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DOI | 10.1007/s00382-018-4357-2 |
Non-monsoonal precipitation response over the Western Himalayas to climate change | |
Krishnan, R.1; Sabin, T. P.1; Madhura, R. K.1; Vellore, R. K.1; Mujumdar, M.1; Sanjay, J.1; Nayak, S.2; Rajeevan, M.2 | |
2019-04-01 | |
发表期刊 | CLIMATE DYNAMICS |
ISSN | 0930-7575 |
EISSN | 1432-0894 |
出版年 | 2019 |
卷号 | 52页码:4091-4109 |
文章类型 | Article |
语种 | 英语 |
国家 | India |
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. |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000467187600017 |
WOS关键词 | EXTREME WINTER PRECIPITATION ; SOUTH ASIAN MONSOON ; MOUNTAIN REGIONS ; KARAKORAM ; DISTURBANCES ; VARIABILITY ; SURFACE ; TRENDS ; MODEL ; TEMPERATURES |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/181887 |
专题 | 气候变化 |
作者单位 | 1.Indian Inst Trop Meteorol, Ctr Climate Change Res, Pune 411008, Maharashtra, India; 2.Minist Earth Sci, 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]. CLIMATE DYNAMICS,2019,52:4091-4109. |
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,52,4091-4109. |
MLA | Krishnan, R.,et al."Non-monsoonal precipitation response over the Western Himalayas to climate change".CLIMATE DYNAMICS 52(2019):4091-4109. |
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