Ocean models are generally forced by synthetic (global) NWP model wind fields. It has however bee...
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The aim of this work is to find optimal error correlation functions that enable 2DVAR to arrive a...
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Wind vectors derived from scatterometer measurements are spatially detailed as compared to global...
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This document describes the interaction between the ADM-Aeolus zero-wind-calibration measurements...
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The difference between the theoretical Rayleigh-Brillouin lineshape and the measured lineshape fr...
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