Terra/ASTER地表温度与地面观测气温的关系

IF 0.3 Q4 GEOGRAPHY, PHYSICAL
Konno Shohei, Izumi Takeki, Takahashi Hideo
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引用次数: 5

摘要

本研究利用Terra/ aster获取的地表温度(LST)数据,估算了一个丘陵地区不同地表覆盖类型在冬季晴朗无风夜晚的近地气温(Ta)。地表温度与Ta的温差(ΔT)与土地覆盖类型及其空间范围有关。在扩大的林地面积内,面积(ΔTm)的空间平均ΔT为−0.1°C,地表温度与Ta的关系变异性较小(标准差ΔT (SD)=0.8°C),相关性较高(Ta与LST的决定系数R2 =0.70)。这一结果表明,我们可以直接从该地区的地表温度来评估Ta。在裸地扩展区,ΔTm、SD和R2分别为- 1.5°C、0.9°C和0.85,表明通过ΔTm校正LST可以准确估计Ta。在人工土地扩展面积上,ΔTm呈现无统计学意义的趋势。在一种以上土地覆盖混合区域,混合区域林地的ΔTm、SD和R2分别为−0.8°C、0.9°C和0.71,这表明我们可以通过ΔTm校正LST来精确估算该区域的Ta。混交区裸地虽然ΔTm为−1.4℃,但变化较大(SD=1.4℃),相关性较低(R2=0.33)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Relationship between Terra/ASTER Land Surface Temperature and Ground-observed Air Temperature
This study estimated near-ground air temperature (Ta) from Terra/ASTER-obtained land surface temperature (LST) for different land cover categories in a hilly region under a clear and calm night in winter. Temperature differences (ΔT) between LST and Ta were related to the land cover categories and their spatial extents. In the extended area of forest land, spatially averaged ΔT in the area (ΔTm) was −0.1°C, and the relationship between LST and Ta showed less variability (standard deviation of ΔT (SD)=0.8°C) and high correlation (coefficient of determination between Ta and LST (R2)=0.70). This result suggests we can evaluate Ta directly from LST in this area. In the extended area of bare land, ΔTm, SD and R2 were −1.5°C, 0.9°C and 0.85, respectively, which indicated that accurate estimation of Ta is possible by correcting LST by ΔTm. In the extended area of artificial land, ΔTm showed statistically non-significant trend. In the case of intermingled area of more than one type of land cover, ΔTm, SD and R2 were −0.8°C, 0.9°C and 0.71 in the forest land of the intermingled area, which suggested that we can estimate Ta in this area precisely by correcting LST by ΔTm. In the bare land of the intermingled area, though ΔTm was −1.4°C, large variations (SD=1.4°C) and low correlations (R2=0.33) were found.
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CiteScore
1.50
自引率
0.00%
发文量
4
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