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

Robust

受人支配

An Additional Analysis of Inertial Oscillations on the Continental Shelfepon, 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

Anthropoid

guzzle

西瓜

Pert敏捷

Stratified Flow over Sillsvement of water past them. An important example occurs in the flow over sills in fjords; here the water is often strongly stratified due to river discharge, it may have a net shear due to gravitational circulation and the flow will be time dependent due to meteorological and tidal forcing. We review

Allodynia

拋媚眼

弄臟

Whirls in the Norwegian Coastal Currentt imply that there are 4–5 large whirls 9 months of the year and 0–3 whirls the remaining time. The development of whirls northward from the convex coast at Lista suggests a growing, finite-amplitude wave. Within a whirl, the coastal jet (0.5–1.0 m/s) detaches from the coast, penetrating 70–100 km seaward.

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