Titlebook: Oceanology of China Seas; Volume 1–2 Zhou Di,Liang Yuan-Bo,Zeng Cheng-Kui (C. K. Tseng) Book 1994 Springer Science+Business Media Dordrecht

喜悅

書目名稱Oceanology of China Seas影響因子(影響力)




書目名稱Oceanology of China Seas影響因子(影響力)學(xué)科排名




書目名稱Oceanology of China Seas網(wǎng)絡(luò)公開度




書目名稱Oceanology of China Seas網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Oceanology of China Seas被引頻次




書目名稱Oceanology of China Seas被引頻次學(xué)科排名




書目名稱Oceanology of China Seas年度引用




書目名稱Oceanology of China Seas年度引用學(xué)科排名




書目名稱Oceanology of China Seas讀者反饋




書目名稱Oceanology of China Seas讀者反饋學(xué)科排名

Hiatal-Hernia

拖網(wǎng)

978-94-010-4372-4Springer Science+Business Media Dordrecht 1994

RACE

Water Masses in China SeasThe water in the shallow parts of the Huanghai (Yellow) and East China seas is affected greatly by climatic and geographical conditions; it does not have the homogeneity and conservativeness of ocean water. Temperature and salinity data gained in 1978–1980 monthly sectional observations were used to study the water masses in these areas.

Choreography

同步左右

詼諧

Tides, Tidal Currents and Storm Surge Set-Up of South China SeaTidal oscillations in the South China Sea (SCS) are mainly co-oscillating tides spread from tidal waves of the Pacific Ocean. The independent tide generated by the rising force of the moon and the sun is much smaller, but is important to the deeper area of the SCS and has strong effect to semidiurnal constituents.

companion

Vulnerary

Kuroshio Intrusion and Taiwan Warm Current north (Fig. 1). It is connected with the South China Sea at the southwest through the Taiwan Strait and to the Japan Sea at the northeast through the Korea Strait. East and south of the Ryukyu Archipelago is the North Pacific Ocean.

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