Preprints
https://doi.org/10.5194/egusphere-2024-2845
https://doi.org/10.5194/egusphere-2024-2845
19 Sep 2024
 | 19 Sep 2024

PDO-driven interdecadal variability of snowfall over the Karakoram and Western Himalaya

Priya Bharati, Pranab Deb, and Kieran M. R. Hunt

Abstract. Our study reveals that the negative phase of the Pacific Decadal Oscillation (PDO−) leads to increased winter (DJF) snowfall in the Karakoram and Western Himalayas (KH) from 1940 to 2022. Interdecadal variations in DJF snowfall during the PDO− are attributed to deep convection and adiabatic cooling near the tropopause in both the northwest Pacific and KH region. Additionally, a wave-like pattern characterized by a trough (anomalous cyclone) north of KH and a ridge (anomalous Tibetan Plateau anticyclone) east of KH in the upper atmosphere, along the northward shift of the DJF Subtropical Jet (STJ) was observed. A strong positive correlation between DJF STJ strength and DJF snowfall in KH as well as a significant negative correlation between DJF STJ strength and DJF PDO, suggests a wave response over KH to the direct forcing over the northwest Pacific Ocean. The intensified STJ across KH results in higher frequency of Western disturbances, leading to anomalous moisture convergence and increased DJF precipitation in the region during the PDO−. These findings hold significant implications for the decadal predictability of winter snowfall in KH by the various phases of PDO.

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Journal article(s) based on this preprint

13 Feb 2025
Pacific Decadal Oscillation-driven interdecadal variability of snowfall over the Karakoram and the Western Himalayas
Priya Bharati, Pranab Deb, and Kieran Mark Rainwater Hunt
Weather Clim. Dynam., 6, 197–210, https://doi.org/10.5194/wcd-6-197-2025,https://doi.org/10.5194/wcd-6-197-2025, 2025
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The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.

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Snowfall in the Karakoram and Western Himalayas (KH) correlates negatively with the Pacific...

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