2017
DOI: 10.1007/s00382-017-3604-2
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Future projections of Indian summer monsoon rainfall extremes over India with statistical downscaling and its consistency with observed characteristics

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Cited by 39 publications
(15 citation statements)
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“…We studied the projected change in extreme rainfall events simulated by the high‐resolution RCM, by computing the index for very wet days, R95p (defined as the number of days when daily mean rainfall exceeds 95th percentile value during the present‐day simulation at each grid point), during JJAS season of 10‐year period from WRF_CCSM4_PD and WRF_CCSM4_FD simulations. It is found that there are widespread increase in the occurrence of wet days over most parts of the Indian region especially most of the coastal areas, central India, and northeast India (not shown) that is consistent with the statistical downscaling study by Shashikanth et al (). Future changes in R95p index for southern WG along with the high topography contours (for 980 and 1,800 m) and for CMZ are shown in Figure c.…”
Section: Projected Changes In Indian Summer Monsoonsupporting
confidence: 88%
“…We studied the projected change in extreme rainfall events simulated by the high‐resolution RCM, by computing the index for very wet days, R95p (defined as the number of days when daily mean rainfall exceeds 95th percentile value during the present‐day simulation at each grid point), during JJAS season of 10‐year period from WRF_CCSM4_PD and WRF_CCSM4_FD simulations. It is found that there are widespread increase in the occurrence of wet days over most parts of the Indian region especially most of the coastal areas, central India, and northeast India (not shown) that is consistent with the statistical downscaling study by Shashikanth et al (). Future changes in R95p index for southern WG along with the high topography contours (for 980 and 1,800 m) and for CMZ are shown in Figure c.…”
Section: Projected Changes In Indian Summer Monsoonsupporting
confidence: 88%
“…The annual average rainfall in this area is 200 to 500cm, which increases from the southwestern coastal plains to the mountain areas in the east due to the orographic effect of the Western Ghats (Kuriakose et al, 2009;Sajinkumar et al, 2011). Under the global climate change, extreme rainfall events have hit India frequently (Mishra et al, 2018) and the extreme rainfall events during the monsoon season are expected to increase (Hunt and Menon, 2020;Rai et al, 2019Rai et al, , 2020Shashikanth et al, 2018), making it more vulnerable to slope failures.…”
Section: Study Areamentioning
confidence: 99%
“…Between 1 June and 26 August 2018, the southern Indian state of Kerala witnessed the most severe extreme rainfall event since 1924 (Agarwal, 2018;Megha et al, 2019;Sankar, 2018;Vishnu et al, 2019). The torrential rains triggered several thousand landslides (Singh et al, 2018) and extensive flooding, affecting 5.4 million people in over 1200 villages and causing enormous property losses (buildings, roads, and agriculture damage) and more than 440 casualties (Mishra et al, 2018;Vishnu et al, 2019). Furthermore, the following year, from 8 to 14 August, 2019, Kerala was hit again by another extreme precipitation event, causing more than 100 deaths due to landslides and floods (Koshy, 2019).…”
Section: Introductionmentioning
confidence: 99%