EGU24-3329, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-3329
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Evaluation of MODIS LST products over the Tibetan Plateau and plain areas with in situ measurements

Yuting Qi1, Lei Zhong1,2,3, Yaoming Ma4,5, Yunfei Fu1, Zixin Wang1, and Peizhen Li1
Yuting Qi et al.
  • 1University of Science and Technology of China, (qiyuting@mail.ustc.edu.cn)
  • 2Jiangsu Collaborative Innovation Center for Climate Change, Nanjing, China, (zhonglei@ustc.edu.cn)
  • 3the CAS Center for Excellence in Comparative Planetology, Heifei, China, (zhonglei@ustc.edu.cn)
  • 4Institute of Tibetan Plateau Research, Chinese Academy of Sciences, (ymma@itpcas.ac.cn)
  • 5College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, (ymma@itpcas.ac.cn)

Land surface temperature (LST) is a crucial physical parameter for hydrological, meteorological, climatological, and climate change studies. To encourage the use of satellite-derived LST products in a wide range of applications, providing feedback on product performance over regional and global scales is an urgent task. However, considering that the uncertainty of newly released LST products is still unclear, it is urgently necessary to perform a comprehensive validation and error analysis, especially in areas with special geographical and weather conditions such as the Tibetan Plateau (TP). In particular, fewer studies have been concerned with the degraded LST retrieval accuracy over the TP because of the sparse ground measurements. In this study, MODIS LST products (C6) were comprehensively evaluated based on independent ground observation systems with different atmospheric and LST conditions. The in situ measurements collected from the TORP and SURFRAD systems are located on the North American Plain and the TP, respectively, incorporating various land cover types, including barren land, grassland, cropland, shrubland and sparse and dense vegetation, among others. Prior to the validation, LST products with different spatial resolutions were compared to ensure the spatial representativeness of ground-based measurements at satellite pixel scale. The evaluation results indicated that relatively high-quality in situ LST can be obtained during nighttime with relatively homogeneous spatial distribution. Compared with the North American Plain (with a mean RMSE of 1.56 K), MODIS LST retrieval has larger discrepancies (mean RMSE of 2.34 K) over the TP with complex terrain and variable weather. Various factors affecting LST retrieval accuracy were analyzed, which were categorized into 1) the simulated atmospheric and surface temperature condition settings, 2) the input data uncertainty, and 3) others. Among them, the emissivity determination is the primary source of the uncertainty in the generalized split-window algorithm, where the overestimated emissivity causes an underestimation of LST. It is expected to develop new LST retrieval algorithm to meet the quality specifications of users over the TP. Overall, this study identifies critical further research needs and improve the understanding of LST product performance under complex circumstance.

How to cite: Qi, Y., Zhong, L., Ma, Y., Fu, Y., Wang, Z., and Li, P.: Evaluation of MODIS LST products over the Tibetan Plateau and plain areas with in situ measurements, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-3329, https://doi.org/10.5194/egusphere-egu24-3329, 2024.