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20 kwi 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.
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]
Some provide evidence of relatively warm temperatures (most pronounced during the summer months) in several regions, including the North Atlantic, northern Europe, China, and parts of North America, as well as the Andes, Tasmania, and New Zealand.
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.
30 paź 2014 · Medieval Warm Period (Global) -- Summary. Between the 10th and 14th centuries AD, earth's average global temperature may have been warmer than it is today, according to the analyses of Lamb (1977, 1984, 1988) and Grove (1988).
The Medieval Climatic Optimum (also known as the Lit-tle Climatic Optimum, Medieval Warm Period, or Medieval Warm Epoch) refers to a period of climatic history during which temperatures in Europe and neighboring regions of the North Atlantic are believed to have been comparable to, or to have even exceeded, those of the late 20th century.
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 ...
