Arctic Warming and Eurasian Cooling: Weakening and Reemergence

Abstract

The observed Eurasian winter surface cooling from the 1990s to the early 2010s, which is contrary to global warming, has been extensively studied. Previous studies revealed that the surface cooling trend has significantly weakened in the past decade. Based on large‐ensemble simulations, this study reveals that the weakening of Eurasian surface cooling is primarily driven by the atmospheric internal variability, which coincides with the weakening of Arctic mid‐tropospheric warming and Eurasian mid‐tropospheric cooling. Negative Arctic Oscillation (−AO) and Ural blocking (UB) in combination dominate the intensity of Arctic mid‐tropospheric warming and Eurasian mid‐tropospheric cooling. In the future, there is a possibility that the severe Eurasian cooling trend with comparable magnitude to that during 1990–2013 may reemerge accompanied with Arctic mid‐tropospheric warming, in response to the decadal strengthening of −AO and UB. This may occur before the 2050s, when the atmospheric internal variability is able to overwhelm the effects of greenhouse gases.

Ural Blocking and the Amplitude of Wintertime Cold Surges over North China Detected by a Cooling Algorithm

“…Meanwhile, there are significant cold temperature anomalies over Siberia. The temperature contrast is known as the Warm Arctic-Cold Siberia (WACS) or Warm Arctic-Cold Eurasia (WACE) pattern [31], which is closely related to the upstream warm and downstream cold temperature advection of the Ural blocking high [32][33][34][35][36]. For weak and medium groups, the warm temperature anomalies can extend into the coastal areas of the Eurasian continent.…”