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Mapping actual evapotranspiration by combining landsat TM and NOAA-AVHRR images: Application to the Barrax area, Albacete, Spain

机译:通过结合Landsat TM和NOAA-AVHRR图像绘制实际的蒸散量:在西班牙阿尔巴塞特Barrax地区的应用

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摘要

A method that permits determination of actual evapotranspiration, ET, in heterogeneous areas has been proposed. It is based on the relation ET=ETm-B(T-s-T-sm), which combines meteorological, National Oceanic and Atmospheric Administration advanced very high resolution radiometer (NOAA-AVHRR), and Landsat thematic mapper (TM) data. Thus, the maximum evapotranspiration for each crop, ETm, is obtained from in situ measurements carried out in a meteorological station; the temperature difference between each pixel and the pixel that has the maximum evapotranspiration, T-s-T-sm, is calculated for each crop from NOAA-AVHRR data; and the crop distribution in the area is known through a Landsat TM image. The semi-empirical coefficient B is derived for each crop in two ways: (1) experimentally and (2) by the identification of crop structure parameters. We have applied the proposed method to the Barrax region, Albacete, whose main crops, maize (Zea mays L.) and barley (Ordeum vulgare L.), cover a 10 km x 10 km area. With Penman's method as the standard, a method validation was conducted and an acceptable precision was obtained (+/-0.8 mm day(-1) and +/-1.0 mm day(-1) for barley and maize, respectively). Finally, actual evapotranspiration images are supplied. (C) Elsevier Science Inc., 1998. [References: 23]
机译:已经提出了一种可以确定异质地区实际蒸散量ET的方法。它基于关系ET = ETm-B(T-s-T-sm),该关系结合了气象,国家海洋和大气管理局高级超高分辨率辐射计(NOAA-AVHRR)和Landsat专题测绘仪(TM)数据。因此,每种作物的最大蒸散量ETm是从气象站进行的原位测量获得的。根据NOAA-AVHRR数据,为每种作物计算每个像素与具有最大蒸散量的像素T-s-T-sm之间的温差;通过Landsat TM图像可以知道该地区的农作物分布。每种作物的半经验系数B可以通过两种方式得出:(1)实验和(2)通过确定作物结构参数。我们已将建议的方法应用到Barrax地区Albacete,其主要农作物玉米(Zea mays L.)和大麦(Ordeum vulgare L.)的面积为10 km x 10 km。以Penman方法为标准,进行了方法验证,并获得了可接受的精度(大麦和玉米分别为+/- 0.8 mm day(-1)和+/- 1.0 mm day(-1))。最后,提供了实际的蒸散量图像。 (C)Elsevier Science Inc.,1998年。[参考:23]

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