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  5. The INGV-CMCC Seasonal Prediction System: improved ocean initial conditions
 
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The INGV-CMCC Seasonal Prediction System: improved ocean initial conditions

Author(s)
Alessandri, A. 
Centro Euro-Mediterraneo per i cambiamenti Climatici, Bologna, Italy 
Borrelli, A. 
Centro Euro-Mediterraneo per i Cambiamenti Climatici, Bologna, Italy 
Masina, S. 
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia 
Cherchi, A. 
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia 
Gualdi, S. 
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia 
Navarra, A. 
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia 
Di Pietro, P. 
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia 
Language
English
Obiettivo Specifico
3.7. Dinamica del clima e dell'oceano
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Title of the book
Monthly Weather Review 
Issue/vol(year)
/138 (2010)
ISSN
0027-0644
Electronic ISSN
1520-0493
Publisher
American Meteorological Society
Pages (printed)
2930-2952
Issued date
2010
URI
https://www.earth-prints.org/handle/2122/5852
Subjects
03. Hydrosphere::03.01. General::03.01.03. Global climate models 
Keywords
  • ocean modelling

  • global climate models...

  • seasonal forecast

  • coupled models

Abstract
The development of the INGV (Istituto Nazionale di Geofisica e Vulcanologia)-CMCC (Centro
Euro-Mediterraneo per i Cambiamenti Climatici) Seasonal Prediction System (SPS) is
documented. In this SPS the ocean initial conditions estimation includes a Reduced Order
Optimal Interpolation procedure for the assimilation of temperature and salinity profiles
at the global scale. Nine member ensemble forecasts have been produced for the period
1991-2003 for two starting dates per year in order to assess the impact of the subsurface
assimilation in the ocean for initialization.
Comparing the results with control simulations (i.e.: without assimilation of subsurface
profiles during ocean initialization), we showed that the improved ocean initialization increases
the skill in the prediction of tropical Pacific SSTs in our system for boreal winter
forecasts. Considering the forecast of the El Ni˜no 1997-1998, the data assimilation in the
ocean initial conditions leads to a considerable improvement in the representation of its onset
and development.
Our results indicate a better prediction of global scale surface climate anomalies for the
forecasts started in November, probably due to the improvement in the tropical Pacific. For
boreal winter, in both tropics and extra tropics, we show significant increases in the capability
of the system to discriminate above normal and below normal temperature anomalies.
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