4.7 Article

Estimation of 30 m land surface temperatures over the entire Tibetan Plateau based on Landsat-7 ETM+ data and machine learning methods

Journal

INTERNATIONAL JOURNAL OF DIGITAL EARTH
Volume 15, Issue 1, Pages 1038-1055

Publisher

TAYLOR & FRANCIS LTD
DOI: 10.1080/17538947.2022.2088873

Keywords

Google Earth Engine; remote sensing; machine learning; land surface temperature; random forest

Funding

  1. Second Tibetan Plateau Scientifc Expedition and Research (STEP) Program [2019QZKK0103]
  2. Strategic Priority Research Program of Chinese Academy of Sciences [XDA20060101]
  3. National Natural Science Foundation of China [41875031, 41522501, 41275028, 91837208]
  4. Chinese Academy of Sciences [QYZDJSSW-DQC019]
  5. CLIMATE-TPE [32070]

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Land surface temperature (LST) retrieval over the Tibetan Plateau (TP) is improved using a random forest regression (RFR) model and an improved generalized single-channel (SC) algorithm. The LST results derived from these methods show smaller root mean square errors compared to other products.
Land surface temperature (LST) is an important parameter in land surface processes. Improving the accuracy of LST retrieval over the entire Tibetan Plateau (TP) using satellite images with high spatial resolution is an important and essential issue for studies of climate change on the TP. In this study, a random forest regression (RFR) model based on different land cover types and an improved generalized single-channel (SC) algorithm based on linear regression (LR) were proposed. Plateau-scale LST products with a 30 m spatial resolution from 2006 to 2017 were derived by 109,978 Landsat 7 Enhanced Thematic Mapper Plus images and the application of the Google Earth Engine. Validation between LST results obtained from different algorithms and in situ measurements from Tibetan observation and research platform showed that the root mean square errors of the LST results retrieved by the RFR and LR models were 1.890 and 2.767 K, respectively, which were smaller than that of the MODIS product (3.625 K) and the original SC method (5.836 K).

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