Publications

Cao, C; Li, JS; Jia, XD; Wang, SL; Wan, B (2024). Spatial and temporal variation of water clarity in typical reservoirs in the Beijing-Tianjin-Hebei region observed by GF1-WFV satellite data. JOURNAL OF OCEANOLOGY AND LIMNOLOGY.

Abstract
Rapidly monitoring regional water quality and the changing trend is of great practical and scientific significance, especially for the Beijing-Tianjin-Hebei (BTH) region of China where water resources are relatively scarce and inland water bodies are generally small. The remote sensing data of the GF1 satellite launched in 2013 have characteristics of high spatial and temporal resolution, which can be used for the dynamic monitoring of the water environment in small lakes and reservoirs. However, the water quality remote sensing monitoring model based on the GF1 satellite data for lakes and reservoirs in BTH is still lacking because of the considerable differences in the optical characteristics of the lakes and reservoirs. In this paper, the typical reservoirs in BTH-Guanting Reservoir, Yuqiao Reservoir, Panjiakou Reservoir, and Daheiting Reservoir are taken as the study areas. In the atmospheric correction of GF1-WFV, the relative radiation normalized atmospheric correction was adopted after comparing with other methods, such as 6S and FLAASH. In the water clarity retrieval, a water color hue angle based model was proposed and outperformed other available published models, with the R2 of 0.74 and MRE of 31.7%. The clarity products of the four typical reservoirs in the BTH region in 2013-2019 were produced using the GF1-WFV data. Based on the products, temporal and spatial changes in clarity were analyzed, and the main influencing factors for each water body were discussed. It was found that the clarity of Guanting, Daheiting, and Panjiakou reservoirs showed an upward trend during this period, while that of Yuqiao Reservoir showed a downward trend. In the influencing factors, the water level of the water bodies can be an important factor related to the water clarity changes in this region.

DOI:
10.1007/s00343-024-3114-0

ISSN:
2523-3521