Titlebook: Circulation and Contaminant Fluxes in the North Sea; Jürgen Sündermann Book 1994 Springer-Verlag Berlin Heidelberg 1994 Contaminat Transpo

osteomalacia

書(shū)目名稱(chēng)Circulation and Contaminant Fluxes in the North Sea影響因子(影響力)




書(shū)目名稱(chēng)Circulation and Contaminant Fluxes in the North Sea影響因子(影響力)學(xué)科排名




書(shū)目名稱(chēng)Circulation and Contaminant Fluxes in the North Sea網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱(chēng)Circulation and Contaminant Fluxes in the North Sea網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




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書(shū)目名稱(chēng)Circulation and Contaminant Fluxes in the North Sea被引頻次學(xué)科排名




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書(shū)目名稱(chēng)Circulation and Contaminant Fluxes in the North Sea讀者反饋




書(shū)目名稱(chēng)Circulation and Contaminant Fluxes in the North Sea讀者反饋學(xué)科排名

夾死提手勢(shì)

Seasonal and Interannual Variability in the Atmosphere and in the Seaorth Sea. Since this transport is also affected by atmospheric fields, wind and temperature fields were determined for a region encompassing the North Sea and the adjoining parts of the Atlantic for the years mentioned above. In order to evaluate the representativity of the cruise results it is nece

cogent

propose

Large-Scale Distribution of Contaminants in Spring 1986 and Winter 1986/87exchange between North Sea and Atlantic, large amounts of contaminants are held back by ad- and absorptive processes on the North Sea shelf. The contaminants may be transported in the waterway adsorbed onto suspended matter. When these reach sedimentation areas, the particles settle on the bottom an

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Atmospheric Transport of Contaminants, Their Ambient Concentration and Input into the North Seaonents. The few data for the open sea, however, have left large uncertainties in quantitative estimates (Cambray et al. 1975). Modelling indicated that there should be a steep decrease in deposition depending on meteorological conditions, and that coastal stations overpredict the input substantially

transdermal

transdermal

花爭(zhēng)吵

Mean and Local Transport in Aireter for modelling of tracer transports in the ocean (Chap. 3.2). The objective of this section is to resolve the atmospheric input of trace substances into the North Sea in space and time and to discuss local features.

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Evaluation of the North Sea, Joining in Situ and Remotely Sensed Data with Model Resultsi synoptic observations. Isoline maps of any concentrations derived from cruises of several weeks’ length do not show an actual situation but a mixture of the spatial distribution as well as the temporal development, which cannot be separated from each other. The plotted distribution includes effect