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ENACT CLS TASKS The RIO-03 Combined Mean Dynamic Topography (CMDT) |
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The direct method The synthetic method CMDT versus OCCAM, Levitus and Le Grand CMDT RIO-03 References |
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CMDT RIO-03
References
[1]: Rio, M.-H. and F. Hernandez, 2003: A Mean Dynamic Topography computed over the world ocean from altimetry, in-situ measurements and a geoid model. Submitted to Journal of Geophysical Research. [2]: Rio, M.-H. and F. Hernandez, 2003: High frequency response of wind-driven currents measured by drifting buoys and altimetry over the world ocean. Journal of Geophysical Research, 108, 39-1. [3]: Rio, M.-H., 2003: Combinaison de données in situ, altimétriques et gravimétriques pour l'estimation d'une topographie dynamique moyenne globale. Ed. CLS. PhD Thesis, University Paul Sabatier (Toulouse III, France), 260pp. [4]: Hernandez, F., P.-Y. Le Traon, and R. Morrow, 1995: Mapping mesoscale variability of the Azores Current using TOPEX/POSEIDON and ERS-1 altimetry, together with hydrographic and Lagrangian measurements. Journal of Geophysical Research, 100, 24995-25006. [5]: Le Traon, P.-Y. and F. Hernandez, 1992: Mapping the oceanic mesoscale circulation: validation of satellite altimetry using surface drifters. Journal of Atmospheric and Oceanic Technology, 9, 687-698. OCCAM modelling: |
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The direct method The synthetic method CMDT versus OCCAM, Levitus and Le Grand CMDT RIO-03 References |
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