Impact of agricultural water management interventions on upstream-downstream trade-offs in the upper Cauvery catchment, southern India: a modelling study*

被引:3
|
作者
Wable, Pawan S. [1 ]
Garg, Kaushal K. [1 ]
Nune, Rajesh [1 ]
Venkataradha, Akuraju [1 ]
Anantha, K. H. [1 ]
Srinivasan, Veena [2 ]
Ragab, Ragab [5 ]
Rowan, John [4 ]
Keller, Virginie [5 ]
Majumdar, Pradeep [3 ]
Rees, Gwyn [5 ]
Singh, Ramesh [1 ]
Dixit, Sreenath [1 ]
机构
[1] ICRISAT Dev Ctr, Int Crops Res Inst Semiarid Trop, Hyderabad 502324, Telangana, India
[2] Ashoka Trust Res Ecol & Environm ATREE, Bengaluru, India
[3] Indian Inst Sci IISc, Bengaluru, India
[4] Univ Dundee, Dundee, Scotland
[5] UK Ctr Ecol & Hydrol, Wallingford, Oxon, England
基金
英国自然环境研究理事会;
关键词
catchment treatment; reservoir inflow; surface runoff; water balance; LAND-USE CHANGES; BLUE NILE BASIN; SWAT MODEL; CLIMATE-CHANGE; RIVER-BASIN; HYDROLOGICAL RESPONSES; ECOSYSTEM SERVICES; FUTURE CLIMATE; CROP YIELD; SOIL;
D O I
10.1002/ird.2662
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
The Cauvery basin in southern India is experiencing transboundary issues due to increasing water demand. This study analysed water balance components and the impact of agricultural water management (AWM) interventions in the upper Cauvery catchment of the Cauvery basin. Results showed that the study catchment receives an average of 1280 mm of annual rainfall. Of this, 29% (370 mm) flows downstream, 54% (700 mm) contributes to evapotranspiration (ET) and 17% (215 mm) contributes to groundwater recharge and surface storage. Rainfall varies from 700 to 5400 mm and the Western Ghats (mountain pass) are the main source of freshwater generation. The estimated ET in different catchments ranged from 500 to 900 mm per annum. An increase in the allocation of fresh water supplied by all three reservoirs (Hemavathi, Harangi and KRS) was observed in the canal command areas, from 1450 million cubic metres (MCM) yr?(1) in 1971-1980 to 3800 MCM yr?(1) in 2001-2010. AWM interventions harvested 140-160 MCM (13-20 mm) of surface runoff upstream of the upper Cauvery and reduced inflow into the Krishnaraja Sagar reservoir by 2-6%. The study findings are useful for designing and planning suitable water management interventions at basin scale.
引用
收藏
页码:472 / 494
页数:23
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