Abstract As the Earth continues to heat, paleoclimate evidence suggests transient reversals will result in accentuating the temperature polarities, leading to increase in the intensity and frequency of extreme weather events. Pleistocene paleoclimate records indicate interglacial temperature peaks have been are consistentlysucceeded by transient stadial freeze events,such as the Younger Dryas and the 8.5 kyr-old Laurentideice melt, attributed to cold[Read More...]
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