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New refinements and validation of the collection-6 MODIS land-surface temperature/emissivity product

机译:Collection-6 MODIS地表温度/发射率产品的新改进和验证

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According to the radiance-based (R-based) validation of the collection-5 or version-5 (C5 or V5) Terra and Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) land-surface temperature (LST) level-2 products at 42 sites in a wide LST range in different seasons and years, the LST errors are within ±. 2. K (within ±. 1. K in most cases) for all the sites but six bare soil sites. The V5 LSTs are underestimated by more than 2. K and up to 4.5. K at the desert site near In-salah, Algeria. Three refinements were implemented in the V6.3.0 daily LST Product Generation Executive (PGE)16 code: 1) refine the original viewing angle dependent split-window algorithm by adding two sets of coefficients separately for retrieval of daytime and nighttime LSTs at bare soil pixels in the hot and warm bare soil zone (HAWBSZ) within latitude range from 38° to 49.5°, 2) adjust the emissivity difference in bands 31 and 32 for bare soil pixels in HAWBSZ, and 3) incorporate the new refined split-window algorithm into the dayight algorithm for retrieving surface emissivity and temperature values at 6. km grids in HAWBSZ. The V6.3.0 PGE16 code was tested with C6 Aqua and Terra MODIS input data over a period of one year or longer in selected tile regions. The resulting C6 level-2 LST products were evaluated at five bare soil sites in north Africa, where radiosonde observation data for atmospheric temperature and water vapor profiles are available, with 12 R-based validation data sets as follows: the mean LST error is within ±. 0.6. K in 10 validate data sets, 0.8. K in one data set (for daytime LSTs at SVU site) and 1.9. K in another set (for daytime LSTs at Farafra site). The standard deviation of the C6 LST validation errors is less than 0.5. K in all the 12 validation data sets but the data set for daytime LSTs at Farafra site at 0.7. K. Statistical and viewing angle dependence analyses of the retrieved surface emissivity values also indicate that the C6 level-3 LST products are much better than the previous C4.1 and C5 products.
机译:根据集合5或版本5(C5或V5)的Terra-Aqua中分辨率成像光谱仪(MODIS)地表温度(LST)2级产品的基于辐射度(基于R)的验证在不同季节和年份的大范围LST中,LST误差均在±以内。除六个裸露的土壤位点外,所有位点均为2. K(大多数情况下在±1. K之内)。 V5 LST被低估了2.K以上,最高为4.5。 K在阿尔及利亚因萨拉附近的沙漠地带。在V6.3.0每日LST产品生成执行程序(PGE)16代码中实现了三项改进:1)通过分别添加两组系数以在裸露的土壤像素处检索白天和夜间的LST,改进原始的依赖于视角的拆分窗口算法。在38°至49.5°纬度范围内的热和暖裸土区(HAWBSZ)中,2)调整HAWBSZ中裸土像素的波段31和32的发射率差异,以及3)合并了新的改进的分割窗口算法进入白天/夜晚算法,以获取HAWBSZ中6. km网格处的表面发射率和温度值。 V6.3.0 PGE16代码已在选定的图块区域中使用C6 Aqua和Terra MODIS输入数据进行了为期一年或更长时间的测试。在北非的五个裸露土壤场所对所得的C6 2级LST产品进行了评估,那里有有关大气温度和水蒸气剖面的探空仪观测数据,其中包括12个基于R的验证数据集:平均LST误差在±。 0.6。 10个验证数据集中的K为0.8。一个数据集中的K(用于SVU站点的白天LST)和1.9。另一组中的K(用于Farafra站点的白天LST)。 C6 LST验证错误的标准偏差小于0.5。在所有12个验证数据集中,K除外,但Farafra站点的白天LST的数据集为0.7。 K.对检索到的表面发射率值的统计和视角依赖性分析还表明,C6 3级LST产品要比以前的C4.1和C5产品好得多。

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