoned pig farming, and from then on
seal hunting provided over three quarters of their food. While there are no signs that this adversely affected their health, by mid century trade with Norway fell away and there was little demand for their exports of seal skins and walrus tusks. One of the last documents of their occupation dates from 1408, and over the remainder of that century the remaining Vikings left in what seems to have been an orderly withdrawal, largely due to social factors such as increased availability of farms in Scandinavian countries.
[22]
Around 1000AD the climate was sufficiently warm for the north of
Newfoundland to support a Viking colony and led to the descriptor "
Vinland." An extensive settlement at
L'Anse aux Meadows was found and originally excavated by
Helge Ingstad.
[23]
In the
Chesapeake Bay, researchers found large temperature excursions (changes from the mean temperature of that time) during the Medieval Warm Period (about 950–1250) and the
Little Ice Age (about 1400–1700, with cold periods persisting into the early 20th century), possibly related to changes in the strength of North Atlantic
thermohaline circulation.
[24] Sediments in
Piermont Marsh of the lower
Hudson Valley show a dry Medieval Warm period from AD 800–1300.
[25]
Prolonged droughts affected many parts of the western
United States and especially eastern
California and the west of
Great Basin.
[15][26] Alaska experienced three time intervals of comparable warmth:
AD 1–300, 850–1200, and post-1800.
[27] Knowledge of the North American Medieval Warm Period has been useful in dating occupancy periods of certain Native American habitation sites, especially in arid parts of the western U.S.
[28][29] Review of more recent archaeological research shows that as the search for signs of unusual cultural changes during the MWP has broadened, some of these early patterns (for example, violence and health problems) have been found to be more complicated and regionally varied than previously thought while others (for example, settlement disruption, deterioration of long distance trade, and population movements) have been further corroborated.
[30]
Other regions
The climate in equatorial east
Africa has alternated between drier than today, and relatively wet. The drier climate took place during the Medieval Warm Period (~AD 1000–1270).
[31]
A
sediment core from the eastern Bransfield Basin,
Antarctic Peninsula, preserves climatic events in the
Little Ice Age and Medieval Warm Period.
[32] The core shows a distinctly cold period about AD 1000–1100, illustrating that during the "warm" period there were, regionally, periods of both warmth and cold.
Corals in the tropical
Pacific Ocean suggest that relatively cool, dry conditions may have persisted early in the millennium, consistent with a
La Niña-like configuration of the
El Niño-Southern Oscillation patterns.
[33] Although there is an extreme scarcity of data from
Australia (for both the Medieval Warm Period and
Little Ice Age) evidence from wave-built shingle terraces for a permanently full
Lake Eyre[34] during the 9th and 10th centuries is consistent with this La Niña-like configuration, though of itself inadequate to show how lake levels varied from year to year or what climatic conditions elsewhere in Australia were like.
The MWP has been noted in Chile in a 1500-year lake bed
sediment core,
[35] as well as in the Eastern Cordillera of Ecuador.
[36]
Adhikari and Kumon (2001), whilst investigating sediments in
Lake Nakatsuna in central Japan, finding a warm period from AD 900 to 1200 that corresponded to the Medieval Warm Period and three cool phases, of which two could be related to the Little Ice Age.
[37] Another research in northeastern Japan shows that there is one warm/humid interval from AD 750 to 1200, and two cold/dry intervals from AD 1 to 750 and 1200 to present.
[7] Ge
et al. studied temperatures in China during the past 2000 years; they found high uncertainty prior to the 16th century but good consistency over the last 500 years,
highlighted by the two cold periods 1620s–1710s and 1800s–1860s, and the warming during the 20th century. They also found that the warming during the 10–14th centuries in some regions might be comparable in magnitude to the warming of the last few decades of the 20th century which was unprecedented within the past 500 years.
[38]
A 1979 study from the University of Waikato found that "Temperatures derived from an
18O/
16O profile through a stalagmite found in a
New Zealand cave (40.67°S, 172.43°E) suggested the Medieval Warm Period to have occurred between AD 1050 and 1400 and to have been 0.75 °C warmer than the Current Warm Period."
[39] The MWP has also been evidenced in New Zealand by an 1100-year tree-ring record.
[40]
A reconstruction based on ice cores found the Medieval Warm Period could be distinguished in tropical South America from about 1050 to 1300, followed in the 15th century by the Little Ice Age. Peak temperatures did not rise as high as those from the late 20th century, which were unprecedented in the area during the study period going back around 1600 years.
[41]
