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The Medieval Warm Period (MWP) was a time of warm climate in the North Atlantic region from c.950 to c.1250, followed by the Little Ice Age. The MWP was not a globally uniform event and its causes and effects are still debated by researchers.
20 kwi 2021 · Learn how the Medieval warm period was a regional event of temperature rise between 750 and 1350 AD, mainly driven by natural climate patterns. Discover how it affected human societies and ecosystems in different parts of the world.
Learn about the controversial climate interval that allegedly occurred from 900 to 1300 CE, mainly in the Northern Hemisphere. Find out the evidence, causes, and implications of the medieval warm period for modern climate change.
19 kwi 2016 · The medieval warm period (AD 725 – 1025) was a time of climate stability and economic growth, as well as expansion of trade and migration. Learn how this period was influenced by natural and human factors, and how it contrasted with the following Medieval Quiet Period.
Średniowieczne optimum klimatyczne – okres ocieplenia znany głównie z rejonu północnego Atlantyku (Europa, Ameryka Północna), które miało miejsce ok. 800–1300 n.e. Nastąpiło ono po chłodnym okresie tzw. średniowiecznej wędrówki ludów w Europie, czyli wczesnośredniowiecznym ochłodzeniu. Kończy ten okres mała epoka lodowa.
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.
Learn about the Medieval Warm Period, a historical period of warmer and drier conditions globally between 800 and 1250 CE. Explore chapters and articles on Greenland, tree rings, and the Anthropocene from ScienceDirect Topics.
