Abstract As the dominant atmospheric circulation pattern over the western Tibetan Plateau (TP), the Western Tibetan Vortex (WTV) exerts substantial control on springtime 2 m surface air temperature (T2m). However, its underlying radiative processes remain unclear. This study integrates GEWEX satellite observations with ERA5 and MERRA‐2 reanalysis, applying surface energy balance diagnostics to quantify the WTV’s radiative forcing on T2m variability. We find the WTV explains ∼66% of T2m variance (R = 0.81) across the western TP and the adjacent Southwest Asia. Downward shortwave radiation (DSW) emerges as the primarily radiative factor modulated by the WTV via cloud radiative forcing (CRF) processes. Specifically, anticyclonic WTV events reduce cloudiness, generating positive CRF anomalies that enhancing surface DSW and cause warming. Conversely, cyclonic events increase cloudiness, producing negative CRF anomalies that diminish DSW and induce cooling. These findings advance understanding of the radiative processes by which the upper circulations modulate the surface climate over the TP.
Observations from the Little Bunker
Last updated: February 24, 2026 10:22 PM
Atmospheric CO₂
429.9 ppm
+17.3
ppm/year
Atmospheric CH₄
1946.47 ppb
+6.49
ppb/year
Global Temperature
+1.48 °C
Peak: +1.73°C
World Population
8.1 billion
+67
million/year