Titlebook: Oceanic and Anthropogenic Controls of Life in the Pacific Ocean; Proceedings of the 2 V. I. Ilyichev,V. V. Anikiev Conference proceedings 1

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書目名稱Oceanic and Anthropogenic Controls of Life in the Pacific Ocean影響因子(影響力)




書目名稱Oceanic and Anthropogenic Controls of Life in the Pacific Ocean影響因子(影響力)學(xué)科排名




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書目名稱Oceanic and Anthropogenic Controls of Life in the Pacific Ocean網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Oceanic and Anthropogenic Controls of Life in the Pacific Ocean被引頻次




書目名稱Oceanic and Anthropogenic Controls of Life in the Pacific Ocean被引頻次學(xué)科排名




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書目名稱Oceanic and Anthropogenic Controls of Life in the Pacific Ocean年度引用學(xué)科排名




書目名稱Oceanic and Anthropogenic Controls of Life in the Pacific Ocean讀者反饋




書目名稱Oceanic and Anthropogenic Controls of Life in the Pacific Ocean讀者反饋學(xué)科排名

Canvas

危機(jī)

Diaphragm

Mineral Aerosol over and Deposition to the Pacific Ocean the oceans. These particles have relatively short residence times in both atmosphere and hydrosphere, and therefore their concentrations are sensitive to changes in weather, climate, perturbations by human’s activities, etc. In addition, many trace metals are associated with aluminosilicates (miner

Alpha-Cells

Radiation

Some Results of Study of Currents on the Southern Shelf of Vietnamry is contiguous with the coastal zone of Central Vietnam. The dominant climatic factor of the region as well as the whole of S China Sea is the monsoon: the NE monsoon blows from December to March (in winter) and the SW monsoon blows from June to September (in summer). Numerical calculations of the

Lobotomy

On Vertical Mixing in Shelf and Frontal Zones of the Oceanients of all kinds, complicated vertical structure of hydrophysical properties, great importance of internal waves, turbulence, 3-D circulation and vertical mixing. Being interrelated, all these phenomena must be studied in complex.

Basal-Ganglia

A Numerical Model of the Formation of Cold Front and Its Derived Circulation on the Shelf paper to simulate and describe the physical process of the formation of cold front and its derived circulation, in which only surface heating, thermally driving and tidal mixing are taken into account. As a result, calculated sectional distribution of water temperature, horizontal and vertical circ

鼓掌

Hydrological fronts of the Northeast Pacific Ocean in Autumn Seasontructure and isolation, classification and determination of front positions was carried out. The main types of water structure in the regions are subarctic and subtropical ones separated by the subtropic front which belongs to the area near 40°N. Zoning of the water area according to 6 types of wate

Friction