A threefold rise in widespread extreme rain events over central India

被引:478
作者
Roxy, M. K. [1 ]
Ghosh, Subimal [2 ]
Pathak, Amey [2 ]
Athulya, R. [1 ,3 ]
Mujumdar, Milind [1 ]
Murtugudde, Raghu [4 ]
Terray, Pascal [5 ,6 ]
Rajeevan, M. [1 ,7 ]
机构
[1] Indian Inst Trop Meteorol, Ctr Climate Change Res, Pune 411008, Maharashtra, India
[2] Indian Inst Technol, Dept Civil Engn, Bombay 400076, Maharashtra, India
[3] Cochin Univ Sci & Technol, Dept Phys Oceanog, Kochi 682016, India
[4] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA
[5] Univ Paris 06, UPMC, Sorbonne Univ, CNRS,IRD,MNHN,LOCEAN Lab, 4 Pl Jussieu, F-75005 Paris, France
[6] IITM, IISc, Indo French Cell Water Sci, IRD Joint Int Lab,NIO, Pune 411008, Maharashtra, India
[7] Govt India, Minist Earth Sci, Lodhi Rd, New Delhi 110003, India
来源
NATURE COMMUNICATIONS | 2017年 / 8卷
关键词
ASIAN SUMMER MONSOON; LOW-PRESSURE SYSTEMS; WARMING ENVIRONMENT; CLIMATE-CHANGE; PRECIPITATION EXTREMES; INCREASING TREND; DRY SPELLS; OCEAN; VARIABILITY; PREDICTION;
D O I
10.1038/s41467-017-00744-9
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Socioeconomic challenges continue to mount for half a billion residents of central India because of a decline in the total rainfall and a concurrent rise in the magnitude and frequency of extreme rainfall events. Alongside a weakening monsoon circulation, the locally available moisture and the frequency of moisture-laden depressions from the Bay of Bengal have also declined. Here we show that despite these negative trends, there is a threefold increase in widespread extreme rain events over central India during 1950-2015. The rise in these events is due to an increasing variability of the low-level monsoon westerlies over the Arabian Sea, driving surges of moisture supply, leading to extreme rainfall episodes across the entire central subcontinent. The homogeneity of these severe weather events and their association with the ocean temperatures underscores the potential predictability of these events by two-to-three weeks, which offers hope in mitigating their catastrophic impact on life, agriculture and property.
引用
收藏
页数:11
相关论文
共 76 条
  • [1] Indian Ocean Dipole modulates the number of extreme rainfall events over India in a warming environment
    Ajayamohan, R. S.
    Rao, Suryachandra A.
    [J]. JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN, 2008, 86 (01) : 245 - 252
  • [2] Increasing Trend of Synoptic Activity and Its Relationship with Extreme Rain Events over Central India
    Ajayamohan, R. S.
    Merryfield, William J.
    Kharin, Viatcheslav V.
    [J]. JOURNAL OF CLIMATE, 2010, 23 (04) : 1004 - 1013
  • [3] SENSITIVITY OF MONSOON CIRCULATIONS TO CHANGES IN SEA-SURFACE TEMPERATURES
    ALAPATY, K
    RAMAN, S
    MOHANTY, UC
    MADALA, RV
    [J]. ATMOSPHERIC ENVIRONMENT, 1995, 29 (16) : 2139 - 2156
  • [4] ALI H, 2017, SCI REP UK, V7
  • [5] Observed and projected urban extreme rainfall events in India
    Ali, Haider
    Mishra, Vimal
    Pai, D. S.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2014, 119 (22) : 12621 - 12641
  • [6] Atmospheric warming and the amplification of precipitation extremes
    Allan, Richard P.
    Soden, Brian J.
    [J]. SCIENCE, 2008, 321 (5895) : 1481 - 1484
  • [7] Moist Dynamical Linkage between the Equatorial Indian Ocean and the South Asian Monsoon Trough
    Annamalai, H.
    [J]. JOURNAL OF THE ATMOSPHERIC SCIENCES, 2010, 67 (03) : 589 - 610
  • [8] [Anonymous], 2009, CLIMATE DATA MONITOR
  • [9] CADET DL, 1987, MON WEATHER REV, V115, P653, DOI 10.1175/1520-0493(1987)115<0653:WVTOTI>2.0.CO
  • [10] 2