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20 kwi 2021 · 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 ...
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.
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 c. 950 to c. 1250. [2]
20 kwi 2021 · 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...
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 phrase “Medieval Warm Epoch” was coined by climatologist H. H. Lamb in 1965 to describe the period of warming in Western Europe and the Northern Atlantic that seemed indicated by several lines of evidence, mostly paleoclimatic and anecdotal (historical accounts dating from the period).
The Medieval Warm Period (MWP) was also called the “Early Medieval Warm Epoch” (Lamb, 1977, 1982) and the “Neo-Atlantic” by some palynologists. The expression “Little Climatic Optimum” (LCO) has sometimes been employed to contrast it with the dramatic warming of the “Atlantic” phase of the late Mesolithic to Neolithic ages ...