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Effect of the revisit interval and temporal upscaling methods on the accuracy of remotely sensed evapotranspiration estimates

机译:重访间隔和时间放大方法对遥感蒸散量估算精度的影响

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Accurate spatially distributed estimates of actual evapotranspiration (ET) derived from remotely sensed data are critical to a broad range of practical and operational applications. However, due to lengthy return intervals and cloud cover, data acquisition is not continuous over time, particularly for satellite sensors operating at medium (?~??100?m) or finer resolutions. To fill the data gaps between clear-sky data acquisitions, interpolation methods that take advantage of the relationship between ET and other environmental properties that can be continuously monitored are often used. This study sought to evaluate the accuracy of this approach, which is commonly referred to as temporal upscaling, as a function of satellite revisit interval. Using data collected at 20 Ameriflux sites distributed throughout the contiguous United States and representing four distinct land cover types (cropland, grassland, forest, and open-canopy) as a proxy for perfect retrievals on satellite overpass dates, this study assesses daily ET estimates derived using five different reference quantities (incident solar radiation, net radiation, available energy, reference ET, and equilibrium latent heat flux) and three different interpolation methods (linear, cubic spline, and Hermite spline). Not only did the analyses find that the temporal autocorrelation, i.e., persistence, of all of the reference quantities was short, it also found that those land cover types with the greatest ET exhibited the least persistence. This carries over to the error associated with both the various scaled quantities and flux estimates. In terms of both the root mean square error (RMSE) and mean absolute error (MAE), the errors increased rapidly with increasing return interval following a logarithmic relationship. Again, those land cover types with the greatest ET showed the largest errors. Moreover, using a threshold of 20?% relative error, this study indicates that a return interval of no more than 5?days is necessary for accurate daily ET estimates. It also found that the spline interpolation methods performed erratically for long return intervals and should be avoided.
机译:从遥感数据中得出的实际蒸散量(ET)的准确空间分布估算值对于广泛的实际和操作应用至关重要。但是,由于返回间隔时间长且云层密布,数据采集不能随时间连续进行,特别是对于以中等(?〜?100?m)或更高分辨率运行的卫星传感器。为了填补晴空数据采集之间的数据空白,经常使用利用ET和可以连续监视的其他环境属性之间关系的插值方法。这项研究试图评估这种方法的准确性,通常将其称为时间上移,作为卫星重访间隔的函数。本研究使用在美国各地连续分布的20个Ameriflux站点收集的数据(代表四种不同的土地覆盖类型(作物,草地,森林和开放式林冠))作为卫星越过日期的完美检索的代理,评估了每日ET估算值使用五个不同的参考量(入射太阳辐射,净辐射,可用能量,参考ET和平衡潜热通量)和三个不同的插值方法(线性,三次样条和Hermite样条)。分析不仅发现所有参考量的时间自相关(即持久性)都很短,而且还发现那些具有最大ET的土地覆盖类型的持久性最小。这会导致与各种缩放量和通量估计值相关的误差。就均方根误差(RMSE)和平均绝对误差(MAE)而言,随着对数关系的增加,误差随着返回间隔的增加而迅速增加。同样,那些具有最大ET的土地覆盖类型显示出最大的误差。而且,使用相对误差的20%阈值,这项研究表明,准确的每日ET估算需要不超过5天的返回间隔。还发现,样条插值方法在返回间隔较长时无法正常执行,应避免使用。

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