Monitoring groundwater fluctuations over India during Indian Summer Monsoon (ISM) and Northeast monsoon using GRACE satellite: Impact on agriculture

被引:15
作者
Singh, Anil Kumar [1 ,2 ]
Tripathi, Jayant Nath [2 ]
Kotlia, Bahadur Singh [3 ]
Singh, K. K. [1 ]
Kumar, Amit [1 ]
机构
[1] Indian Meteorol Dept, New Delhi 110003, India
[2] Univ Allahabad, Dept Earth & Planetary Sci, Allahabad 211002, Uttar Pradesh, India
[3] Kumaun Univ, Ctr Adv Study Geol, Naini Tal 263001, India
关键词
GRACE; GLDAS; TWS; Indian Summer Monsoon (ISM); NE monsoon; India; IMD GRIDDED RAINFALL; PRECIPITATION VARIABILITY; CENTRAL HIMALAYA; WATER-RESOURCES; CLIMATE-CHANGE; HIGH-PLAINS; DEPLETION;
D O I
10.1016/j.quaint.2018.10.036
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Since 2002, Gravity Recovery and Climate Experiment (GRACE) satellite has provided monthly estimates of land water storage variations by monitoring time-variable components of earths gravity field. We present GRACE satellite RLO5 gravity data at 1 degrees x 1 degrees resolution to estimate terrestrial water storage change (surface water + groundwater) over India during Indian Summer Monsoon (ISM) and Northeast (NE) monsoon periods for the year 2015. As the NE monsoon was above normal in 2015, groundwater storage has increased significantly. By using GLDAS2.1 (1 degrees x 1 degrees resolution data) land surface state variables, we deduced as to how Terrestrial Water Storage (TWS) is partitioned into canopy water and soil moisture components. By computing storage changes in GRACE TWS, Global Land Data Assimilation System (GLDAS) land surface state variables and by using a terrestrial-based water balance approach, we calculated changes in the groundwater storage. The GRACE data indicate the variation of 15 cm in the TWS during the ISM period over India and a gain of 2.35 cm NE season over Peninsular India. After the ISM season, the groundwater storage was increased by 13 cm over India and 6.45 cm during the NE monsoon over Peninsular India. We also observed a high run-off (sub-surface + surface) rate in both the monsoon periods. The accumulated rainfall over India was estimated as 76.58 cm out of which 33.8 cm was computed as run-off (ISM season). Similarly, the mean rainfall in Peninsular India was calculated as 8 cm out of which 3.86 cm was approximated as run-off (NE monsoon season).
引用
收藏
页码:342 / 351
页数:10
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