Paper
22 December 2000 Tracking anticyclonic open-sea eddies in the Algerian basin by altimetry
Jordi Isern-Fontanet, Jose de Jesus Salas Perez, S. Ruiz, Jordi Font, C. Millot
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Abstract
The evolution of an open-sea eddy, previously detected by IR imagery, is studied using Sea Level Anomalies (SLA) maps. This evolution is compared with the information given by surface drifters deployed along eddy diameter, during ALGERS98 cruise in western Mediterranean. Preliminary results show a good agreement between the structure observed form drifters trajectories and the velocity field obtained from SLA maps assuming a geostrophic balance. The center of the eddy is taken as the grid point of maximum SLA. Differences between this center and the center given by the drifters seen to be due to the precision of the grid used by altimetric maps. From the position of the centers the propagation velocity of the eddy is obtained. The mean velocity obtained from altimetry is 2.7 km/day which is coherent with previous studies.
© (2000) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
Jordi Isern-Fontanet, Jose de Jesus Salas Perez, S. Ruiz, Jordi Font, and C. Millot "Tracking anticyclonic open-sea eddies in the Algerian basin by altimetry", Proc. SPIE 4172, Remote Sensing of the Ocean and Sea Ice 2000, (22 December 2000); https://doi.org/10.1117/12.411709
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Cited by 3 scholarly publications.
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KEYWORDS
Infrared imaging

Infrared radiation

In situ metrology

Infrared detectors

Lanthanum

Solids

3D metrology

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