Observations on the Circulation in the Alboran Sea Using ERS1 Altimetry and Sea Surface Temperature Data

Abstract Data from the altimeter onboard the European Remote Sensing Satellite (ERSI) was used to Study the circulation of the Alboran Sea between 35° and 38°N, 0° and 6°W. This region is dominated by two anticyclonic gyres that are quasi-stationary in space but at times collapse over periods as short as 9 days. Maps of sea level residual, between February 1992 and December 1993, were created from the ERSI data with high correlation between sea surface temperature and residual sea level in the eastern part of the Alboran Sea. The spatially coherent signal was then extracted using the technique of complex empirical orthogonal analysis with the first three modes statistically significant. The variability of the first complex empirical orthogonal function mode appears to be associated with the incoming jet through the straits of Gibraltar with three time periods of high amplitude during the 1992–93 time frame. The second and third modes appear to be associated with the variability of both the western and eas...

[1]  R. Preisendorfer,et al.  A Significance Test for Principal Components Applied to a Cyclone Climatology , 1982 .

[2]  Richard H. Rapp,et al.  The Ohio State 1991 geopotential and sea surface topography harmonic coefficient models , 1991 .

[3]  J. Gascard,et al.  Water masses and circulation in the Western Alboran Sea and in the Straits of Gibraltar , 1985 .

[4]  P. L. Violette,et al.  The Atlantic inflow in the western Alboran Sea , 1990 .

[5]  J. Horel Complex Principal Component Analysis: Theory and Examples , 1984 .

[6]  Jordi Font,et al.  Comparison between ERS-1 SAR images and acoustic Doppler current profiler (ADCP) velocity data in the Alboran Sea , 1994, Remote Sensing.

[7]  Joaquín Tintoré,et al.  Mesoscale Dynamics and Vertical Motion in the Alborán Sea , 1991 .

[8]  P. L. Violette Short-term Measurements of Surface Currents Associated with the Alboran Sea Gyre during Donde Va? , 1986 .

[9]  G. Parrilla,et al.  The Physical Oceanography of the Alboran Sea. , 1987 .

[10]  Joaquín Tintoré,et al.  A study of an intense density front in the eastern Alboran Sea: the Almeria-Oran front , 1988 .

[11]  Victor Zlotnicki,et al.  Seasonal variability in global sea level observed with Geosat altimetry , 1989 .

[12]  P. L. Violette,et al.  Variations in the structure of the anticyclonic gyres found in the Alboran Sea , 1990 .

[13]  William G. Pichel,et al.  Comparative performance of AVHRR‐based multichannel sea surface temperatures , 1985 .

[14]  B. Cushman-Roisin,et al.  A General Theory for Equivalent Barotropic Thin Jets , 1993 .

[15]  P. E. Laviolette The Western Mediterranean Circulation Experiment (WMCE) , 1990 .

[16]  J. Vázquez Observations on the long-period variability of the Gulf Stream downstream of Cape Hatteras , 1993 .

[17]  John B. Shoven,et al.  I , Edinburgh Medical and Surgical Journal.

[18]  R. Arnone,et al.  The origin and characteristics of the Algerian Current , 1990 .

[19]  Paul E. La Violette,et al.  The Western Mediterranean Circulation Experiment (WMCE): Introduction , 1990 .