WebFeb 16, 2011 · The wind stress data covers the globe from 79.5°S to 79.5°N with 1° horizontal resolution, spanning from March 1992 to December 2000. The Niño 3.4 index is obtained from the Climate Prediction Center of the … Web58N) zonal wind stress, tx, being relatively too strong compared to the y derivative of the wind stress curl term, (curlt)y, associated with the intertropical convergence zone. This is confirmed in solutions forced by interannual winds, which exhibit a wide range of responses from being very similar to the observed NECC to being extremely
SST and wind stress perturbations for seasonal and annual …
WebA Global Ocean Wind Stress Climatology Based on ECMWF Analyses. This report discusses the computations of the surface wind stress over the global oceans using … WebECMWF Ocean ReAnalysis System 5 (ORAS5) Jan 1980: Dec 2024: 1981-2010: ECMWF ORAS5 Documentation: ECMWF Ocean ReAnalysis System 5 (ORA20C) Jan 1979 (Jan 1901 at EC) Dec 2009: ... Wind Stress Forcing, u component: N/m**2: Momentum Flux, v component: Wind Stress Forcing, v component: N/m**2: Total Downward Heat Flux at … can通讯和485通讯区别
ECMWF ERA Interim, Daily
WebA GLOBAL OCEAN WIND STRESS CLIMATOLOGY BASED ON ECMWF ANALYSES KEVIN E. TRENBERTH JERRY G. OLSON WILLIAM G. LARGE T (ANNUAL) 0 30E 60E 90E 120E 150E 180 150 120N 90 6W 30W 0 CLIMATE AND GLOBAL DYNAMICS DIVISION ... The wind stress statistics over the southern oceans are believed to be the … WebThe new Surface Wind Thematic Assembly Center (TAC) builds on the heritage of the former OSI TAC. Scatterometers provide important global information on the air-sea interface (fluxes) and on ocean forcing by their wind and surface stress products. Wind stress forces ocean dynamics, triggers mixing of water and evaporates water. Webwind-driven contribution can be isolated from the total observed current. [6] The second step of the study is to use these high-frequency wind-driven currents together with the ECMWF (European Centre for Medium-Range Weather Forecasts) wind stress data to fit a wind-driven current model based on Ekman theory [Ekman, 1905]. According to Ekman’s caj文件用什么打开