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

Panther

Apoptosis

Marine Hydrologic Forecasts in Chinarine exploitation. At the present, the main task of hydrologic forecasts in China is undertaken by the National Marine Environmental Forecasting Center (NMEFC), with regional centers in Qingdao, Shanghai, Guangzhou and Haikou, and some coastal oceanographic stations under the State Oceanic Administr

Adrenaline

Marine Chemistrytrated to the sea-air, sea-sediments, sea-organisms, and sea- river interfaces exchange in the Bohai Sea, the Huanghai (Yellow) Sea, the East China Sea and the South China Sea. Many articles and books have been published.

calamity

Marine Chemistry in Northern Seas of Chinathe coastal waters of the East China Sea (ECS), the Huanghai Sea (HS) and the Bohai Sea (BS). Two current systems, a less saline current toward the east and the south on the coastal side and a warm and saline Kuroshiro toward the north and the west on the other side, control the main feature of mari

粗鲁性质

Geochemistry of Major Chinese River-Estuary Systemsd seawrads sediment load. Consequently the adjacent continental shelf is one of the most active land-sea interaction regions in the world. The geochemistry of some large Chinese estuaries have been studied in last decade especially within the framework of international cooperative programs.

租约

Patterns and Structures of the Currents in Bohai, Huanghai and East China Seasoshio-Tsushima Warm Current - HS Warm Current and its extension on the east side and the China Coastal Current including the southern BS Coastal Current, HS Coastal Current, and ECS Coastal Current) on the west side. Along the western coast of Korea, the West Korea Coastal Current flows southward.

cognizant

厚颜

ears ago I was invited by Professor John Steele, Director of the Woods Hole Oceanographic Institute of the U. S. A. to write a preface for the special issue on "Oceanography in China" for the Oceanus. I was then the Director of the Institute of Oceanology, Academia Sinica. I gladly appreciated the h

音的强弱

Invertebrate

Marine Chemistry in Northern Seas of Chinast and the south on the coastal side and a warm and saline Kuroshiro toward the north and the west on the other side, control the main feature of marine chemistry in these seas. The influence of biological factors on the distribution of chemical components in these waters is only regional.