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Analysis of the CODE observations suggests free types of events, two primarily synoptic-scale conditions which lead to stronger-than-normal upwelling-favorable winds over the shelf and three primarily mesoscale events which lead to wind relaxation. About half of the wind relaxation events observed in 1981 and 1982 are believed to be associated with either coastal-trapped gravity currents or internal Kelvin waves that About this PDF file: This new digital representation of the original work has been recomposed from XML files created from the original paper book, not from the original typesetting files.

Page breaks are true to the original; line lengths, word breaks, heading styles, and other typesetting-specific formatting, however, cannot be retained, and some typographic errors may have been accidentally inserted. Please use the print version of this publication as the authoritative version for attribution. STATE-OF-THE-ART OVERVIEW: PHYSICAL OCEANOGRAPHIC PROCESSES, FEATURES, AND METHODS OF POTENTIAL IMPORTANCE TO THE ESP 30 About this PDF file: This new digital representation of the original work has been recomposed from XML files created from the original paper book, not from the original typesetting files.

Data generated during the field studies are also sent to NOAA's National Oceanographic Data Center (NODC) for archiving. The deliverables of the modeling studies generally include a final report, a user's manual for the model, and some form of model predictions. For modeling studies on the east, west, and gulf coasts, the principal data deliverables have been predictions of the mean climatological flows over various time scales at spatial resolutions of typically 15 to 30 km. These have been the Figure 4 Offshore minerals management organizational chart.

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Assessment of the U.S. Outer Continental Shelf Environmental Studies Program : Physical Oceanography by Commission on Life Sciences Staff


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