International Crops Research Institute for Semi-Arid Tropics (ICRISAT), Patancheru, Telangana 502324, India; Agricultural and Biological Engineering (ABE) Department, SWFREC, University of Florida (UF), Immokalee, FL 34142, United States.
Agricultural and Biological Engineering (ABE) Department, SWFREC, University of Florida (UF), Immokalee, FL 34142, United States.
Sci Total Environ. 2018 Sep 1;635:725-740. doi: 10.1016/j.scitotenv.2018.04.130. Epub 2018 Apr 24.
Simultaneous effects of future climate and irrigation intensification on surface and groundwater systems are not well understood. Efforts are needed to understand the future groundwater availability and associated surface flows under business-as-usual management to formulate policy changes to improve water sustainability. We combine measurements with integrated modeling (MIKE SHE/MIKE11) to evaluate the effects of future climate (2040-2069), with and without irrigation expansion, on water levels and flows in an agricultural watershed in low-storage crystalline aquifer region of south India. Demand and supply management changes, including improved efficiency of irrigation water as well as energy uses, were evaluated. Increased future rainfall (7-43%, from 5 Global Climate Models) with no further expansion of irrigation wells increased the groundwater recharge (10-55%); however, most of the recharge moved out of watershed as increased baseflow (17-154%) with a small increase in net recharge (+0.2mm/year). When increased rainfall was considered with projected increase in irrigation withdrawals, both hydrologic extremes of well drying and flooding were predicted. A 100-year flow event was predicted to be a 5-year event in the future. If irrigation expansion follows the historical trends, earlier and more frequent well drying, a source of farmers' distress in India, was predicted to worsen in the future despite the recharge gains from increased rainfall. Storage and use of excess flows, improved irrigation efficiency with flood to drip conversion in 25% of irrigated area, and reduced energy subsidy (free electricity for 3.5h compared to 7h/day; $1 billion savings) provided sufficient water savings to support future expansion in irrigated areas while mitigating well drying as well as flooding. Reductions in energy subsidy to fund the implementation of economically desirable (high benefit-cost ratio) demand (drip irrigation) and supply (water capture and storage) management was recommended to achieve a sustainable food-water-energy nexus in semi-arid regions.
未来气候和灌溉集约化对地表水和地下水系统的综合影响还不甚清楚。需要努力了解在常规管理下未来地下水的可利用情况以及相关地表水流量,以便制定政策变化来提高水资源可持续性。我们结合测量和综合模型(MIKE SHE/MIKE11)来评估未来气候(2040-2069 年)的影响,包括有无灌溉扩张,对印度南部低存储结晶含水层地区农业流域的水位和水流的影响。评估了需求和供应管理变化,包括提高灌溉水效率以及能源利用。未来降雨增加(5 个全球气候模型的 7-43%)而没有进一步扩大灌溉井,增加了地下水补给(10-55%);然而,大部分补给都流出流域,导致基流增加(17-154%),而净补给仅略有增加(+0.2mm/年)。当考虑到增加的降雨和预计的灌溉用水量增加时,预计会出现井干涸和洪水泛滥的极端水文事件。预测 100 年一遇的流量事件在未来将成为 5 年一遇的事件。如果灌溉扩张遵循历史趋势,尽管增加降雨会带来补给增加,但印度农民的困境之源——更早和更频繁的水井干涸,预计在未来会恶化。储存和利用多余的水流,在 25%的灌溉区将洪水转换为滴灌,减少能源补贴(与每天 7 小时相比,节省 10 亿美元,电费从免费 3.5 小时改为收费),这些措施提供了足够的水资源节约,以支持未来灌溉面积的扩大,同时缓解水井干涸和洪水泛滥问题。建议减少能源补贴,为实施经济上可取的(高成本效益比)需求(滴灌)和供应(水捕获和储存)管理提供资金,以实现半干旱地区的粮食-水-能源可持续性。