Retrieval of high spatial resolution mountainous land surface temperature considering topographic and adjacency effects

IF 6 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Science China Earth Sciences Pub Date : 2024-09-02 DOI:10.1007/s11430-023-1398-2
Zhiwei He, Bohui Tang, Zhaoliang Li
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Abstract

Land surface temperature (LST) is a key parameter reflecting the interaction between land and atmosphere. Currently, thermal infrared (TIR) quantitative remote sensing technology is the only means to obtain large-scale, high spatial resolution LST. Accurately retrieving high spatial resolution mountainous LST (MLST) plays an important role in the study of mountain climate change. The complex terrain and strong spatial heterogeneity in mountainous areas change the geometric relationship between the surface and satellite sensors, affecting the radiation received by the sensors, and rendering the assumption of planar parallelism invalid. In this study, considering the influence of complex terrain in mountainous areas on atmospheric downward radiation and the thermal radiation contribution of adjacent pixels, a mountainous TIR radiative transfer model based on the sky view factor was developed. Combining with the atmospheric radiative transfer model MODTRAN 5.2, a nonlinear generalized split-window algorithm suitable for high spatial resolution MLST retrieval was constructed and applied to Landsat-9 TIRS-2 satellite TIR remote sensing data. The analysis results indicate that neglecting the topographic and adjacency effects would lead to significant discrepancies in LST retrieval, with simulated data showing LST differences of up to 2.5 K. Furthermore, due to the lack of measured MLST in the field, the MLST accuracy obtained by this retrieval method was indirectly validated using the currently recognized highest-accuracy forward 3D radiative transfer model DART. The MLST and emissivity were input into the DART model to simulate the brightness temperature at the top of the atmosphere (TOA) of Landsat-9 band 10, and compared with the brightness temperature at TOA of Landsat-9 band 10. The RMSE (Root Mean Square Error) for the two subregions was 0.50 and 0.61 K, respectively, indicating that the method proposed can retrieve high-precision MLST.

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考虑地形和毗邻效应的高空间分辨率山地地表温度检索
陆地表面温度(LST)是反映陆地与大气相互作用的一个关键参数。目前,热红外定量遥感技术是获取大尺度、高空间分辨率 LST 的唯一手段。准确获取高空间分辨率的山区 LST(MLST)对研究山区气候变化具有重要作用。山区复杂的地形和强烈的空间异质性改变了地表和卫星传感器之间的几何关系,影响了传感器接收的辐射,使平面平行假设失效。本研究考虑到山区复杂地形对大气向下辐射和相邻像素热辐射贡献的影响,建立了基于天空视角因子的山区 TIR 辐射传递模型。结合大气辐射传输模型 MODTRAN 5.2,构建了适用于高空间分辨率 MLST 检索的非线性广义分窗算法,并将其应用于 Landsat-9 TIRS-2 卫星 TIR 遥感数据。分析结果表明,忽略地形和邻近效应会导致 LST 检 测结果存在显著差异,模拟数据显示 LST 差异高达 2.5 K。此外,由于缺乏实地测量的 MLST,因此使用目前公认精度最高的前向三维辐射传递模型 DART 间接验证了该检索方法获得的 MLST 精度。将 MLST 和发射率输入 DART 模型,模拟 Landsat-9 波段 10 的大气顶部(TOA)亮度温度,并与 Landsat-9 波段 10 的大气顶部亮度温度进行比较。两个子区域的 RMSE(均方根误差)分别为 0.50 和 0.61 K,表明所提出的方法可以获取高精度的 MLST。
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来源期刊
Science China Earth Sciences
Science China Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
9.60
自引率
5.30%
发文量
135
审稿时长
3-8 weeks
期刊介绍: Science China Earth Sciences, an academic journal cosponsored by the Chinese Academy of Sciences and the National Natural Science Foundation of China, and published by Science China Press, is committed to publishing high-quality, original results in both basic and applied research.
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