Arturo Reyes-González, J. Kjaersgaard, T. Trooien, C. Hay, L. Ahiablame
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引用次数: 3
摘要
利用复杂方程和遥感短波和热红外图像估算实际作物蒸散发(ET a)图可能具有挑战性,并且可能需要输入无法获得的数据。因此,在可获得的输入数据有限或所得到的ET估计有较大不确定性可接受的情况下,有机会创造一种更简单和更快的方法,使用较少的输入参数生成ET地图。我们比较了基于作物系数和ndvi的(K - c-NDVI)方法与全能量平衡(EB)方法估算的ET a。利用Landsat 7和Landsat 8的晴空图像对美国南达科他州东部两个生长季节玉米的ET a进行了处理和估算。结果表明,2015年和2016年生长季,K - c-NDVI方法的ET a值分别比EB方法低18%和11%。在研究期间,采用K - c-NDVI方法估算ET a的精度降低了17%。这两年的平均偏差误差为0.81 mm day -1,均方根误差(RMSE)为0.37 mm day -1。日平均ET a为5.3 mm day -1。K - c-NDVI方法对ET a的估计效果可以接受,表明该方法可以在集中的区域和场尺度上以最小的输入参数估计短时间内的ET a。
Assessing Accuracy of Vegetation Index Method to Estimate Actual Evapotranspiration
The estimation of actual crop evapotranspiration (ET a ) maps using complex equations and remotely sensed shortwave and thermal infrared imagery can be challenging and may require input data that are not available. There is an opportunity, therefore to create a simpler and faster method to generate ET a maps using fewer input parameters for situations where limited input data is available or greater uncertainty in the resulting ET estimates are acceptable. We compared the estimates of ET a produced by a crop coefficient and NDVI-based (K c-NDVI ) method to a full energy balance (EB) method. Clear sky images from Landsat 7 and Landsat 8 were processed and used for the ET a estimations from maize during two growing seasons in eastern South Dakota, USA. The results showed that the ET a values from the K c-NDVI method were lower than the ET a values from the EB method by 18% for 2015 and 11% for 2016 growing season. During study period the accuracy of ET a estimation decreased 17% with the K c-NDVI method. For both years the mean bias error was 0.81 mm day -1 and the root mean square error (RMSE) was 0.37 mm day -1 . The average daily ET a of 5.3 mm day -1 . The K c-NDVI method performed acceptable for ET a estimations, indicating that this method can be used to estimate ET a with minimum input parameters at focused regional and field scales for short time periods.