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Comparison and evaluation of different dryness indices based on vegetation indices-land surface temperature/albedo feature space

机译:基于植被指数的不同干旱指标的比较与评价 - 土地表面温度/ Albedo特征空间

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Nowadays, there are many dryness indices based on vegetation indices (VI_s)-land surface temperature (T_s) feature space. Which dry-ness index should we use in dryness monitoring? The differences and capabilities for dryness monitoring among seven indices were evaluated in this study. These dryness indices were based on VI_s-T_s or Albedo feature space. For instance, Temperature Vegetation Dryness Index (TVDI) from a triangle NDVI (Normalized Difference Vegetation Index)-T_s feature space (TVDI_t), TVDI from bi-parabolic NDVI-T_s feature space (TVDI_c), TFDI from FPAR (Fraction of Absorbed Photosynthetically Active Radiation)-T_s feature space, TVDI from LAI (Leaf Area Index)-T_s feature space (TLDI), TVDI from EVI (Enhanced Vegetation Index)-T_s feature space (TEDI), TVDI from SAVI (Soil Adjusted Vegetation Index)-T_s feature space (TSDI) and Vegetation Condition Albedo Dryness Index (VCADI) from NDVI-Albedo feature space. In this study, the assimilated 5/10 cm depth soil moisture, field measured 10 cm depth soil moisture, precipitation, and the assimilated land surface temperature data were selected as the indicators to test the performance of each dryness index in two periods of 2013/2015 and three periods of 2018. The results showed that the spatial distributions of dryness from TVDI_c, TVDI_t, TFDI, TLDI, TEDI, and TSDI were similar, except for VCADI. The ability of TSDI and TVDI_t in dryness monitoring was not as good as TVDI_c and TEDI, however, the robustness of them was stable and can be an alternative dryness index. TFDI can be applied to evaluate dryness conditions, but its robustness was not stable and its monitoring performance was not as good as other indices in Shaanxi province, China. Although TLDI can detect dryness conditions when NDVI reached saturation, its robustness was worse than TEDI. When NDVI did not reach saturation, TVDI_c had the best ability in dryness monitoring. TEDI was the optimal dryness index when NDVI was approaching or reaching saturation. This study determined that NDVI reached saturation (LAI = 3) when its average value was >0.5368.
机译:如今,基于植被指数(VI_S) - 地表面温度(T_S)特征空间存在许多干旱指标。我们应该在干燥监测中使用哪种干燥的指数?本研究评估了七个指数中干燥监测的差异和能力。这些干燥度指数基于VI_S-T_S或Albedo特征空间。例如,来自三角形NDVI(归一化差异植被指数)的温度植被干燥指数(TVDI)-T_S特征空间(TVDI_T),来自Bi-Parafolic NDVI-T_S的TVDI功能空间(TVDI_C),来自FPAR的TFDI(Absted Leadered的分数)主动辐射)-T_S特征空间,来自Lai的TVDI(叶面积索引)-T_S特征空间(TLDI),来自EVI的TVDI(增强型植被指数)-T_S功能空间(TEDI),来自SAVI的TVDI(土壤调整后植被指数) - 来自NDVI-Albedo特色空间的T_S特征空间(TSDI)和植被条件Albedo Drice Index(VCadi)。在这项研究中,选择的5/10cm深度土壤水分,田间测量10厘米深度土壤水分,降水,并选择同化的陆地温度数据作为测试每年2013年两个时期每个干燥指数的性能的指标/ 2015年和2018年的三个时期。结果表明,除了VCADI之外,TVDI_C,TVDI_T,TFDI,TDI,TFDI和TSDI的干燥空间分布相似。 TSDI和TVDI_T在干燥监测中的能力并不像TVDI_C和TEDI那么好,但是,它们的稳健性稳定,可以是替代的干旱指数。 TFDI可以应用于评估干燥条件,但其鲁棒性并不稳定,其监测性能并不像陕西省的其他指数一样好。尽管当NDVI达到饱和时,TLDI可以检测干燥条件,但其鲁棒性比TEDI更差。当NDVI没有达到饱和时,TVDI_C具有干燥监测的最佳能力。当NDVI接近或达到饱和时,Tedi是最佳的干燥指数。该研究确定当其平均值> 0.5368时,NDVI达到饱和度(Lai = 3)。

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