ty -jour a2 -donateo，antonio au -zhan，ming -jin au -xia，lingjun au -zhan，longfei au -wang，yuanhao py -2020 da -2020/12/08 ti-评估和分析土壤温度数据的评估和分析。Poyang Lake Basin，中国SP -8839111 VL -2020 AB-土壤温度反映了当地因素的影响，例如地区的植被，土壤和大气。因此，重要的是要了解土壤温度的区域变化。但是，鉴于缺乏足够的空间和/或时间覆盖的观察结果，通常很难使用观察数据来研究区域变化。基于Nanchang和Ganzhou站点的观察数据以及ERA-Interim/Land Reanalysis数据，本研究分析了Poyang Lake Basin上土壤温度的时空分布特征。检查了四个土壤深度，分别记录为ST1，ST2，ST3和ST4，为0-7、7-28、28-100和100–289厘米。结果表明，观察数据与不同深度的重新分析数据之间的密切相关。重新分析数据可能会在Poyang湖盆地上重现土壤温度的主要时空分布，但通常低估了其大小。从时间上讲，盆地有明显的变暖趋势。在季节性上，温度升高是春季最快的，除了ST4以外，春季最快，冬季最慢的温度升高。 The temperature increase was faster for ST1 than the other depths. The warming trend was almost the same for ST2, ST3, and ST4. An abrupt change of annual soil temperature at all depths occurred in 1997, and annual soil temperatures at all depths were abnormally low in 1984. Spatially, annual soil temperature decreased with latitude, except for the summer ST1. Because of the high temperature and precipitation in summer, the ST1 values were higher around the lake and the river. The climatic trend of soil temperature generally increased from south to north, which was opposite to the distribution of soil temperature. These findings provide a basis for understanding and assessing the variation of soil temperature in the Poyang Lake Basin. SN - 1687-9309 UR - https://doi.org/10.1155/2020/8839111 DO - 10.1155/2020/8839111 JF - Advances in Meteorology PB - Hindawi KW - ER -