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Postglacial Sea level Rise Curve and Meltwater Pulses (MWP)
Postglacial Sea level Rise Curve and Meltwater Pulses (MWP)
Greenland temperature trend after the Last Glacial Maximum, derived from the Greenland ice cores. It shows local warming of the Late Glacial Interstad
Greenland temperature trend after the Last Glacial Maximum, derived from the Greenland ice cores. It shows local warming of the Late Glacial Interstadial, ( ), followed by very low temperatures for the most part of the Younger Dryas, rapidly rising afterwards to reach the level of the globally warm Holocene. This trend is not representative of the global temperatures - Southern Hemisphere experienced opposite changes during the Late Glacial Interstadial and the Younger Dryas.