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Disentangling the Response of Vagetation to Rainfall Anomalies for Drought Evaluation Over the Indus Basin

机译:解开迷惑对茚上盆地干旱评估的降雨异常的响应

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Drought hazards induced by continuous water shortage may damage crop growth and cause severe grain loss. With one of the most intensive irrigation systems, the Indus basin has supported agriculture for millennia and feeds up more than 300 million people. The water supply for the basin scale irrigation is dominated by melting of glaciers and snowpack in the Himalaya and Karakoram mountain ranges, ground water as well as the Asian monsoon rainfall. To understand how ecosystems over the Indus basin with such complex water supply mechanism response to meteorological drought (rainfall shortage) is critical for future drought monitoring and evaluation applications. This study evaluated the spatiotemporal response pattern using correlation analysis of rainfall anomalies (3-month scale) and vegetation anomalies (1-month scale) with long-term satellite observations. The result found that the vegetation over northern Indus valley significantly coupled to rainfall variation during both summer (Kharif) and winter (Rabi) monsoon season. While significant response during Kharif season also was identified over the southern part, especially over the Punjab, where was well equipped with irrigation system. We concluded that special attention should be paid to drought assessment in terms of rainfall and vegetation anomaly over the Indus basin.
机译:连续缺水诱导的干旱危害可能会损害作物生长并导致严重的晶粒损失。由于最强烈的灌溉系统之一,印度盆地支持农业为千年,并饲养超过3亿人。盆地灌溉的供水是通过喜马拉雅山脉和卡拉库拉姆山脉,地面水以及亚洲季风降雨的冰川和积雪融化。要了解在梧桐盆地的生态系统如何具有这种复杂的供水机制对气象干旱(降雨短缺)对未来的干旱监测和评估应用至关重要。该研究评估了使用长期卫星观测的降雨异常(3个月标度)和植被异常(1个月规模)的相关分析的时空响应模式。结果发现,在植被北部印度河流域无论在夏季(秋收)和冬季(拉比)季风季节期间显著耦合到降雨量的变化。虽然在Kharif季期间的重大反应也被南部的核查,特别是在旁遮普席上,在那里配备了灌溉系统。我们得出结论,在印度盆地的降雨和植被异常方面应特别注意干旱评估。

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