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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Satellite-based water use dynamics using historical Landsat data (1984–2014) in the southwestern United States
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Satellite-based water use dynamics using historical Landsat data (1984–2014) in the southwestern United States

机译:基于卫星的水使用动态使用历史Landsat数据(1984-2014)在美国西南部

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AbstractRemote sensing-based field-scale evapotranspiration (ET) maps are useful for characterizing water use patterns and assessing crop performance. The relative impact of climate variability and water management decisions are better studied and quantified using historical data that are derived using a set of consistent datasets and methodology. Historical (1984–2014) Landsat-based ET maps were generated for major irrigation districts in California, i.e., Palo Verde and eight other sub-basins in parts of the middle and lower Central Valley. A total of 3396 Landsat images were processed using the Operational Simplified Surface Energy Balance (SSEBop) model that integrates weather and remotely sensed images to estimate monthly and annual ET within the study sites over the 31years. Model output evaluation and validation using gridded-flux data and water balance ET approaches indicated relatively good correspondence (R2up to 0.88, root mean square error as low as 14mm/month) between SSEBop ET and validation datasets. In a pairwise comparison, annual variability of agro-hydrologic parameters of actual evapotranspiration (ETa), land surface temperature (Ts), and runoff (Q) were found to be more variable than their corresponding climatic counterparts of atmospheric water demand (ETo), air temperature (Ta), and precipitation (P
机译:<![cdata [ 抽象 基于遥感的字段雕刻eVapotranspiration(et)地图对于用于表征水使用模式并评估作物性能的映射非常有用。使用使用一组一致的数据集和方法获得的历史数据更好地研究和量化气候变异性和水管理决策的相对影响。历史(1984-2014)在加利福尼亚州的主要灌溉区,即帕洛佛得多和中下部和下部地区部分地区的主要灌溉区产生了基于Landsat的ET地图。使用运行简化的表面能量平衡(SSEBOP)模型处理了3396个Landsat图像,该模型集成了天气和远程感测图像,以在31年的研究网站内估计每月和年度ET。模型输出评估和验证使用网格通量数据和水平衡ET方法表示相对良好的通信(R 2 高达0.88,根均方误差低至14mm /月)SSEBOP等和验证数据集之间。在成对比较中,实际蒸散的农业水文参数年度变异性( et a ),陆地温度( T s )和径流( q )比其对应的大气水需求相应的气候对应物更具变量( et O ),空气温度( T a )和降水( p

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