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

Hemochromatosis

书目名称Coastal Oceanography影响因子(影响力)




书目名称Coastal Oceanography影响因子(影响力)学科排名




书目名称Coastal Oceanography网络公开度




书目名称Coastal Oceanography网络公开度学科排名




书目名称Coastal Oceanography被引频次




书目名称Coastal Oceanography被引频次学科排名




书目名称Coastal Oceanography年度引用




书目名称Coastal Oceanography年度引用学科排名




书目名称Coastal Oceanography读者反馈




书目名称Coastal Oceanography读者反馈学科排名

受伤

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.

贞洁

贞洁

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

有说服力

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