Geo Map from Scientific Research

The same as in (a), but the temperature change is between short interstadial and stadial (simulated Overshoot minus Stadial phases), and Westerlies and low-level water vapor transport are during the short DO warming events. The time periods of simulated Overshoot, Interstadial and Stadial phases refer to Fig. 4a. The definition of short, intermediate-long and super-long interstadials refers to Fig. 3. TP indicates the approximate location of the Tibetan Plateau. DO Dansgaard-Oeschger.

DOI