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Comparison of Leaf Area Index Surface Temperature and Actual Evapotranspiration Estimated Using the METRIC Model and In Situ Measurements

机译:使用METRIC模型和原位测量估算的叶面积指数表面温度和实际蒸散量的比较

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摘要

The verification of remotely sensed estimates of surface variables is essential for any remote sensing study. The objective of this study was to compare leaf area index (LAI), surface temperature (Ts), and actual evapotranspiration (ETa), estimated using the remote sensing-based METRIC model and in situ measurements collected at the satellite overpass time. The study was carried out at a commercial corn field in eastern South Dakota. Six clear-sky images from Landsat 7 and Landsat 8 (Path 29, Row 29) were processed and used for the assessment. LAI and Ts were measured in situ, and ETa was estimated using an atmometer and independent crop coefficients. The results revealed good agreement between the variables measured in situ and estimated by the METRIC model. LAI showed r2 = 0.76, and RMSE = 0.59 m2 m−2, the Ts comparison had an agreement of r2 = 0.87 and RMSE 1.24 °C, and ETa presented r2 = 0.89 and RMSE = 0.71 mm day−1.
机译:遥感估计的地表变量估计值对于任何遥感研究都是必不可少的。这项研究的目的是比较叶面积指数(LAI),表面温度(Ts)和实际蒸散量(ETa),它们是使用基于遥感的METRIC模型估算的,并在卫星越过时收集了实地测量值。这项研究是在南达科他州东部的一个商业玉米田进行的。处理了来自Landsat 7和Landsat 8(路径29,第29行)的六张晴空图像,并将其用于评估。 LAI和Ts是在原位测量的,ETa是使用测温仪和独立的作物系数估算的。结果显示就地测量和由METRIC模型估算的变量之间具有良好的一致性。 LAI显示r 2 = 0.76,RMSE = 0.59 m 2 m -2 ,Ts比较与r 2一致 = 0.87和RMSE 1.24°C,ETa表示r 2 = 0.89和RMSE = 0.71 mm天 -1

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