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

机译:1982-2001年中国干旱干旱地区的遥感研究

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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:简要介绍了缺水指数(WDI)。并使用1982-2001年NDVI的NOAA AVHRR数据集,通道4和通道5的光温估算了10天的WDI图像。基于10天的WDI图像,代表着遭受干旱和干旱破坏的像素每年都要收拾农田。只有在作物发育过程中(3月〜10月)的WDI大于0.75时,像素才被认为是干旱的。并且WDI大于0.7连续两个多十年发生了,该像素被视为干旱损坏。除1980年代初以外,受干旱和干旱破坏的农田的遥感面积与统计结果具有相似的动态。我想反对1980年代初的统计结果。无论如何,结果表明,遥感WDI可用于恢复干旱和受损的农田,也证明了WDI在评估区域土壤水状况方面的合理性。

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