- Home
- » Tags
- » Wind stress
Top View
- Sea Surface Wind Stress and Drag Coefficients: the HEXOS Results
- Comparison of Wind Speed and Wind Stress in the Southern Ocean Chin-Ying Chien
- 1.4 Wind Stress Vector Over Sea Waves
- Coastal Upwelling Under the Influence of Westerly Wind Burst in the North of Papua Continent, Western Pacific
- Friction and Ocean Turbulence Part II
- Characteristics and Dynamics of Wind-Driven Upwelling in the Alaskan Beaufort Sea Based on Six Years of Mooring Data ⁎ Peigen Lina,B, , Robert S
- Lecture 1 Ekman Currents in the Ocean Lecture 7 7.1 Surface Wind Stress
- Midlatitude Wind Stress–Sea Surface Temperature Coupling in the Vicinityof Oceanic Fronts
- Wind Stress Curl Forcing of the Coastal Ocean Near Point Conception, California*
- Viscosity Effects in Wind Wave Generation
- Impact of Surface Waves on Wind Stress Under Low to Moderate Wind Conditions
- Wind‐Driven Evolution of the North Pacific Subpolar Gyre Over the Last
- Atlantic Ocean Hua Jiang,1 Rui Xin Huang,2 and Hui Wang1 Received 28 January 2007; Revised 27 October 2007; Accepted 4 December 2007; Published 14 March 2008
- Introduction to Physical Oceanography and Climate Spring 2020 FAS Course Web Page for EPS 131
- Basics of Ocean Circulation
- Eddy-Mean-Flow Interaction in a Barotropic Ocean Model
- Analysis of Wind Stress Algorithms and Computation of the Wind Stress Curl in Bodega Bay, California
- Estimating Eddy Stresses by Fitting Dynamics to Observations Using a Residual-Mean Ocean Circulation Model and Its Adjoint
- Momentum Flux Measurements in the Airflow Over Wind-Generated Surface Waves
- Ekman Layer Processes Equations of Motion
- Wind Stress Forcing of the Ocean in the SOC Climatology: Comparisons with the NCEP–NCAR, ECMWF, UWM/COADS, and Hellerman and R
- Barotropic Versus Baroclinic Eddy Saturation Navid C
- Wind Generated Currents in Shallow Water
- A Global Climatology of Surface Wind and Wind Stress Fields from Eight Years of Quikscat Scatterometer Data
- Lesson 11 Frictional Flows
- The Atmospheric Response to North Atlantic SST Trends, 1870–2019
- OSCAT Wind Stress & Wind Stress Curl Products
- UNAM, Mexico Lecture 3: the Wind-Driven Oceanic Circulation
- Effects of Wind on Convection in Strongly and Weakly Baroclinic Flows with Application to the Labrador Sea*
- Buoyancy and Wind-Driven Convection at Mixed Layer Density Fronts
- Sea Surface Roughness and Drag Coefficient Under Free Convection Conditions
- Eddy Viscosity
- Swell Impact on Wind Stress and Atmospheric Mixing in a Regional
- Lecture 10: Ocean Circulation Basic Ocean Current Systems
- And Wave-Induced Viscous Stresses Over Strongly Forced Wind Waves
- Alongshore Wind Stress (Out of the Page) the Ekman Layer Takes About a Day to Spin up (Actually the Timescale Is ~ 1/F) with Net Transport to the Right (N
- Climate Model Wind Stress Biases in the Northern Low Latitudes from a Momentum Balance Perspective
- Comparison of Atmospheric Model Wind Stress with Three Different Convective Parameterizations: Sensitivity of Tropical Paci®C Ocean Simulations
- Deep Convection in the Irminger Sea Forced by the Greenland Tip Jet
- Wind-Driven Ekman Dynamics, Concepts of Turbulent Mixed Layer & Thermocline
- Wind and Wave-Driven Circulation in a Fetch-Limited Coastal Basin: Western Long Island Sound" (2019)
- 6. the Ocean's Response to North Atlantic Oscillation Variability