Evaluation of the China Ocean Reanalysis (CORA) in the South China Sea -- Journal of Oceanology and Limnology,2020,38(6):1640-1653

	Cite this paper:
	FAN Maoting, WANG Huizan, ZHANG Weimin, HAN Guijun, WANG Pinqiang. Evaluation of the China Ocean Reanalysis (CORA) in the South China Sea[J]. Journal of Oceanology and Limnology, 2020, 38(6): 1640-1653

Evaluation of the China Ocean Reanalysis (CORA) in the South China Sea

FAN Maoting¹, WANG Huizan¹, ZHANG Weimin^1,2, HAN Guijun³, WANG Pinqiang¹

1 College of Meteorology and Oceanography, National University of Defense Technology, Changsha 410073, China;
2 Key Laboratory of Software Engineering for Complex Systems, National University of Defense Technology, Changsha 410073, China;
3 School of Marine Science and Technology, Tianjin University, Tianjin 300072, China

Abstract:

The daily regional reanalysis product of the China Ocean Reanalysis (CORA) product was released in website in 2018. Using in situ observational data including Argo profiling floats, drifters, and cruise data, the performance of CORA in the South China Sea in terms of temperature, salinity, current and mixed layer depths is evaluated based on timescale (seasonal and interannual) and spatial distribution characteristics. The CORA temperature, salinity, and mixed layer depth show certain seasonal and interannual variations. In 50-400 m depth in the SCS, the CORA temperature is colder in winter and warmer in summer and autumn. In 0-150 m in the SCS, the CORA salinity is higher in most time of the year. However, in the second half of the year, the salinity is slightly weaker in 100-150 m depth. In most years, the CORA mixed layer depths tend to be shallower, and in season, shallower in winter and deeper in summer. In spatial distribution, the closer the area is to the coast, the greater the CORA errors would be. The CORA temperature is colder in the western side and warmer in the eastern side, resulting in a weaker SCS western boundary current (SCSwbc). In most areas, the CORA mixed layer depths are shallower. In the area close to the coast, the CORA mixed layer depths change rapidly, and the deviations in the mixed layer depths are larger. In the central SCS, the CORA mixed layer depths change slowly, and the deviations in the mixed layer depths are also small.

Key words: China Ocean Reanalysis (CORA)|South China Sea (SCS)|drifter, Argo|cruise data|evaluation

Received: 2019-06-06 Revised: 2019-08-09

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