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Large-Scale Atmospheric Response to the 1964–65 Pacific Equatorial Warming
Large-Scale Atmospheric Response 1964–65 Pacific Equatorial Warming
2009/4/3
Time series of surface winds and sea surface temperatures at Canton Island, covering the period 1962–67, are interpreted to show that the major changes in the temperature of the large central and east...
The response of a simple Great Lake model to wind stress is studied theoretically. The model is of constant depth and of circular shape, continuously stratified with a thermocline region of linear den...
Transient Long-Wave Response for a Multiple-Island System
Transient Long-Wave Response Multiple-Island System
2009/4/2
An interpretation of the tsunami response at the Hawaiian island of Kauai has been carried out utilizing simple geometric representations which include the three-island system of Kauai, Niihau and Oah...
A Numerical Study of the Response of an Idealized Ocean to Large-Scale Surface Heat and Momentum Flux
Momentum Flux Idealized Ocean Large-Scale Surface Heat
2009/3/24
A numerical model of a 6-level, baroclinic ocean with a flat bottom and a regular coast line extending from 51.25S to 48.75N is integrated over 125 years of simulated time using a finite-difference an...
El Niño—The Dynamic Response of the Equatorial Pacific Ocean to Atmospheric Forcing
El Niñ o—The Dynamic Response Atmospheric Forcing Equatorial Pacific Ocean
2009/3/24
El Niño is the occasional appearance of warm water off the coast of Peru; its presence results in catastrophic consequences in the fishing industry. A new theory for the occurrence of El Ni&nti...
Eastern Tropical Ocean Response to Changing Wind Systems；with Application to El Niño
Eastern Tropical Ocean El Niñ o Changing Wind Systems
2009/3/7
El Niño is an anomalous condition that historically has been studied in the coastal region of the eastern tropical South Pacific. The phenomenon is commonly characterized there by the rapid app...
Oceanic Subarctic Fronts of the Central Pacific：Structure of and Response to Atmospheric Forcing
Central Pacific Oceanic Subarctic Fronts Atmospheric Forcing
2009/3/7
The oceanic fronts in the subarctic region of the central North Pacific are investigated and related to atmospheric forcing. The thermohaline structure indicates a near balance between horizontal temp...
Response of the Coastal Boundary Layer on the North Shore of Lake Ontario to a Fall Storm
Coastal Boundary Layer Fall Storm North Shore of Lake Ontario
2009/3/7
Water temperature measurements have been made from a ship steaming continuously around a 10 km square on the north shore of Lake Ontario during a vigorous upwelling and downwelling cycle generated by ...
The Time-Dependent Response of a Circular Basin of Variable Depth to a Wind Stress
Time-Dependent Variable Depth Circular Basin Wind Stress
2009/3/7
By solving an initial value problem, the time-dependent response of a large circular model lake to a steady wind stress has been investigated. Bottom stress has been neglected. The forced response has...
An infinitely deep stratified ocean on a equatorial beta plane is forced with a periodic wind system. The resulting linearized motion is shown to result in a deep cellular flow structure in rough agre...
Numerical Computation of Tsunami Response for Island Systems
Numerical Computation Tsunami Response Island Systems
2009/3/7
A numerical procedure has been developed to determine the tsunami response of an island system and the surrounding underwater topography. The main algorithm in based on the Eulerian equations of motio...
Sea Surface Temperature Response to Variations in Atmospheric Wind Forcing
Sea Surface Temperature Atmospheric Wind Forcing
2009/2/23
Sea surface temperature changes occurring during atmospheric forcing events defined in terms of wind speed are examined with the long time series of surface data at Ocean Weather Ships P, V and N in t...
A Hindcast of Barotropic Response over the Oregon-Washington Continental Shelf during the Summer of 1972
Barotropic Response Summer Oregon-Washington Continental Shelf
2009/2/23
Hindeasts of bottom currents on the southern Washington continental shelf are made on the basis of a long-wave approximation to the vorticity equation for a barotropic flow. Resistance of the shelf bo...
Numerical Simulations of the Ocean's Nonlinear, Baroclinic Response to Translating hurricanes
Numerical Simulations Ocean's Nonlinear Translating hurricanes
2009/2/23
An asymmetric nonlinear ocean model is employed to investigate the oceanic response to moving hurricanes. A turbulent kinetic energy budget is used to parameterize the stress-induced vertical mixing. ...
Oceanic Thermal Response to Strong Atmospheric Forcing II. The Role of One-Dimensional Processes
Oceanic Thermal Response Strong Atmospheric Forcing One-Dimensional Processes
2009/2/23
The oceanic response to individual atmospheric forcing events during September to December is studied using ocean weather ship observations supplemented by simulations with a bulk turbulent kinetic en...