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A study of the Alboran Sea mesoscale system by means of empirical orthogonal function decomposition of satellite data

A study of the Alboran Sea mesoscale system by means of empirical orthogonal function decomposition of satellite data
A study of the Alboran Sea mesoscale system by means of empirical orthogonal function decomposition of satellite data
ALBORAN SEA, REMOTE SENSING, SATELLITES, CHLOROPHYLL, SURFACE TEMPERATURE, EMPIRICAL ORTHOGONAL FUNCTIONS, EOF
0924-7963
293-311
Baldacci, A.
b5ef0ad2-c1b1-4a58-a528-c12899e718aa
Corsini, G.
dd150a5d-ec46-466a-a5a4-3f17b312efb0
Grasso, R.
c020b26b-124b-4787-a160-c61871cb0d8d
Manzella, G.
9e53700d-dde4-42fe-9074-5af85346f8f3
Allen, J.T.
b251a62b-f443-4591-b695-9aa8c4d73741
Cipollini, P.
276e356a-f29e-4192-98b3-9340b491dab8
Guymer, T.H.
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Snaith, H.M.
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Baldacci, A.
b5ef0ad2-c1b1-4a58-a528-c12899e718aa
Corsini, G.
dd150a5d-ec46-466a-a5a4-3f17b312efb0
Grasso, R.
c020b26b-124b-4787-a160-c61871cb0d8d
Manzella, G.
9e53700d-dde4-42fe-9074-5af85346f8f3
Allen, J.T.
b251a62b-f443-4591-b695-9aa8c4d73741
Cipollini, P.
276e356a-f29e-4192-98b3-9340b491dab8
Guymer, T.H.
0ef2c701-1900-46e0-a595-49707cc32c32
Snaith, H.M.
40f759ed-8c90-4d76-8e9c-7d7a4c264adf

Baldacci, A., Corsini, G., Grasso, R., Manzella, G., Allen, J.T., Cipollini, P., Guymer, T.H. and Snaith, H.M. (2001) A study of the Alboran Sea mesoscale system by means of empirical orthogonal function decomposition of satellite data. Journal of Marine Systems, 29 (1-4), 293-311. (doi:10.1016/S0924-7963(01)00021-5).

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Published date: 2001
Keywords: ALBORAN SEA, REMOTE SENSING, SATELLITES, CHLOROPHYLL, SURFACE TEMPERATURE, EMPIRICAL ORTHOGONAL FUNCTIONS, EOF

Identifiers

Local EPrints ID: 7991
URI: http://eprints.soton.ac.uk/id/eprint/7991
ISSN: 0924-7963
PURE UUID: ef65cf67-1974-43f4-8c99-6442feadc7e0

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Date deposited: 24 Aug 2004
Last modified: 15 Mar 2024 04:50

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Contributors

Author: A. Baldacci
Author: G. Corsini
Author: R. Grasso
Author: G. Manzella
Author: J.T. Allen
Author: P. Cipollini
Author: T.H. Guymer
Author: H.M. Snaith

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