Estimating Cloudy-Sky Land Surface Temperature From FY-3D/MERSI-II Using the Surface Energy Balance Theory

This letter reports the first cloudy-sky land surface temperature (LST) retrieval from the MEdium Resolution Spectral Imager-II (MERSI-II) onboard Fengyun-3D (FY-3D). In this study, a new cloudy-sky LST retrieval algorithm was adapted for FY-3D/MERSI-II. The method consists of two key components: (1) estimating the hypothetical clear-sky LST using geographically weighted regression (GWR) downscaling and linear model correction, and (2) quantifying the temperature difference (ΔT) caused by cloud radiative effect (CRE) based on surface energy balance (SEB) theory. Validation against in situ LST measurements from the SURFRAD and HiWATER networks indicates that the retrieved cloud-sky LST exhibits a bias of 0.02 K and a root mean square error (RMSE) of 3.77 K. The results confirm that the algorithm achieves reliable retrieval of FY-3D/MERSI-II cloudy-sky LST, with the ΔT correction term making a notable contribution. This method is expected to be used to generate the operational FY-3D cloudy-sky LST product.

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Publication Details

Journal
IEEE Geoscience and Remote Sensing Letters
Published
2025-01-01
DOI
https://doi.org/10.1109/lgrs.2025.3569674
Citations
1
Primary Topic
Urban Heat Island Mitigation
Type
article
Field-Weighted Citation Impact
0.80

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article

Estimating Cloudy-Sky Land Surface Temperature From FY-3D/MERSI-II Using the Surface Energy Balance Theory

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1 citations
IEEE Geoscience and Remote Sensing Letters
Urban Heat Island Mitigation
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article

Estimating Cloudy-Sky Land Surface Temperature From FY-3D/MERSI-II Using the Surface Energy Balance Theory

Jie Cheng, Xiangchen Meng, Lixin Dong, Weihan Liu, Chenze Wu
article en
1 citations

Abstract

This letter reports the first cloudy-sky land surface temperature (LST) retrieval from the MEdium Resolution Spectral Imager-II (MERSI-II) onboard Fengyun-3D (FY-3D). In this study, a new cloudy-sky LST retrieval algorithm was adapted for FY-3D/MERSI-II. The method consists of two key components: (1) estimating the hypothetical clear-sky LST using geographically weighted regression (GWR) downscaling and linear model correction, and (2) quantifying the temperature difference (ΔT) caused by cloud radiative effect (CRE) based on surface energy balance (SEB) theory. Validation against in situ LST measurements from the SURFRAD and HiWATER networks indicates that the retrieved cloud-sky LST exhibits a bias of 0.02 K and a root mean square error (RMSE) of 3.77 K. The results confirm that the algorithm achieves reliable retrieval of FY-3D/MERSI-II cloudy-sky LST, with the ΔT correction term making a notable contribution. This method is expected to be used to generate the operational FY-3D cloudy-sky LST product.

IEEE Geoscience and Remote Sensing LettersVol. 22
China Meteorological Administration (CN), Qufu Normal University (CN), Beijing Normal University (CN), State Key Laboratory of Remote Sensing Science (CN)
National Natural Science Foundation of China
Affordable and clean energy
Openalex Percentile: Top 30%
Urban Heat Island Mitigation
0.80
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