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  5. From weather to ocean predictions: an historical viewpoint
 
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From weather to ocean predictions: an historical viewpoint

Author(s)
Pinardi, Nadia  
Department of Physics and Astronomy, University of Bologna, Viale B. Pichat 6/2, 40127 Bologna Italy  
Cavaleri, L.  
CNR-Istituto di Scienze Marine, Venice, Italy  
Coppini, Giovanni  
Centro EuroMediterraneo sui Cambiamenti Climatici, Lecce, Italy  
De Mey, P.  
LEGOS, Toulouse, France  
Fratianni, Claudia  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia  
Huthnance, J.  
Proudman Oceanographic Laboratory, Bidslon Observatory, Birkenhead, Merseyside, United Kingdom  
Lermusiaux, P. F. J.  
Department of Mechanical Engineering, Massachusetts Institute of Technology, Cambridge, MA 02139, USA  
Navarra, Antonio  
Centro EuroMediterraneo sui Cambiamenti Climatici, Lecce, Italy  
Preller, R.  
Naval Research Laboratory, Stennis Space Center, Mississippi, USA  
Tibaldi, S.  
Centro EuroMediterraneo sui Cambiamenti Climatici, Lecce, Italy  
Language
English
Obiettivo Specifico
4A. Oceanografia e clima
Status
Published
JCR Journal
JCR Journal
Journal
Journal of Marine Research  
Issue/vol(year)
3/73 (2017)
Pages (printed)
103-159
Date Issued
2017
DOI
10.1357/002224017821836789
URI
https://www.earth-prints.org/handle/2122/11669
Subjects
03.03. Physical  
Subjects

atmospheric predictio...

Abstract
This paper reviews the historical development of concepts and practices in the science of ocean
predictions. It begins with meteorology, which conducted the first forecasting experiment in 1950,
followed by wind waves, and continuing with tidal and storm surge predictions to arrive at the first
successful ocean mesoscale forecast in 1983. The work of Professor A. R. Robinson of Harvard University,
who produced the first mesoscale ocean predictions for the deep ocean regions is documented
for the first time. The scientific and technological developments that made accurate ocean predictions
possible are linked with the gradual understanding of the importance of the oceanic mesoscales and
their inclusion in the numerical models. Ocean forecasting developed first at the regional level, due to
the relatively low computational requirements, but by the end of the 1990s, it was possible to produce
global ocean uncoupled forecasts and coupled ocean-atmosphere seasonal forecasts.
Type
article
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