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Study on Drought-stricken and Drought-damaged farmland in China during 1982~2001 with Remote Sensing

机译:1982〜2001年中国中国干旱和干旱受损农田的研究与遥感

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The water deficit index (WDI) was introduced briefly. And the 10-day WDI images were estimated with the 1982~2001 NOAA AVHRR dataset of NDVI, light temperature of channel 4 and channel 5. Based on the 10-day WDI images, the pixels that represent the drought-stricken and drought-damaged farmland were picked up for every year. Only when WDI greater than 0.75 during crop development (March ~October) happened in more than one decades, the pixel was thought as drought-stricken. And WDI greater than 0.7 happened in more than two continuous decades, the pixel was treated as drought-damaged. The remotely sensed acreage of drought-stricken and drought-damaged farmland have similar dynamics as the statistical results except in early 1980s. I would like to oppugn the statistical results in early 1980s. Anyway, results showed that remotely sensed WDI is useful in retrieving drought stricken and damaged farmland and it also verified the rationality of WDI in evaluating regional soil water status.
机译:简要介绍了水资源赤字指数(WDI)。估计了10天的WDI图像,估计了NDVI的1982〜2001年NOAA数据集,频道4和通道5.基于10天的WDI图像,该像素代表干旱灾害和干旱损坏的像素农田每年都被拿起。只有在农作物发展期间大于0.75的WDI(三月〜10月)发生在超过一十年的时候,才会被认为是干旱灾害的。在两年以上的几十年中,WDI大于0.7,像素被视为干旱损坏。除了20世纪80年代初,偏远感受到的干旱和干旱损坏的农田的种植面积与统计结果相似。我想在20世纪80年代初抵抗统计结果。无论如何,结果表明,遥感的WDI在检索干旱和受损的农田中有用,而且还验证了WDI在评估区域土壤水分状态方面的合理性。

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