The leading mode of the atmospheric background flow over the North Atlantic–Arctic Ocean
(ie, 300-hPa meridional wind; V300-EOF1) exhibited notable decadal variations during 1979 …

Atmospheric water vapor content (WVC) is a critical factor for East Asian winter precipitation.
This study investigates the dominant modes of interannual variability in WVC over East Asia …

The East Asian winter monsoon (EAWM) is the key indicator for the cold surge activities,
influencing East Asia during winter, and the El Niño‐Southern Oscillation (ENSO) is one of …

The time-varying influences of the wintertime Arctic Oscillation (AO) on the concurrent East
Asian surface air temperature (EAT) are investigated based on JRA-55 reanalysis data …

This study discovers that the interannual synchronization of winter temperature anomalies
between northern Eurasia and North America is closely related to variation in the second …

Eurasian teleconnection pattern (EU) and its two variants (EU1 and EU2) are the
representative wintertime atmospheric teleconnections over Eurasian continent. They are …

The Arctic region warms about twice as much as the global average, and this so-called
Arctic amplification (AA) might increase the moisture flux towards Siberia (Cohen et al …

Abstract The East Asian winter monsoon (EAWM) consists of subsystems such as the
Siberian high, Aleutian low, East Asian trough, low-level northerly wind and high-level East …

Despite rapid global warming, Eurasia experienced unusual winter cooling from around
1992–2012, whose cause is still debated. By analyzing observations and model simulations …

This study investigated the relationship between the summer Arctic Dipole (AD) anomaly
and the climatic variability in Eurasia during the period 1979–2021. It was found that the …