Abstract The Tibetan Plateau (TP) has experienced an accelerated wintertime warming in
recent decades under global warming, but consensus on its causes has not yet been …

In recent decades, the Barents Sea has warmed more than twice as fast as the rest of the
Arctic in winter, but the exact causes behind this amplified warming remain unclear. In this …

To analyze links among key processes that contribute to Arctic‐midlatitude teleconnections
we apply causal discovery based on graphical models known as causal graphs. First, we …

Future precipitation levels remain uncertain because climate models have struggled to
reproduce observed variations in temperature‐precipitation correlations. Our analyses of …

Global climate models, focused on projecting anthropogenic warming, have not detected an
increase in sea surface temperature (SST) at low latitudes comparable to the observed one …

Based on modern observations, historical proxy data, and climate model simulations, this
paper provides a comprehensive overview of the past, present and future evolution …

Recent research has shown that snow cover induces extreme wintertime cooling and has
detrimental impacts. Although the dramatic loss of Arctic sea ice certainly has contributed to …

Arctic warming has significant environmental and social impacts. Arctic long‐term warming
trend is modulated by decadal‐to‐multidecadal variations. Improved understanding of how …

Temperature anomalies considerably influence the regional climate and weather of the
extratropics. By the end of this century, climate models project an intensification of synoptic …

This study investigates the variation in available potential energy of stationary eddies in the
mid‐troposphere over the midlatitude Northern Hemisphere (30°–60° N) from 1950 to 2021 …