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The Response of Wave Directions to Changing Wind Directions
Wave Directions Wind Directions
2009/1/7
From the premise that the net growth of wave energy induced by wind is centered around the wind direction, a relaxation model for the response of the main wave direction to changes in the wind directi...
Large-Scale, Low-Frequency Response on the Continental Shelf Due to Localized Atmospheric Forcing Systems
Large-Scale Continental Shelf Low-Frequency Response Localized Atmospheric Forcing Systems
2009/1/6
The first-order wave equation model of Gill and Schumann, which describes the flow induced on the continental shelf by the longshore wind stress, evaluated at the coast, is extended in three ways. Fir...
The Response of Wind-Wave Spectra to Changing Winds. Part I：Increasing Winds
Wind-Wave Spectra Changing Winds Increasing Winds
2009/1/6
Continuous time series of wind profiles and wind waves under growing conditions, recorded at Shirahama Oceanographic Tower Station and discussed by Kawai, Okada and Toba, have been reanalysed for this...
The Response of Stratified Shelf and Slope Waters to Steady Offshore Forcing
Stratified Shelf Slope Waters Offshore Forcing
2009/1/5
The effect of steady, deep-ocean forcing on the flow over a continental slope and shelf region is examined using a linear and time-independent numerical model which includes continuous stratification,...
Interhemispheric Asymmetry in the Transient Response of a Coupled Ocean–Atmosphere Model to a CO2 Forcing
Transient Response CO2 Forcing Coupled Ocean–Atmosphere Model
2009/1/5
Numerical experiments are carried out using a general circulation model of a coupled ocean-atmosphere system with idealized geography, exploring the transient response of climate to a rapid increase o...
Frictionally Modified Continental Shelf Waves and the Subinertial Response to Wind and Deep-0cean Forcing
Continental Shelf Waves Subinertial Response Deep-0cean Forcing
2009/1/4
Analytic solutions am obtained for the barotropic shelf circulation caused by wind and deep-ocean forcing at subinertial frequencies. An Inclined beach model of the continental shelf is used and only ...
The Response of a Linear Model of the Tropical Pacific to Surface Winds from the NCAR General Circulation Model
global circulation model sea surface temperatures Linear Model Surface Winds
2009/1/4
An experiment in which surface wind stress data from the National Center for Atmospheric Research global circulation model (GCM) was used to drive a simple model of the tropical Pacific is described. ...
The Wind-Driven Shelf and Slope Water Flow in Terms of a Local and a Remote Response
Wind-Driven Shelf Slope Water Flow Remote Response
2009/1/4
Clarke and Van Gorder suggest that many coastally trapped wave modes are needed to describe the wind-driven shelf and slope water alongshore velocity field. Calculations with an harmonic wind forcing ...
Vertical Structure of the Ocean Current Response to a Hurricane
Airborne eXpendable Current Profilers Garrett-Munk spectra
2008/12/30
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 Pro...
Subinertial Frequency Response of Wind-Driven Currents in the Mixed layer Measured by Drifting Buoys in the Midlatitude North Pacific
Fleet Numerical Ocean Center Frequency Response Wind-Driven Currents Mixed layer
2008/12/30
Previous analyses of satellite-tracked drifting buoy data (30 m drogue depth) and Fleet Numerical Ocean Center (FNOC) surface wind stress in the midlatitude North Pacific during autumn/winter have sho...
A data-adaptive technique, the iterative maximum likelihood method, is used to estimate directional wave spectra from data collected by three pitch-and-roll buoys, during two turning wind events of th...
Wind-Driven Response of Ocean Surface Infrared Signals
Wind-Driven Ocean Surface Infrared Signals
2008/12/30
In the course of archiving positions of the edge of the Loop Current from satellite infrared (IR) data, we have found a substantial amount of energy at periods in the “wind-driven band.” Using a techn...
Free Surface Effects on the Near-Inertial Ocean Current Response to a Hurricane
Free Surface Effects Hurricane Near-Inertial Ocean Current
2008/12/27
During the passage of hurricane Frederic in 1979, four ocean current meter arrays in water depths of 100–950 m detected both a baroclinic and a depth-independent response in the near-inertial frequenc...
Transient Response of a Global Ocean-Atmosphere Model to a Doubling of Atmospheric Carbon Dioxide
Transient Response Atmospheric Carbon Dioxide Global Ocean-Atmosphere Model
2008/12/27
The transient response of climate to an instantaneous increase in the atmospheric concentration of carbon dioxide has been investigated by a general circulation model of the coupled ocean-atmosphere-l...
A Three-Dimensional Barotropic Model of the Response of the Australian North West Shelf to Tropical Cyclones
Barotropic Model Tropical Cyclones Australian North West Shelf
2008/12/27
A three-dimensional barotropic model using a -coordinate or depth transformation, and forced with tropical cyclone wind and atmospheric pressure fields has been applied to the continental shelf and sl...