# The Karakoram/Western Tibetan vortex: seasonal and year-to-year variability

Climate Dynamics, Feb 2018

The “Karakoram Vortex” (KV), hereafter also referred to as the “Western Tibetan Vortex” (WTV), has recently been recognized as a large-scale atmospheric circulation system related to warmer (cooler) near-surface and mid-lower troposphere temperatures above the Karakoram in the western Tibetan Plateau (TP). It is characterized by a deep, anti-cyclonic (cyclonic) wind anomaly associated with higher (lower) geopotential height in the troposphere, during winter and summer seasons. In this study, we further investigate the seasonality and basic features of the WTV in all four seasons, and explore its year-to-year variability and influence on regional climate. We find the WTV accounts for the majority of year-to-year circulation variability over the WTP as it can explain over 50% ($${R^2} \geqslant 0.5$$) variance of the WTP circulation on multiple levels throughout the troposphere, which declines towards the eastern side of the TP in most seasons. The WTV is not only more (less) active but also has a bigger (smaller) domain area, with a deeper (shallower) structure, in winter and spring (summer and autumn). We find that the WTV is sensitive to both the location and intensity of the Subtropical Westerly Jet (SWJ), but the relationship is highly dependent on the climatological mean location of SWJ axes relative to the TP in different seasons. We also show that the WTV significantly modulates surface and stratospheric air temperatures, north–south precipitation patterns and total column ozone surrounding the western TP. As such, the WTV has important implications for the understanding of atmospheric, hydrological and glaciological variability over the TP.

This is a preview of a remote PDF: https://link.springer.com/content/pdf/10.1007%2Fs00382-018-4118-2.pdf

Xiao-Feng Li, Hayley J. Fowler, Nathan Forsythe, Stephen Blenkinsop, David Pritchard. The Karakoram/Western Tibetan vortex: seasonal and year-to-year variability, Climate Dynamics, 2018, 1-24, DOI: 10.1007/s00382-018-4118-2