2019
DOI: 10.1007/s12040-019-1177-7
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The impacts of the approaching western disturbances (WDs) on the surface meteorological variables over the north-west Himalaya (NWH), India

Abstract: Eastward-moving upper air troughs in the subtropical westerlies, commonly known as the western disturbances (WDs) in the Asian subcontinent, are primary sources of precipitation over the northwest Himalayan (NWH) region and the northern plains of India during winter. Many simulation case studies with the help of numerical weather prediction models and a few observational case studies have been conducted to understand the spatial structure, dynamics, energy and weather associated with the WDs over the NWH in th… Show more

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Cited by 6 publications
(3 citation statements)
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“…Also of note is the cooler lower troposphere over Pakistan and North India in SIME-CAM5 compared to CTRL-CAM5. This is very unlikely to be related to the reduced WD activity in SIME-CAM5, since WDs are known to reduce near-surface temperature in this region through enhanced cloud cover, snowfall, and by advection of cool air from higher latitudes (Hunt et al, 2018b;Singh et al, 2019;Sandeep and Prasad, 2020). Instead, this may be related to a continued strengthening of the Karakoram anomaly (Farinotti et al, 2020) or increased cloudburst activity (Kumar et al, 2018).…”
Section: Resultsmentioning
confidence: 98%
“…Also of note is the cooler lower troposphere over Pakistan and North India in SIME-CAM5 compared to CTRL-CAM5. This is very unlikely to be related to the reduced WD activity in SIME-CAM5, since WDs are known to reduce near-surface temperature in this region through enhanced cloud cover, snowfall, and by advection of cool air from higher latitudes (Hunt et al, 2018b;Singh et al, 2019;Sandeep and Prasad, 2020). Instead, this may be related to a continued strengthening of the Karakoram anomaly (Farinotti et al, 2020) or increased cloudburst activity (Kumar et al, 2018).…”
Section: Resultsmentioning
confidence: 98%
“…WDs can cause coldwaves -prolonged periods of below-average temperature -both through cold air advection by northerlies in the rear sector and through reduced insolation caused by their deep and widespread cloud cover, as well as radiative conditions that favour surface frost (Mooley, 1957). Recent composite studies of WD structure have shown that they are associated with a lower-tropospheric cold anomaly of 2-3K (Hunt et al, 2018b;Singh et al, 2019b;. In case studies, WDs have been associated with considerably more severe coldwaves (Gupta et al, 2019).…”
Section: Coldwavesmentioning
confidence: 99%
“…WDs can cause coldwaves -prolonged periods of below-average temperature -both through cold air advection by northerlies in the rear sector and through reduced insolation caused by their deep and widespread cloud cover, as well as radiative conditions that favour surface frost (Mooley, 1957). Recent composite studies of WD structure have shown that they are associated with a lower-tropospheric cold anomaly of 2-3K (Hunt et al, 2018b;Singh et al, 2019b;. In case studies, WDs have been associated with considerably more severe coldwaves (Gupta et al, 2019).…”
Section: Coldwavesmentioning
confidence: 99%