Publications des scientifiques de l'IRD

Morrow R., Carret A., Birol F., Nino Fernando, Valladeau G., Boy F., Bachelier Céline, Zakardjian B. (2017). Observability of fine-scale ocean dynamics in the northwestern Mediterranean Sea. Ocean Science, 13 (1), p. 13-29. ISSN 1812-0784.

Titre du document
Observability of fine-scale ocean dynamics in the northwestern Mediterranean Sea
Année de publication
2017
Type de document
Article référencé dans le Web of Science WOS:000392137300001
Auteurs
Morrow R., Carret A., Birol F., Nino Fernando, Valladeau G., Boy F., Bachelier Céline, Zakardjian B.
Source
Ocean Science, 2017, 13 (1), p. 13-29 ISSN 1812-0784
Technological advances in the recent satellite altimeter missions of Jason-2, SARAL/AltiKa and CryoSat-2 have improved their signal-to-noise ratio, allowing us to observe finer-scale ocean processes with along-track data. Here, we analyse the noise levels and observable ocean scales in the northwestern Mediterranean Sea, using spectral analyses of along-track sea surface height from the three missions. Jason-2 has a higher mean noise level with strong seasonal variations, with higher noise in winter due to the rougher sea state. SARAL/AltiKa has the lowest noise, again with strong seasonal variations. CryoSat-2 is in synthetic aperture radar (SAR) mode in the Mediterranean Sea but with lower-resolution ocean corrections; its statistical noise level is moderate with little seasonal variation. These noise levels impact on the ocean scales we can observe. In winter, when the mixed layers are deepest and the submesoscale is energetic, all of the altimeter missions can observe wavelengths down to 40-50 km (individual feature diameters of 20-25 km). In summer when the submesoscales are weaker, SARAL can detect ocean scales down to 35 km wavelength, whereas the higher noise from Jason-2 and CryoSat-2 blocks the observation of scales less than 50-55 km wavelength. This statistical analysis is completed by individual case studies, where filtered along-track altimeter data are compared with co-located glider and high-frequency (HF) radar data. The glider comparisons work well for larger ocean structures, but observations of the smaller, rapidly moving dynamics are difficult to co-locate in space and time (gliders cover 200 km in a few days, altimetry in 30 s). HF radar surface currents at Toulon measure the meandering Northern Current, and their good temporal sampling shows promising results in comparison to co-located SARAL altimetric currents. Techniques to separate the geostrophic component from the wind-driven ageostrophic flow need further development in this coastal band.
Plan de classement
Limnologie physique / Océanographie physique [032]
Description Géographique
MEDITERRANNEE
Localisation
Fonds IRD [F B010068883]
Identifiant IRD
fdi:010068883
Contact
  • Coordonnées :
    IST / IRD Ile-de-France
    32 avenue Henri Varagnat
    93140 Bondy Cedex
    France
    Horizon Pleins textes
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