搜索结果: 1-15 共查到“理学 Wind Forcing”相关记录28条 . 查询时间(0.138 秒)
On stochastic stability of regional ocean models with uncertainty in wind forcing
stochastic stability regional ocean models uncertainty in wind forcing
font style='font-size:12px;'>
2009/11/3
A shallow-water model was used to understand model error induced by non-Gaussian wind uncertainty. Although the model was simple, it described a generic system with many degrees of freedom randomized ...
Wave fluxes of equatorial Kelvin waves and QBO zonal wind forcing derived from SABER and ECMWF temperature space-time spectra
Wave fluxes equatorial Kelvin waves QBO zonal wind forcing SABER
font style='font-size:12px;'>
2009/6/22
The quasi-biennial oscillation (QBO) of the zonal mean zonal wind is a dynamical phenomenon of the tropical middle atmosphere. Influences of the QBO can even be found at mid and high latitudes. It is ...
Sea Surface Temperature Response to Variations in Atmospheric Wind Forcing
Sea Surface Temperature Atmospheric Wind Forcing
font style='font-size:12px;'>
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...
Resonant Topographic Response of Nearshore Currents to Wind Forcing
topographic wave effect Nearshore Currents Wind Forcing
font style='font-size:12px;'>
2009/2/5
Model calculations and current meter observations are analyzed in the spectral domain and in the time domain to investigate effects of topographic waves on the response of nearshore currents to wind. ...
Mean Flow Generation on a Continental Margin by Periodic Wind Forcing
Mean Flow Generation Continental Margin Periodic Wind Forcing
font style='font-size:12px;'>
2009/1/21
The generation of an alongshore mean flow by the nonlinear interaction of forced barotropic shelf waves over a continental margin is studied using a wind-forced, f-plane model with bottom friction in ...
Frictional Response of Continental Shelf Water to Local Wind Forcing
coastal sea level Continental Shelf Water Local Wind Forcing
font style='font-size:12px;'>
2009/1/16
Because of relatively strong tidal currants and little notification, the response of continental shelf water to wired off South Carolina is predominantly frictional and barotropic. Currents measured a...
Frictional Continental Shelf Waves and the Circulation Response of a Continental Shelf to Wind Forcing
Frictional Continental Shelf Waves Continental Shelf Wind Forcing
font style='font-size:12px;'>
2009/1/16
This paper is an examination of the wind-forced circulation on continental shelves with bottom friction. Since the response is integrally dependent on the cross-shelf structures and dispersion charact...
The Response of Stratified, Frictional Flow of Shelf and Slope Waters to Fluctuating Large-Scale, Low-Frequency Wind Forcing
Frictional Flow Slope Waters Fluctuating Large-Scale Low-Frequency Wind Forcing
font style='font-size:12px;'>
2009/1/15
Numerical and analytical models are developed to discuss large-scale, low-frequency, wind-driven fluctuations over the continental shelf and slope in the presence of realistic density stratification a...
The Resonant Response of Interannual Baroclinic Rossby Waves to Wind Forcing in the Eastern Midlatitude North Pacific
Interannual Baroclinic Rossby Waves Wind Forcing Eastern Midlatitude North Pacific
font style='font-size:12px;'>
2009/1/15
During the four year period 1976–80, mesoscale anomalies of 300 m temperature in the eastern midlatitude North Pacific were observed propagating westward from the coast of North America to 165°W at ap...
Stochastic Wind Forcing of Baroclinic Rossby Waves in the Presence of a Meridional Boundary
Stochastic Wind Forcing Baroclinic Rossby Waves Meridional Boundary
font style='font-size:12px;'>
2009/1/15
The quasigeostrophic response of a continuously stratified ocean to a band-limited white-noise windstress curl is examined in an infinite and semi-infinite ocean. Baroclinic Rossby waves—predominantly...
The Distortion of a Baroclinic Fofonoff Gyre by Wind Forcing
Baroclinic Fofonoff Gyre Wind Forcing
font style='font-size:12px;'>
2009/1/5
The subtropical recirculation regions are considered as examples of nonlinear free flow—“baroclinic Fofonoff gyres.” In the interior, where relative vorticity may be neglected, the quad-geostrophic as...
Wind Forcing and the Zonal Structure of the Equatorial Undercurrent
Wind Forcing Equatorial Undercurrent Zonal Structure
font style='font-size:12px;'>
2009/1/4
A recently developed nonlinear inviscid model of the equatorial undercurrent is coupled to wind-driven surface layer. Wind stress drives a poleward Ekman flow, causing equatorial divergence of surface...
Quasi-geostrophic Ocean Response to Real Wind Forcing：The Effects of Temporal Smoothing
Quasi-geostrophic Ocean Response Real Wind Forcing Temporal Smoothing
font style='font-size:12px;'>
2008/12/24
A one-degree, flat bottom, eight-layer quasi-geostrophic model of the North Pacific Ocean is forced by six different wind stress curl datasets, all derived from seven years of twice daily analyses at ...
Local and Remote Wind Forcing of New South Wales Inner Shelf Currents and Sea Level
adjusted sea level coastal trapped wave New South Wales
font style='font-size:12px;'>
2008/12/23
Linear multiple regression analysis is used to identify the locally and remotely wind-driven components of the nearshore current and adjusted sea level (ASL) variability at Sydney, New South Wales. Th...
The Local and Nonlocal Response of Conception Bay to Wind Forcing
Conception Bay Wind Forcing
font style='font-size:12px;'>
2008/12/19
In this paper the response of Conception Bay to wind forcing is discussed. Current meter and thermistor chain observations are analysed and compared with output from a reduced-gravity numerical model....