2002
DOI: 10.1360/02tb9081
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Intraseasonal variability of the subsurface temperature ob-served in the South China Sea (SCS)

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Cited by 11 publications
(5 citation statements)
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“…Prominent temperature variation in the SCS is restricted to the mixed layer [ Zhou and Gao , ], where salinity is also quite variable due to basin‐wide precipitation, river runoff from the surrounding landmasses, and advection of deeper water masses [ Wang and Li , ; Wang and Wang , ]. During the weaker and wetter southwest monsoon (May to September), surface water temperatures of the warm pool peak at >29°C.…”
Section: Upper Ocean Temperatures In the South China Seamentioning
confidence: 99%
See 1 more Smart Citation
“…Prominent temperature variation in the SCS is restricted to the mixed layer [ Zhou and Gao , ], where salinity is also quite variable due to basin‐wide precipitation, river runoff from the surrounding landmasses, and advection of deeper water masses [ Wang and Li , ; Wang and Wang , ]. During the weaker and wetter southwest monsoon (May to September), surface water temperatures of the warm pool peak at >29°C.…”
Section: Upper Ocean Temperatures In the South China Seamentioning
confidence: 99%
“…Prominent temperature variation in the SCS is restricted to the mixed layer [Zhou and Gao, 2003], where salinity is also quite variable due to basin-wide precipitation, river runoff from the surrounding landmasses, REGENBERG ET AL.…”
Section: Upper Ocean Temperatures In the South China Seamentioning
confidence: 99%
“…Shannon-Weiner index and Pielou index were high in summer and low in spring while Margalef index was high in summer and low in winter. According to the standards of Kuang Qijun [12], Zhou Guangjie [14] and Shu Jianmin [15], etc., the water quality of Shilianghe reservoir was determined as α-medium pollution type. Compared to Nvshahu lake [16], Honghu lake [17] and Jiantan reservoir [18], the Shannon-Wiener index, Margalef index and Pielou index of Shilianghe reservoir were all relatively lower.…”
Section: Discussmentioning
confidence: 99%
“…The SCS is controlled by the Southeast Asia monsoon system, and the basin-scale circulation in the upper ocean is regulated by the monsoon [Wyrtki, 1961]. Sea surface temperature (SST) and subsurface temperature in the SCS have intra-seasonal variations [Zhou and Gao, 2002], with amplitudes from 0.3°C to 0.5°C [Kawamura et al, 1988; Krishnamurti et al, 1988; Zhou et al, 1995]. The atmosphere has a memory shorter than the ocean.…”
Section: Introductionmentioning
confidence: 99%