Characteristics of meteorological droughts in northwestern India

被引:28
作者
Amrit, Kumar [1 ]
Pandey, Rajendra P. [2 ]
Mishra, Surendra K. [1 ]
机构
[1] Indian Inst Technol Roorkee, Dept Water Resources Dev & Management, Roorkee 247667, UK, India
[2] Natl Inst Hydrol, Roorkee 247667, UK, India
关键词
Northwestern India; Drought return period; Drought severity; Meteorological drought; SOUTHEASTERN UNITED-STATES; FREQUENCY-ANALYSIS; RIVER-BASIN; RETURN PERIOD; RAINFALL; SEVERITY; DURATION; RISK; PRECIPITATION; VARIABILITY;
D O I
10.1007/s11069-018-3402-0
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This study analyses regional drought characteristics (frequency, severity, and persistence) of meteorological droughts occurred in the northwestern parts falling under arid and semiarid regions of India with mean annual rainfall ranging between 100 and 900mm. A drought is defined as a season or a year with rainfall less than 75% of corresponding mean at a place. Long-term monthly rainfall records (1901-2013) of 90 districts of north-west India located in the states of Punjab, Haryana, Rajasthan and Gujarat are used in the analysis. The percentage departure of seasonal rainfall from long-term average rainfall has been used for identification of onset, termination, and quantification of drought severity. The average frequency varied from once every 3-4years. The westerly districts have an average drought return period of 3years, while districts lying toward the east had droughts once every 4years. Only four of the 90 districts in the study area experienced droughts once every 5years. Persistent droughts of 2, 3, and 4year duration occurred widely. Severe droughts occurred in the years 1904, 1905, 1911, 1918, 1931, 1939, 1985, 1986, 1987, 1993, and 2002, with an average frequency of severe drought events of one in 10years. The analysis presented in this paper improves understanding of the regional drought characteristics and will inform drought mitigations and strategies in these arid and semiarid areas.
引用
收藏
页码:561 / 582
页数:22
相关论文
共 91 条
[1]   Assessment of meteorological drought characteristics over Central India [J].
Amrit K. ;
Pandey R.P. ;
Mishra S.K. .
Sustainable Water Resources Management, 2018, 4 (04) :999-1010
[2]  
[Anonymous], 1976, REP PROGR REV 1
[3]   Climatic change in mountain regions: A review of possible impacts [J].
Beniston, M .
CLIMATIC CHANGE, 2003, 59 (1-2) :5-31
[4]   Changes in European drought characteristics projected by the PRUDENCE regional climate models [J].
Blenkinsop, S. ;
Fowler, H. J. .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2007, 27 (12) :1595-1610
[5]  
Byun HR, 1999, J CLIMATE, V12, P2747, DOI 10.1175/1520-0442(1999)012<2747:OQODSA>2.0.CO
[6]  
2
[7]   Drought Analysis Using Copulas [J].
Chen, Lu ;
Singh, Vijay P. ;
Guo, Shenglian ;
Mishra, Ashok K. ;
Guo, Jing .
JOURNAL OF HYDROLOGIC ENGINEERING, 2013, 18 (07) :797-808
[8]   DROUGHT OCCURRENCE PROBABILITIES AND RISKS OF DEPENDENT HYDROLOGIC PROCESSES [J].
Chung, Chen-hua ;
Salas, Jose D. .
JOURNAL OF HYDROLOGIC ENGINEERING, 2000, 5 (03) :259-268
[9]   REGIONAL FREQUENCY-ANALYSIS OF ANNUAL MAXIMUM STREAMFLOW DROUGHT [J].
CLAUSEN, B ;
PEARSON, CP .
JOURNAL OF HYDROLOGY, 1995, 173 (1-4) :111-130
[10]   Agricultural drought mitigation and management of sustained agricultural development in India [J].
Das, HP .
Natural Disasters and Extreme Events in Agriculture: Impacts and Mitigation, 2005, :277-303