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首页> 外文期刊>Photogrammetric Engineering & Remote Sensing: Journal of the American Society of Photogrammetry >Determining Irrigated Areas and QuantifyingBlue Water Use in Europe Using Remote Sensing Meteosat Second Generation (MSG) products and Global Land Data AssimilationSystem (GLDAS) Data
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Determining Irrigated Areas and QuantifyingBlue Water Use in Europe Using Remote Sensing Meteosat Second Generation (MSG) products and Global Land Data AssimilationSystem (GLDAS) Data

机译:使用遥感气象卫星第二代(MSG)产品和全球土地数据同化系统(GLDAS)数据确定欧洲的灌溉面积并量化蓝色水的使用

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摘要

In this paper, we propose an innovative method for identifying irrigated areas and quantifying the blue evapotranspiration (ETb), or irrigation water evapotranspired from the field. The method compares actual ET (ETactuai), or crop water use, values from the Global Land Data Assimilation System (GLDAS) and remote sensing based (ET_(actua)) estimates obtained from Meteosat Second Generation (MSG) satellites. Since GLDAS simulations do not account for extra water supply due to irrigation, it is expected that they underestimate ET_(actual )during the cropping season in irrigated areas. However, remote sensing techniques based on the energy balance are able to observe the total ET_(actua). In order to isolate irrigation effects from other fluctuations that may lead to discrepancies between the different ET_(actual) products, the bias between model simulations and remote sensing observations was estimated using reference targets of rainfed (non-irrigated) croplands on a daily basis in different areas across the study region (Europe). Analysis of the yearly values of ETb (irrigated area and volume obtained for croplands in Europe for 2008) showed that the method identified irrigation when yearly values were higher than 50 mm. The accuracy of the methodwas assessed by analyzing the spatial representativity of the calculated biases and evaluating the daily ET_b values obtained. The irrigated areas were compared with the results provided by Siebert et al.(2007) and Thenkabail et al.(2009b), obtaining a spatial match of 47 and 72 percent, respectively, with overestimation of irrigated area on a country scale. Additional evaluation with the ETb results of Mekonnenand Hoekstra (2011) showed 75 percent of overlap for ±50 mm range. Finally, validation with in situ data on irrigation volumes proved the cogency of our method with less than 20 percent difference between derived and measured values.
机译:在本文中,我们提出了一种创新的方法来识别灌溉区域并量化从田间蒸发的蓝色蒸散量(ETb)或灌溉水。该方法比较了全球陆地数据同化系统(GLDAS)的实际ET(ETactuai)或作物用水量,以及从Meteosat第二代(MSG)卫星获得的基于遥感的估计(ET_(actua))估计值。由于GLDAS模拟不能解决灌溉带来的额外供水问题,因此预计它们会低估灌溉地区作物种植季节的ET_(实际)。但是,基于能量平衡的遥感技术能够观察到总的ET_(actua)。为了将灌溉影响与可能导致不同ET_(实际)产品之间差异的其他波动隔离开来,每天使用雨养(非灌溉)农田的参考目标估算模型模拟与遥感观测值之间的偏差。研究区域的不同区域(欧洲)。对ETb的年值(2008年欧洲农田的灌溉面积和获得的体积)进行的分析表明,该方法可在年值高于50 mm时识别灌溉。通过分析计算的偏差的空间代表性并评估获得的每日ET_b值来评估该方法的准确性。将灌溉面积与Siebert等人(2007)和Thenkabail等人(2009b)提供的结果进行比较,分别得到47%和72%的空间匹配率,而在全国范围内高估了灌溉面积。 Mekonnenand Hoekstra(2011)的ETb结果进行的其他评估显示,在±50 mm范围内有75%的重叠。最后,利用灌溉量的原位数据进行的验证证明了我们的方法的有效性,得出的值与测量值之间的差异小于20%。

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