(?) D. Michel will give the talk at the GOCE User Workshop. In this paper the applicability of multiscale methods to oceanography is demonstrated. More precisely, we use convolutions with certain locally supported kernels to approximate the dynamic topography and the geostrophic flow. As data sets the French CLS01 data are used for the mean sea surface topography and are compared to the EGM96 geoid. Since those two data sets have very different levels of spatial resolutions the necessity of an interpolating or approximating tool is evident. Compared to the standard spherical harmonics approach, the strongly space localizing kernels improve the possibilities of local data analysis here
We study a stationary Quasi-Geostrophic type equation in one or two dimensional spaces, with a quick...
International audienceThe dynamics of the ocean flow are governed by the cascade process where the e...
This paper deals with the problem of determining the sea surface topography from geostrophic flow of...
The following two papers present recent developments in multiscale ocean circulation modeling and mu...
In modern geoscience, understanding the climate depends on the information about the oceans. Coverin...
In contemporary ocean science, modeling systems that integrate understanding of complex multiscale p...
this paper. After reviewing the basics of the multiscale framework we will outline in Section 3 a ne...
International audienceMost existing methods in analyzing motion in Computer Vision do not take into ...
A fast multisca; optimal interpolation algorithm has been adapted to the mapping of hydrographic and...
International audienceThis article develops on a microcanonical formulation for the analysis of the ...
International audienceA fundamental challenge in oceanography is the synoptic determination of ocean...
A challenging problem in oceanography is the dense estimation of the surface of the ocean in a stati...
In principle the global mean geostrophic surface circulation of the ocean can be diagnosed by subtra...
International audienceTwo different products have been developed based on gridded satellite data. Th...
International audienceDerivation of high-resolution (HR) spatial distribution of data is a fundament...
We study a stationary Quasi-Geostrophic type equation in one or two dimensional spaces, with a quick...
International audienceThe dynamics of the ocean flow are governed by the cascade process where the e...
This paper deals with the problem of determining the sea surface topography from geostrophic flow of...
The following two papers present recent developments in multiscale ocean circulation modeling and mu...
In modern geoscience, understanding the climate depends on the information about the oceans. Coverin...
In contemporary ocean science, modeling systems that integrate understanding of complex multiscale p...
this paper. After reviewing the basics of the multiscale framework we will outline in Section 3 a ne...
International audienceMost existing methods in analyzing motion in Computer Vision do not take into ...
A fast multisca; optimal interpolation algorithm has been adapted to the mapping of hydrographic and...
International audienceThis article develops on a microcanonical formulation for the analysis of the ...
International audienceA fundamental challenge in oceanography is the synoptic determination of ocean...
A challenging problem in oceanography is the dense estimation of the surface of the ocean in a stati...
In principle the global mean geostrophic surface circulation of the ocean can be diagnosed by subtra...
International audienceTwo different products have been developed based on gridded satellite data. Th...
International audienceDerivation of high-resolution (HR) spatial distribution of data is a fundament...
We study a stationary Quasi-Geostrophic type equation in one or two dimensional spaces, with a quick...
International audienceThe dynamics of the ocean flow are governed by the cascade process where the e...
This paper deals with the problem of determining the sea surface topography from geostrophic flow of...