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Thursday, August 26, 2021 | History

4 edition of Desoto Canyon eddy intrusion study found in the catalog.

Desoto Canyon eddy intrusion study

Desoto Canyon eddy intrusion study

annual report: year 2

by

  • 100 Want to read
  • 27 Currently reading

Published by U.S. Dept. of Interior, Minerals Management Service, Gulf of Mexico OCS Region in New Orleans .
Written in English

    Subjects:
  • Oceanography -- Mexico, Gulf of,
  • Eddies,
  • Ocean circulation -- Mexico, Gulf of

  • Edition Notes

    Other titlesEddy intrusion study
    StatementScience Applications International Corporation
    SeriesOCS study
    ContributionsUnited States. Minerals Management Service. Gulf of Mexico OCS Region
    The Physical Object
    FormatMicroform
    Paginationiv, 8 leaves
    ID Numbers
    Open LibraryOL14496579M
    OCLC/WorldCa44689135

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Desoto Canyon eddy intrusion study Download PDF EPUB FB2

Desoto Canyon eddy intrusion study by Science Applications International Corporation,U. Dept. of the Interior, Minerals Management Service, Gulf of Mexico OCS Region edition, Microform in.

DeSoto Canyon Eddy Intrusion Study sponsored by the Minerals Management Service (SAIC ). A total of 13 current meter moorings were deployed in the DSC. The moorings were located at m (A1, B1, C1, D1, and E1), m (D9), m (A2, B2, C2, and D2), and m (A3, B3, and C3).

The mooring locations are marked in Fig.   For clarity, the intrusion in this study refers to the flow across the m isobath at the head of DeSoto Canyon in the model. Under the forcing of Desoto Canyon eddy intrusion study book open boundary conditions the model generates a Loop Current in the Gulf of Mexico that sheds anticyclonic eddies of km radius at a period of around 13 by:   The shelf also narrows appreciably between Cape San Blas and DeSoto Canyon.

The addition of wind-driven upwelling over the narrower portions of the shelf can further facilitate upwelling onto the shelf. Note that for the period 38 June, at the beginning of this LC intrusion event, the winds were upwelling by: Eastward wind-driven currents promote large freshwater transport toward the shelf break and the DeSoto Canyon, where eddies with diameters ranging from 50 to km interact with the buoyant plume.

This study evaluates a data-assimilated model simulation of near-surface circulation in DeSoto Canyon (DSC), Gulf of Mexico, with emphasis on analyzing moored current-meter observations and. A major reason for this is a huge underwater canyon called DeSoto Canyon that lies just 60 miles offshore.

It cuts through the Gulfs soft, sloping continental shelf, creating an underwater canyon over 3, feet deep. The canyon acts a chute that sends cold, nutrient-rich ocean water up toward the surface to support lots of marine life, like. Palo Duro Canyon State Park remains one of my favorite year round destinations to hike, camp, picnic or just for a scenic drive.

This book is an instructive tool to appreciate the full composition and varied history of this canyon complex. Having this text completes the s:   In the Gulf of Mexico, programs include the Louisiana Texas (LATEX) Circulation Study, the DeSoto Canyon Eddy Intrusion Study, deepwater studies in the northwest, central and eastern slope regions, a major field study of the Loop Current, and a Gulf-wide deep circulation study using Lagrangian (RAFOS) floats.

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[1] The western boundary current in the North Atlantic is characterized by an intense flow (reaching ms 1, at Desoto Canyon eddy intrusion study book surface) that enters the Caribbean Sea through the Lesser Antilles passages, crosses the entire Caribbean and enters the Gulf of Mexico through the Yucatan Channel, where it is known as the Loop Current.

A characteristic feature of the Loop Current is eddy-shedding events (i. De Soto canyon is a curious S-shaped submarine canyon approximately km south-southwest of Pensacola, Florida.

Seismic reflection profiling shows that an east-west partially buried shoreline, the influence of at least five salt domes, and erosional and depositional structures are responsible for the peculiar shape of the canyon. The northern bank of the east-west part of De Soto canyon is.

This study analyzes the eddy field in the Northwestern Iberian region with a particular focus on the eddies arising from the destabilization of the IPC. It is the first time that an analysis of the Swoddies is done in a year high resolution ocean simulation.

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