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Hurricane wave height and forces--2: Deepwater storm waves dissipate across continental shelf

Journal Article · · Oil Gas J.; (United States)
OSTI ID:7039448
In the first article of this series, we addressed the background and formulation of existing API design criteria for shallow water platforms in the Gulf of Mexico. In this second article, attention is focused on the characterization of storm-generated, deepwater wave heights, and the physical processes which dissipate this energy over the continental shelf. The maximum wave height which can be reasonably expected to affect a structure during its lifetime is one of the most critical factors influencing the design of an offshore structure. The estimation of future maximum wave occurrences must reflect the past history of storm wave occurrences. Thus, long-term historical data bases are essential for estimating maximum wave height occurrences with meaningful reliability. Characterizations of historical storm conditions may be based on either measured or hindcast data. However, since relatively small amounts of measured wave data are available in the Gulf of Mexico, hindcasting techniques are necessary to extend the data base. A hindcast is the reconstruction of an historic event, or series of events, to yield certain meteorological and/or oceanographic data for the study area. Through reconstruction of these events, a series of data may be generated. A statistical analysis can be conducted with the hindcast data to provide estimates of future occurrences.
Research Organization:
PMB Systems Eng., Inc., San Francisco, CA
OSTI ID:
7039448
Journal Information:
Oil Gas J.; (United States), Journal Name: Oil Gas J.; (United States) Vol. 81:39; ISSN OIGJA
Country of Publication:
United States
Language:
English