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

concise

The Influence of Weather and Climateiven by weather events, while the basic features and the long-term variability of the North Sea as, for instance, mean salinity distribution, mean currents, yearly nutrient input by river discharge, distribution of fish species and their year-to-year variation, are mainly due to climate, i.e. the st

GLUT

Seasonal Correlation Between Nutrients and Contaminantsnity of the numerous contaminants to the different phases - dissolved, coloids, particles and organisms of different quality, sediment and aerosols - is variable due to environmental conditions (pH, oxygen) and will change when the contaminants are modified by chemical reactions (speciation, convers

遺傳

乞討

constitutional

Combined Effects of Abiotic and Biotic Factors on Heavy Metal Fluxes88, 1990, 1991). It is readily obvious, however, that no evaluation of metal concentration distributions in different ecosystem compartments of the North Sea is possible without an at least rough knowledge of the biogeochemical behaviour and fate of these elements. During its passage and stay in a m

Herbivorous

On the Reliability of our North Sea Assessmentea. Indeed, before ZISCH no comparable data set existed. It is still necessary to explore the limits of this data in order to avoid overinterpretation, in particular as the ZISCH surveys had to be designed without reference to statistical considerations on sampling schemes (Cochran 1977).

CALL

Local Variability of Surface Currents Based on HF-Radar Measurementse measurement is the necessary first step in the development and testing of such a prediction model. In fact, when near-surface currents are known, it is theoretically possible to numerically calculate the currents and circulation all the way down to the ocean floor.

hedonic

voluble

indignant

Future Trends for Regulatory Management,e measurement is the necessary first step in the development and testing of such a prediction model. In fact, when near-surface currents are known, it is theoretically possible to numerically calculate the currents and circulation all the way down to the ocean floor.