Stalling of near‐inertial waves in a cyclone
Observations at the edge of the Loop Current after hurricane Katrina show inertial energy amplified at a depth of approximately 600∼700 m. Ray‐analysis using the eddy field obtained from a numerical simulation with data assimilation suggests that the amplification is due to inertial motions stalled...
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| Main Authors: | , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Wiley
2008-06-01
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| Series: | Geophysical Research Letters |
| Subjects: | |
| Online Access: | https://doi.org/10.1029/2008GL034273 |
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| _version_ | 1850271126988521472 |
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| author | L.‐Y. Oey M. Inoue R. Lai X.‐H. Lin S. E. Welsh L. J. Rouse Jr. |
| author_facet | L.‐Y. Oey M. Inoue R. Lai X.‐H. Lin S. E. Welsh L. J. Rouse Jr. |
| author_sort | L.‐Y. Oey |
| collection | DOAJ |
| description | Observations at the edge of the Loop Current after hurricane Katrina show inertial energy amplified at a depth of approximately 600∼700 m. Ray‐analysis using the eddy field obtained from a numerical simulation with data assimilation suggests that the amplification is due to inertial motions stalled in a deep cyclone. |
| format | Article |
| id | doaj-art-52ad0b8bb8dd4a7eb0008837beabcea1 |
| institution | OA Journals |
| issn | 0094-8276 1944-8007 |
| language | English |
| publishDate | 2008-06-01 |
| publisher | Wiley |
| record_format | Article |
| series | Geophysical Research Letters |
| spelling | doaj-art-52ad0b8bb8dd4a7eb0008837beabcea12025-08-20T01:52:19ZengWileyGeophysical Research Letters0094-82761944-80072008-06-013512n/an/a10.1029/2008GL034273Stalling of near‐inertial waves in a cycloneL.‐Y. Oey0M. Inoue1R. Lai2X.‐H. Lin3S. E. Welsh4L. J. Rouse Jr.5Program in Atmospheric and Oceanic Sciences Princeton University Princeton New Jersey USADepartment of Oceanography and Coastal Sciences Louisiana State University Baton Rouge Louisiana USAMinerals Management Service Herndon Virginia USAProgram in Atmospheric and Oceanic Sciences Princeton University Princeton New Jersey USACoastal Studies Institute Louisiana State University Baton Rouge Louisiana USADepartment of Oceanography and Coastal Sciences Louisiana State University Baton Rouge Louisiana USAObservations at the edge of the Loop Current after hurricane Katrina show inertial energy amplified at a depth of approximately 600∼700 m. Ray‐analysis using the eddy field obtained from a numerical simulation with data assimilation suggests that the amplification is due to inertial motions stalled in a deep cyclone.https://doi.org/10.1029/2008GL034273near‐inertial wavesloop currentcyclones |
| spellingShingle | L.‐Y. Oey M. Inoue R. Lai X.‐H. Lin S. E. Welsh L. J. Rouse Jr. Stalling of near‐inertial waves in a cyclone Geophysical Research Letters near‐inertial waves loop current cyclones |
| title | Stalling of near‐inertial waves in a cyclone |
| title_full | Stalling of near‐inertial waves in a cyclone |
| title_fullStr | Stalling of near‐inertial waves in a cyclone |
| title_full_unstemmed | Stalling of near‐inertial waves in a cyclone |
| title_short | Stalling of near‐inertial waves in a cyclone |
| title_sort | stalling of near inertial waves in a cyclone |
| topic | near‐inertial waves loop current cyclones |
| url | https://doi.org/10.1029/2008GL034273 |
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