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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. Climate proxy records show peak warmth occurred at different times for different regions, which indicate that the MWP was not a globally uniform…
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mwp climate warm period lia temperature medieval north ice atlantic found ce around global eastern temperatures age also 1000 cold
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| increased availability of farms in Scandinavian countries.EuropeWinters in Central Europe were almost consistently cold between 1000 AD | instance of | which was caused mainly by economic factors | 0.80 | text |
| the late 19th century | instance of | which was caused mainly by economic factors | 0.80 | text |
| a changing landscape | instance of | Other impacts of climate change can be less apparent | 0.80 | text |
| increased availability of farms in Scandinavian countries | instance of | which was caused mainly by economic factors | 0.80 | text |
| Medieval Warm Period | related to Antarctica | The | 0.60 | section |
| Medieval Warm Period | related to Antarctica | MWP | 0.60 | section |
| Medieval Warm Period | related to Antarctica | Southern Ocean | 0.60 | section |
| Medieval Warm Period | related to Antarctica | MWP's | 0.60 | section |
| Medieval Warm Period | related to Antarctica | North Atlantic | 0.60 | section |
| Medieval Warm Period | related to Antarctica | Bransfield Basin | 0.60 | section |
| Medieval Warm Period | related to Antarctica | Antarctic Peninsula | 0.60 | section |
| Medieval Warm Period | related to Antarctica | LIA | 0.60 | section |
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