Coastal Ocean Prediction by Christopher N. K. Mooers

By Christopher N. K. Mooers

About The Product

Published through the yank Geophysical Union as a part of the Coastal and Estuarine experiences Series.

Coastal Ocean Prediction is being released in the course of a interval whilst operational coastal ocean prediction structures are rising in Europe, Asia, Australia, and North the USA. a few of these platforms are associated with actions of the worldwide Ocean staring at process, backed by way of the Intergovernmental Oceanographic fee, global Meteorological association, United countries Environmental application, and the foreign Council of clinical Unions. the worldwide Ocean staring at approach is itself an emergent software of model?]based operational (i.e., continuous and governmentally sanctioned) tracking with coastal ocean, in addition to absolutely international, elements.


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Amer. Meteorol. , 31,303-304, 1950. E. Overland,Meteorology,p. W. T. S. , 1986. , On thetheoryof thekatabaticslopewind, Tellus,35A, 213-218, 1983. J. A. Bullock, The role of antecedentsurface vorticity development asa conditioningprocessin explosivecycloneintensification, Mon. , 1992. , 101, 4235-4254, 1996. E. Overland,Atmospheric structureandmomentum balanceduringa gapwind event in Shelikof Strait, Alaska, Mon. , 117, 1818-1833, 1989. S. West Coast:A review,Bull. M. Lackmann,and J. Gray, Offshore-directed winds in the vicinity of Prince William Sound, Alaska, Mon.

C. andC. N. Flagg,1976. The waterstructure, meancurrents,andshelf-water/slopewaterfront at the New Englandcontinentalshelf. R. Liege, 10, 209-225. Beckers,J. , 1991. J. Mar. Systems,1,315-332. Bleck, R. andD. B. Boudra,1986. or. ,91, 7611-7621. , C. Rooth,D. Hu andL. T. Smith,1992. Salinitydriventhermoclinetransients in a windandthermohalineforcedisopycnalcoordinate modelof the NorthAtlantic. or. , 22, 1486-1505. Blumberg, A. F. and G. L. Melior, 1980. Int. ,Hamburg,1978,editedby JSunderman andK.

This is becausethe offshore Gaspe Current exerts a major influence on the circulationand variability in the bay. At times when the currentintrudesinto the bay, suchas in the Figure, there is a generally cyclonic circulationin the bay. Sometimes,the current roundsthe northeastcomer of the bay without separating,leading to westwardflow along the entire north shore even near the mouth. On the other hand, there are times whenthe Currentseparatescleanlynearthe mouth,anddoesnot enterthe bay at all. The role of separation,togetherwith its mechanism,is discussedextensivelyin Gan et al.

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