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Circulation Modeling in the Northern Adriatic Sea and its Comparison with Nimbus 7 Remotely Sensed Data

  • L. Alberotanza
  • G. Aldighieri
  • V. Barale
  • A. Bergamasco
  • P. Malanotte Rizzoli
  • M. Zicarelli
Part of the Marine Science book series (MR, volume 13)

Abstract

The use of satellite imagery for oceanographic modeling implies the knowledge of many different physical processes and the coverage of many different, successive paths of investigation, each of which constitutes in itself a whole field of research. The following block diagram conveniently summarizes, even though in a very simplified manner, these different passages.

Keywords

Satellite Imagery Remotely Sense Data Scripps Institution Surface Temperature Distribution Successive Path 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. Gordon, H.R., Clarke, D.K., Miller, J.L. and Hovis, W.A., 1980, “Phytoplankton Pigments Derived from the NIMBUS 7 CZCS. Initial Comparisons with Surface Measurements,” Science, 210, 63–66.CrossRefGoogle Scholar
  2. NASA, 1979, “NIMBUS 7 Users’ Guidelines,” private communication. Visibility Lab., Scripps Institution of Oceanography, University of California.Google Scholar
  3. SURFACE II, 1979, “Interpolating Routine Manual,” Internal Report, Scripps Institution of Oceanography, University of California.Google Scholar

Copyright information

© Plenum Press, New York 1981

Authors and Affiliations

  • L. Alberotanza
    • 1
  • G. Aldighieri
    • 1
  • V. Barale
    • 1
  • A. Bergamasco
    • 1
  • P. Malanotte Rizzoli
    • 1
  • M. Zicarelli
    • 2
  1. 1.ISDGM (CNR)VeneziaItaly
  2. 2.Scripps Institution of OceanographyLa JollaUSA

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