2017
DOI: 10.1007/s13143-017-0006-7
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An investigation of reduced western disturbance activity over Northwest India in November - December 2015 compared to 2014 - A case study

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Cited by 9 publications
(8 citation statements)
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“…Winter precipitation is found to be more at higher altitudes as compared to lower altitudes. During his research done in 2015 low presipitation is recorded in November and December month lead to bad effect to winter crop and more air pollution in city [9]. Decreasing trend is seen in frequency of WDs over Himachal Pradesh in his research of time period 1997-2007 [10].…”
Section: Rainfall Behavior In the Areamentioning
confidence: 93%
“…Winter precipitation is found to be more at higher altitudes as compared to lower altitudes. During his research done in 2015 low presipitation is recorded in November and December month lead to bad effect to winter crop and more air pollution in city [9]. Decreasing trend is seen in frequency of WDs over Himachal Pradesh in his research of time period 1997-2007 [10].…”
Section: Rainfall Behavior In the Areamentioning
confidence: 93%
“…Some WDs bring precipitation and rapid surface wind‐speed in the IGP thus modulating air quality (Pawar et al., 2015). For instance, low WD activity in December 2015 likely contributed to extremely high air pollution in New Delhi (Basu et al., 2017). Following Midhuna et al.…”
Section: Change In Local Meteorology With Climate Change and Implicat...mentioning
confidence: 99%
“…Some WDs bring precipitation and rapid surface wind-speed in the IGP thus modulating air quality (Pawar et al, 2015). For instance, low WD activity in December 2015 likely contributed to extremely high air pollution in New Delhi (Basu et al, 2017). Following Midhuna et al (2020) we diagnose the change in WD activity using the Western disturbance index (WDI), the difference in geopotential heights between 850 and 200 hPa over the region 25-40°N 60-80°E.…”
Section: Change In Local Meteorology With Climate Change and Implicat...mentioning
confidence: 99%
“…Devi et al (2020) constructed a simple seasonal forecast model to predict winter precipitation over the Western Himalaya and found a strong negative correlation with the NAO (− 0.57). Basu et al (2017) attributed a weak 2015 winter monsoon to reduced WD activity caused by positive phases of ENSO and the NAO, stating that the positive NAO set up an unfavourable standing wave in the subtropical jet with a blocking anticyclonic anomaly over the subcontinent. Using plankton-based proxies, Munz et al (2017) showed that intense winter monsoons since 1750 coincided with strong negative phases of the NAO.…”
Section: Introductionmentioning
confidence: 99%