Titlebook: North Sea Dynamics; Jürgen Sündermann,Walter Lenz Conference proceedings 1983 Springer-Verlag Berlin Heidelberg 1983 Atlantic Ocean.Coast.

閃爍

書目名稱North Sea Dynamics影響因子(影響力)




書目名稱North Sea Dynamics影響因子(影響力)學(xué)科排名




書目名稱North Sea Dynamics網(wǎng)絡(luò)公開度




書目名稱North Sea Dynamics網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱North Sea Dynamics被引頻次




書目名稱North Sea Dynamics被引頻次學(xué)科排名




書目名稱North Sea Dynamics年度引用




書目名稱North Sea Dynamics年度引用學(xué)科排名




書目名稱North Sea Dynamics讀者反饋




書目名稱North Sea Dynamics讀者反饋學(xué)科排名

impale

Conference proceedings 1983More than 150 participants from 10 coun- tries were present at the Symposium. Of the 58 lectures given, 45 are printed in this book. The manuscripts were reviewed by an international advisory board. The main goal of the organizers was to bring together as many active researchers as possible in this

預(yù)感

On Seasonal Circulation Patterns in the North Sea give only slight modifications and more details, but only vague quantifications. In contrast to this comparatively well established pattern, our knowledge of the circulation at depth is still rather poor.

DEAWL

Nonlinear Effects of Statistical Distribution of Deep Water Wavesransmission of energy between the elementary harmonics. The nonlinear hydrodynamic models have been confirmed in investigations (statistical and spectral analysis) carried out all over the world, especially in the last 10 years.

山頂可休息

Prognostic Storm Surge Simulation with a Combined Meteorological/Oceanographic Model0 m. Topography is included in a slightly smoothed way. Sea surface temperatures obtained from Deutscher Wetterdienst (DWD) are averaged over one week. The most important diabatic processes are included, namely fluxes of heat, moisture, and momentum at the surface, convective fluxes of heat and moisture and condensation of water vapour.

口音在加重

Sea Level Forecasts with an EOF Modeln the Skagerrak-Kattegat than it is in the Baltic. Also, the tidal variations can be disregarded in the Baltic, but are important on the west coast. It was therefore decided to develop separate models for the Swedish west coast; these have been in operational use since July 1981.

高度

Year-To-Year Changes in the Salinity of the Southern North Sea, 1948–1973: A Budget, and it is harder to obtain reliable data. Secondly, fluctuations in the quantity and salinity of water transported from the Atlantic have been invoked as a major source of variability of salinity in the North Sea, the fluctuations being the result of changing wind patterns over the North Atlantic (e.g., Dickson 1971).

木質(zhì)

Evacuate

Currents and Water Balance in the North Seaard. They were commented upon as “an attempt for which we should be grateful”, but they also received critical remarks, and the author himself did not consider them as the final answer (Schumacher 1923).

逃避責(zé)任