基于Landsat-8影像的高原湖泊水体表面温度反演

doi:10.3969/j.issn.0255-8297.2024.06.007

摘要/Abstract

摘要： 目前，在高原环境下的水体表面温度反演成果相对较少，本文结合Landsat-8影像和辐射传输方程法对纳木错湖水体表面温度进行反演并验证其有效性。首先，计算研究区的地表比辐射率；其次，计算同温度下黑体的辐射亮度；最后，利用普朗克函数计算水体表面温度并基于MODIS地表温度产品对反演结果进行验证。实验结果表明，湖泊水体表面温度反演绝对误差最小值为0.449 ℃、最大值为1.685 ℃，均方根误差最小值为1.269 ℃、最大值为1.781 ℃，反演结果与MODIS温度产品的日均温结果较接近，夏季湖泊水体表面温度变化特征基本与纳木错气温一致。该方法可为后续高原湖泊水体水表温度反演研究提供一定的参考。

关键词: 高原湿地, 湖泊表面温度反演, 辐射传输方程法, 纳木错湖, Landsat-8

Abstract: At present, there are few studies on water surface temperature retrieval in the plateau environments. This paper combined Landsat-8 image and radiative transfer equation method to invert the water surface temperature in Namco Lake and verify its effectiveness. First, the surface-specific emissivity of the study area is calculated. Second, the radiation brightness of the blackbody at the same temperature is determined. Finally, the Planck function is used to calculate the water surface temperature and MODIS surface temperature products is used to validate the inversion results. Experimental results show that the minimum absolute error of lake surface temperature retrieval is 0.449 ℃, with a maximum error of 1.685 ℃. The minimum root mean square error ranges from 1.269 ℃ to 1.781 ℃. The inversion results are close to the average daily temperature results from MODIS products. The variation characteristics of lake surface temperature in summer are basically consistent with the temperature of Namco Lake. This method provides a reference for future research on water surface temperature retrieval in plateau lakes.

Key words: plateau wetlands, retrieval of lake surface temperature, radiative transfer equation method, Namco Lake, Landsat-8

中图分类号:

TP79

杭媛芳, 张鹏林. 基于Landsat-8影像的高原湖泊水体表面温度反演[J]. 应用科学学报, 2024, 42(6): 977-987.

HANG Yuanfang, ZHANG Penglin. Retrieval of Lake Surface Temperature in Plateau Based on Landsat-8 Images[J]. Journal of Applied Sciences, 2024, 42(6): 977-987.

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