Fig. 7: Warming mechanisms in different regions of the Eurasian continent.
From: Asynchronous abrupt warming across Eurasia since the 1980s
The figure illustrates the AMO-driven abrupt temperature changes over Eurasia since 1980, highlighting regional and seasonal differences in warming timing and mechanisms. Earliest and most pronounced warming occurred over the Mongolian Plateau and Central Asia due to lower heat capacity, reduced cloud cover, and decreased soil moisture. Europe experienced delayed warming influenced by oceanic moderation and cold advection, while the Mediterranean's warming was further slowed by increased precipitation and cloudiness.
