气候变化领域集成服务门户(CCPortal): Non-monsoonal precipitation response over the Western Himalayas to climate change

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DOI	10.1007/s00382-018-4357-2
	Non-monsoonal precipitation response over the Western Himalayas to climate change
	Krishnan R.; Sabin T.P.; Madhura R.K.; Vellore R.K.; Mujumdar M.; Sanjay J.; Nayak S.; Rajeevan M.
发表日期	2019
ISSN	0930-7575
起始页码	4091
结束页码	4109
卷号	52 期号:2020-07-08
英文摘要	Winter-to-early spring non-monsoonal precipitation over the Western Himalayas (WH) primarily comes from eastward propagating synoptic-scale weather systems known as western disturbances (WDs). Earlier studies have noted that an increasing trend of synoptic-scale WD activity in the past few decades has contributed to enhanced propensity of daily precipitation extremes over the WH, although it remains unclear as to whether these regional changes are manifestations of climate change. This issue is addressed by conducting a suite of long-term climate experiments using a global variable-grid climate model with high-resolution telescopic zooming over the South Asian region. Our findings highlight that human-induced climate change has implications on the rising trend of synoptic-scale WD activity and precipitation extremes over the WH during the recent few decades, and these changes cannot be explained by natural forcing alone. A stronger surface warming, in response to climate change, is noted over the vast expanse of the high-elevated eastern Tibetan Plateau relative to the western side. The model simulations show that strengthening of positive east–west temperature gradient across the Tibetan Plateau tends to alter the background mean circulation in a manner as to favor amplitude enhancements of the synoptic-scale WDs and orographic precipitation over the WH. With continuation of global warming in future and enhancement in the east–west temperature gradient across the Tibetan highlands, the trend of precipitation extremes over the WH and synoptic-scale WD activity are projected to rise into the twenty-first century. While the high-resolution simulations of this study offers promising potential to understand changes in synoptic-scale WD activity and precipitation extremes over the WH, further investigations are necessary to decipher the multi-scale behavior and intricacies of the Himalayan precipitation variability under changing climate. © 2018, Springer-Verlag GmbH Germany, part of Springer Nature.
语种	英语
scopus关键词	climate change; climate modeling; extreme event; future prospect; hydrological response; mountain region; orographic effect; precipitation (climatology); spring (season); synoptic meteorology; winter; China; Himalayas; Qinghai-Xizang Plateau; South Asia
来源期刊	Climate Dynamics
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/146428
作者单位	Centre for Climate Change Research, Indian Institute of Tropical Meteorology, Pashan, Pune, 411 008, India; Ministry of Earth Sciences, New Delhi, India
推荐引用方式 GB/T 7714	Krishnan R.,Sabin T.P.,Madhura R.K.,et al. Non-monsoonal precipitation response over the Western Himalayas to climate change[J],2019,52(2020-07-08).
APA	Krishnan R..,Sabin T.P..,Madhura R.K..,Vellore R.K..,Mujumdar M..,...&Rajeevan M..(2019).Non-monsoonal precipitation response over the Western Himalayas to climate change.Climate Dynamics,52(2020-07-08).
MLA	Krishnan R.,et al."Non-monsoonal precipitation response over the Western Himalayas to climate change".Climate Dynamics 52.2020-07-08(2019).