Horizontal and vertical structure of the representer functions for sea surface measurements in a coastal circulation model

The representer functions used to propagate the information from observations onto model variables in a sequential data assimilation scheme are calculated with a statistical method. The Princeton Ocean Model is used in a simple configuration simulating the North Current flowing along the French coas...

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Veröffentlicht in:Journal of physical oceanography 2000-10, Vol.30 (10), p.2627-2635
Hauptverfasser: ECHEVIN, Vincent, DE MEY, Pierre, EVENSEN, Geir
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creator ECHEVIN, Vincent
DE MEY, Pierre
EVENSEN, Geir
description The representer functions used to propagate the information from observations onto model variables in a sequential data assimilation scheme are calculated with a statistical method. The Princeton Ocean Model is used in a simple configuration simulating the North Current flowing along the French coasts in the northwestern Mediterranean Sea. The influence of sea level measurements on the models' three-dimensional temperature and velocity fields is investigated. Inhomogeneities and directions of anisotropy are evidenced. A comparison with simplified reduced order assimilation methods suggests that such schemes will not allow for consistent assimilation of nearshore altimetric data.
doi_str_mv 10.1175/1520-0485(2000)030<2627:HAVSOT>2.0.CO;2
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source American Meteorological Society; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals
subjects Coastal oceanography, estuaries. Regional oceanography
Data collection
Earth, ocean, space
Exact sciences and technology
External geophysics
Marine
Measurement
Ocean currents
Oceanography
Physics of the oceans
Statistical methods
title Horizontal and vertical structure of the representer functions for sea surface measurements in a coastal circulation model
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