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Equatorial Currents in the Pacific 1950 to 1970 and Their Relations to the Trade Winds
Equatorial Currents Pacific Trade Winds
2009/3/26
The mean meridional profile of dynamic topography across the zonal currents of the equatorial Pacific Ocean is disturbed by the observed deviation of monthly sea level at island stations from the long...
Rotary Cross-Bispectra and Energy Transfer Functions Between Non-Gaussian Vector Processes. II. Winds and Currents off the Oregon Coast
Rotary Cross-Bispectra Non-Gaussian Vector Processes Energy Transfer Functions
2009/3/7
Application of rotary cross-bispectra and energy transfer functions to a set of wind and current data measured from the Totem research buoy shows these elements to be non-Gaussian and that nonlinear i...
Measurements of the components of the heat balance of the upper 30 m of the ocean were made in the Bermuda area in August and September 1974. The quantities measured included surface downwelling and u...
Observed Surface Winds at Middleton Island, Gulf of Alaska and Their Influence on the Ocean Circulation
Observed Surface Winds Middleton Island Ocean Circulation
2009/2/16
Winds observed at an island in the Gulf of Alaska display a large annual signal with maximum easterlies in winter and weak easterlies in summer. For the northern Gulf of Alaska, the monthly mean Ekman...
Wind Stress and Heat Flux over the Ocean in Gale Force Winds
Wind Stress Gale Force Winds Heat Flux
2009/2/16
An offshore stable platform has been instrumented with wind turbulence, temperature and wave height sensors. Data from this platform have been analyzed by the eddy correlation method to obtain wind st...
Open Ocean Momentum Flux Measurements in Moderate to Strong Winds
Ocean Momentum Flux Measurements Strong Winds
2009/2/9
Measurements of the momentum flux were made by the Reynolds flux and dissipation methods on a deep water stable tower operated by the Bedford Institute of Oceanography, A modified Gill propeller-vane ...
The Response of Equatorial Oceans to a Relaxation of the Trade Winds
Equatorial Oceans Trade Winds
2009/2/9
The trade winds over the central Pacific are observed to weaken several months after the appearance of anomalously warm surface waters in the eastern equatorial Pacific Ocean. The following results ob...
The Relationship Between Deep Ocean Currents and Winds East of Barbados
Deep Ocean Currents Winds Barbados
2009/2/7
Observations of currents collected at the POLYMODE array III cluster C (16°N, 54°W) are compared with radiosonde winds measured at Barbados (13°N, 62°W) using a linear response analysis. The winds and...
Wintertime Winds and Coastal Sea-Level Fluctuations in the Northeast China Sea. Part I：Observations
Wintertime Winds Northeast China Sea Coastal Sea-Level Fluctuations
2009/2/6
Analyses of low-pass filtered coastal sea-level data and geostrophic winds derived from surface pressure charts for the period of 1 December 1980 through 31 March 1981 indicate that the wintertime dyn...
The Frictional Nearshore Response to Forcing by Synoptic Scale Winds
Frictional Nearshore Synoptic Scale Winds
2009/1/12
An analytic barotropic model was used to study the nearshore frictional response to synoptic-scale wind forcing. The results depend only on the region where the surface and bottom Ekman layers interac...
Wavenumber Spectra of Pacific Winds Measured by the Seasat Scatterometer
Seasat-A Satellite Scatterometer Wavenumber Spectra
2009/1/12
Vector winds measured by the Seasat-A Satellite Scatterometer (SASS) are analyzed to determine the spatial structure of oceanic surface winds over wavelengths from 200 to 2200 km. The analysis is perf...
Wintertime Winds and Coastal Sea-Level Fluctuations in the Northeast China Sea. Part II：Numerical Model
Wintertime Winds Northeast China Sea Coastal Sea-Level Fluctuations Numerical Model
2009/1/10
As a sequel to data analysis reported in Part I, a numerical model of the wintertime wind-driven circulation of the northeast Chine Sea is developed with the primary purpose of achieving an understand...
Circulation Driven by Winds and Surface Cooling
Surface Cooling vertical velocity Circulation Driven
2009/1/6
A three-layer model of ocean circulation in a Northern Hemisphere basin is driven by winds that are anticyclonic in the south and cyclonic in the north. The ocean is also driven by surface cooling, wh...
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...
A Numerical Study on the Influence of the Mid-Atlantic Ridge on Nonlinear First-Mode Baroclinic Rossby Waves Generated by Seasonal Winds
quasi-geostrophic Nonlinear First-Mode Baroclinic Rossby Waves Mid-Atlantic Ridge Seasonal Winds
2009/1/5
A numerical model simulation investigates the influence of the mid-Atlantic ridge on nonlinear first-mode baroclinic Rossby waves generated by seasonal wind fluctuations. The North Atlantic is simulat...