Vertical Structure of the Ocean Current Response to a Hurricane
Open Access
- 1 May 1989
- journal article
- research article
- Published by American Meteorological Society in Journal of Physical Oceanography
- Vol. 19 (5) , 649-669
- https://doi.org/10.1175/1520-0485(1989)019<0649:vsotoc>2.0.co;2
Abstract
During the passage of hurricane Norbert in 1984, the Hurricane Research Division of NOAA conducted a Planetary Boundary Layer Experiment that included the deployment of Airborne eXpendable Current Profilers (AXCP). A total of. 16 AXCPs provided for the fist time high-resolution vertical profiles of currents and temperatures in hurricane wind conditions. This study focuses on the vertical structure of the near-inertial baroclinic current excited by the passage of this hurricane. The transient hurricane-induced currents are isolated from the AXCP profiles in Norbert by subtracting a spatially-averaged current. Near the center of hurricane Norbert, the WKBJ-scaled vertical wavenumber spectra are a decade greater than the Garrett-Munk spectra (GM75). The fist ten linear, baroclinic free modes are calculated from the spatially-averaged Brunt–Väisälä frequency. To allow a more direct comparison with the AXCP observations in the current wind regime, the near-inertial response for the three dimensional v... Abstract During the passage of hurricane Norbert in 1984, the Hurricane Research Division of NOAA conducted a Planetary Boundary Layer Experiment that included the deployment of Airborne eXpendable Current Profilers (AXCP). A total of. 16 AXCPs provided for the fist time high-resolution vertical profiles of currents and temperatures in hurricane wind conditions. This study focuses on the vertical structure of the near-inertial baroclinic current excited by the passage of this hurricane. The transient hurricane-induced currents are isolated from the AXCP profiles in Norbert by subtracting a spatially-averaged current. Near the center of hurricane Norbert, the WKBJ-scaled vertical wavenumber spectra are a decade greater than the Garrett-Munk spectra (GM75). The fist ten linear, baroclinic free modes are calculated from the spatially-averaged Brunt–Väisälä frequency. To allow a more direct comparison with the AXCP observations in the current wind regime, the near-inertial response for the three dimensional v...This publication has 4 references indexed in Scilit:
- The decay of wind‐forced mixed layer inertial oscillations due to the β effectJournal of Geophysical Research: Oceans, 1989
- Near-Inertial Ocean Current Response to Hurricane FredericJournal of Physical Oceanography, 1987
- Observations of Hurricane-Generated, Near-Inertial Slope ModesJournal of Physical Oceanography, 1986
- Inertial Oscillations due to a Moving FrontJournal of Physical Oceanography, 1985