A wind-forced linear model has been used to produce 21 years (1964--1984) of monthly time series of surface dynamic height in the Equatorial Atlantic. Theclimatological seasonal cycle is substracted, and the statistical characteristics of the residuals are analyzed. An empirical orthogonal function analysis reveals that the most significant pattern has deviations of one sign in the Western Equatorial Atlantic. The anomalies in the last 2 years, 1983 and 1984, are particularly large. The time component of the first empirical orthogonal function peaks in july 1983, changes sign at the end of 1983, and has an extremun of the opposite sign in April 1984. At that time, the zonal slope of dynamic height had reversed with respect to normal along t...
Upper ocean temperature data obtained during the Seasonal Response of the Equatorial Atlantic experi...
International audience10 years of surface geostrophic currents from TOPEX/Poséïdon altimetric data a...
Geosat altimeter data from November 1986 through November 1987 are analyzed over the Tropical Atlant...
A wind-forced linear model has been used to produce 21 years (1964--1984) of monthly time series of ...
Two different wind data sets of the years 1982-1984 are used to force in linear multimode model of t...
Hellerman and Rosenstein's (1983) climatological winds are used to force a linear, continuously stra...
Altimetric data, climatological hydrological data, and numerical model results are compared over the...
Geosat altimeter data between april 1985 and september 1989 are analyzed in the Tropical Atlantic oc...
A new analysis of the historical temperature and salinity profiles in the tropical Atlantic is done ...
In this study we objectively analyze simulated Equatorial Atlantic ocean data on seasonal time scale...
Modelling and observational evidence indicate that interannual variabilities of dynamic height and ...
The equatorial regions of the Earth\u27s oceans are climatically sensitive ones because of the zonal...
Modelling and observational evidence indicate that interannual variabilities of dynamic height and s...
The equatorial regions of the Earth\u27s oceans are climatically sensitive ones because of the zonal...
The equatorial regions of the Earth\u27s oceans are climatically sensitive ones because of the zonal...
Upper ocean temperature data obtained during the Seasonal Response of the Equatorial Atlantic experi...
International audience10 years of surface geostrophic currents from TOPEX/Poséïdon altimetric data a...
Geosat altimeter data from November 1986 through November 1987 are analyzed over the Tropical Atlant...
A wind-forced linear model has been used to produce 21 years (1964--1984) of monthly time series of ...
Two different wind data sets of the years 1982-1984 are used to force in linear multimode model of t...
Hellerman and Rosenstein's (1983) climatological winds are used to force a linear, continuously stra...
Altimetric data, climatological hydrological data, and numerical model results are compared over the...
Geosat altimeter data between april 1985 and september 1989 are analyzed in the Tropical Atlantic oc...
A new analysis of the historical temperature and salinity profiles in the tropical Atlantic is done ...
In this study we objectively analyze simulated Equatorial Atlantic ocean data on seasonal time scale...
Modelling and observational evidence indicate that interannual variabilities of dynamic height and ...
The equatorial regions of the Earth\u27s oceans are climatically sensitive ones because of the zonal...
Modelling and observational evidence indicate that interannual variabilities of dynamic height and s...
The equatorial regions of the Earth\u27s oceans are climatically sensitive ones because of the zonal...
The equatorial regions of the Earth\u27s oceans are climatically sensitive ones because of the zonal...
Upper ocean temperature data obtained during the Seasonal Response of the Equatorial Atlantic experi...
International audience10 years of surface geostrophic currents from TOPEX/Poséïdon altimetric data a...
Geosat altimeter data from November 1986 through November 1987 are analyzed over the Tropical Atlant...