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The Medieval Warm Period, also known as the Medieval Climate Anomaly, refers to a historical period between 800 and 1250 CE characterized by warmer and drier conditions globally. It was a significant warm episode during the Holocene prior to the industrial era, with temperatures comparable to or even warmer than the mid-20th century.
The Medieval Warm Period (MWP), also known as the Medieval Climate Optimum or the Medieval Climatic Anomaly, was a time of warm climate in the North Atlantic region that lasted from about 950 CE to about 1250 CE. [2]
Medieval warm period (MWP), brief climatic interval that is hypothesized to have occurred from approximately 900 ce to 1300 (roughly coinciding with the Middle Ages in Europe), in which relatively warm conditions are said to have prevailed in various parts of the world, though predominantly in the
20 Απρ 2021 · During the Medieval warm period, an increase in solar radiation and decrease in volcanic eruptions created a La Niña-like event that changed the usual patterns.
cold and warm periods during the past millennium by mod-ern standards, only the 20th century could be termed a warm period; the period AD 1000–1400 would be termed a moderately warm period, and the period 1400–1900 a moderately cold period. Evidence for the Southern Hemi-sphere is far sketchier, and it is difficult as yet to reach
1.1.7 Medieval Warm Period (900–1300 AD) The Medieval Warm Period (MWP) was a time of warm climate from about 900–1300 AD, when global temperatures were somewhat warmer than at present. Tempera-tures in the GISP2 ice core were about 2°F (1°C) warmer than modern temperatures (Fig. 8.14).
The Medieval warm period is an asynchronous regional warming caused by natural (not human-driven) climatic variation, whereas we are facing a homogeneous and global warming caused by human activity releasing too much greenhouse gas into the atmosphere.
