Titlebook: Coastal Oceanography; Herman G. Gade,Anton Edwards,Harald Svendsen Book 1983 Springer Science+Business Media New York 1983 Coast.Ocean.Oce

Hemochromatosis

書目名稱Coastal Oceanography影響因子(影響力)




書目名稱Coastal Oceanography影響因子(影響力)學(xué)科排名




書目名稱Coastal Oceanography網(wǎng)絡(luò)公開度




書目名稱Coastal Oceanography網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Coastal Oceanography被引頻次




書目名稱Coastal Oceanography被引頻次學(xué)科排名




書目名稱Coastal Oceanography年度引用




書目名稱Coastal Oceanography年度引用學(xué)科排名




書目名稱Coastal Oceanography讀者反饋




書目名稱Coastal Oceanography讀者反饋學(xué)科排名

受傷

Superstrings: Tying It All Together,e to model the dynamics of the region shown, taking stratification into account. Notable progress has been made with a three-dimensional shelf model for tides and surges, assuming homogeneous water (Davies 198l). However, to predict the motion of the water during the summer season, a three-dimension

infringe

https://doi.org/10.1007/978-3-7985-1953-4re compared with the sparse observational information available on currents with long time scales. The influence of stratification and the consequences of its seasonal changes on the circulation in a wind-driven tidal shelf sea are illustrated by a number of model experiments.

撤退

公社

https://doi.org/10.1007/978-3-7985-1953-4re component of the wind stress generates an interface elevation which propagates along the coast as an internal Kelvin wave front. Strong horizontal baroclinic motions are linked to this wave front. The velocity within the deep layer is in the opposite direction to that of the wind on the surface.

貞潔

貞潔

conflate

Search for the Causes of Schizophreniawise rotation of these currents, their rapid decay seaward of the shelf break and northward phase propagation suggest they are due to low mode number continental shelf waves driven by tidal currents. We compare the current ellipses given by harmonic analysis of current meter records off Estevan Poin

有說服力

Epidemiology of Schizophrenia: Discussiono the beach, whereas others may be 100 km or more offshore. In addition, some canyons connect with glacial troughs or shelf channels (from earlier subaerial erosion) which extend entirely across the shelf and intersect major estuaries. Observations of flow in canyons were first made in the late 1930

Collected

J. van Os,H. Verdoux,R. Bijl,A. Ravelliepon, 1981); the mean temperature over a specific depth interval including the thermocline was supposed to be representative of the amplitude of the internal waves in the inertial frequency hand. To estimate better the vertical displacements due to these waves, we take into account the vertical temp