Preprints
https://doi.org/10.5194/egusphere-2026-5436
https://doi.org/10.5194/egusphere-2026-5436
25 Sep 2026
 | 25 Sep 2026
Status: this preprint is open for discussion and under review for Ocean Science (OS).

Improving Reconstructed HY-1D/COCTS SST for Upwelling Events in the Gulf of Lion through Wind-Informed Cloud Detection

Zhuomin Li, Aida Alvera-Azcárate, Alexander Barth, Nathaniel Bensoussan, Lei Guan, and Na Xu

Abstract. Sea surface temperature (SST) is essential for understanding ocean dynamics and air-sea interactions. SST from the Haiyang-1D (HY-1D) Chinese Ocean Color and Temperature Scanner (COCTS) has been obtained based on the algorithm derived using an atmospheric radiative transfer model. In the Gulf of Lion of the Mediterranean Sea, northwest winds prevail in summer and autumn, which favors upwelling events. This study aims to improve reconstructed HY-1D/COCTS SST for characterizing strong upwelling events in the Gulf of Lion. The study covers the period from May to November 2021(summer and autumn). The research area is 41°N–44°N and 3°E–8°E and the spatial resolution of COCTS SST is 1 km. Owing to persistent cloud cover, 61.92% of all pixels are missing. First, to better utilize COCTS SST, we apply Data Interpolating Empirical Orthogonal Functions (DINEOF) to reconstruct COCTS SST. The validation results for reconstructed COCTS SST show that DINEOF provides accurate statistical results on cloud pixels. We analyze the performance of the reconstructed COCTS SST in 8 sporadic upwelling events using the in situ data as reference. The hourly in situ data from 3 sites located in/nearby distinct upwelling areas from the Gulf of Lion (Marseille-Toulon area). The results show that the reconstructed COCTS SST characterizes most SST cooling events caused by upwelling, but not as intense as the in situ SST. Second, to overcome this limitation, we propose a wind-informed cloud detection procedure that takes into account wind speed and direction in order to improve the classification of upwelling-influenced pixels. The COCTS SST obtained by this improved cloud mask is subsequently reconstructed using DINEOF.  The improved reconstructed COCTS SST has higher consistency with the in situ SST in the upwelling area. The results show the difficulty of cloud masking in areas with strong upwelling events and that the improved reconstructed HY-1D/COCTS SST, enabled by wind-informed cloud detection, have the potential to accurately describe such events.

Competing interests: At least one of the (co-)authors is a member of the editorial board of Ocean Science.

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Zhuomin Li, Aida Alvera-Azcárate, Alexander Barth, Nathaniel Bensoussan, Lei Guan, and Na Xu

Status: open (until 20 Nov 2026)

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Zhuomin Li, Aida Alvera-Azcárate, Alexander Barth, Nathaniel Bensoussan, Lei Guan, and Na Xu
Zhuomin Li, Aida Alvera-Azcárate, Alexander Barth, Nathaniel Bensoussan, Lei Guan, and Na Xu
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Latest update: 25 Sep 2026
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Short summary
In the Gulf of Lion, summer–autumn northwest winds drive coastal upwelling cooling often masked in satellite/reanalysis SST by clouds and strict quality control. We reconstruct HY-1D COCTS SST and validate against three coastal stations. It captures most events but underestimates cooling. We add wind-informed cloud detection using wind speed/direction to recover cold upwelling pixels mislabeled as cloud. Results match in situ SST better, improving SST availability for upwelling studies.
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