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

Phonophobia

致詞

tinnitus

https://doi.org/10.1007/978-3-7985-1953-4Far from the coast, the wind stress curl, associated with the atmospheric front, produces strong interface elevations which increase with time and combine with coastal elevation to give peculiar behaviour of the interface associated with strong currents at the discontinuities.

Inferior

Cirrhosis

簡潔

無彈性

描述

spinal-stenosis

Wind-Forced Shelf Break Upwellingm currents on the shoreward side of the shelf break. Both coastal sea level and the shelf break circulation respond coherently to synoptic wind forcing but quantitative agreement with 2 layer shelf models is poor.

scrutiny

Shelf Waves of Diurnal Period Along Vancouver Islandlinic continental shelf wave described by the model of Brink (1982). Excellent agreement between observed currents and the sum of these two waves is obtained for each of four mooring periods for the last deployment period, when 95% of the variance was explained by these waves.