En-tête de navigationNavigation principaleSuiviFiche


Unité de recherche
PCRD EU
Numéro de projet
95.0640
Titre du projet
HIRETYCS: High Resolution 10 Year Climate Simulations
Titre du projet anglais
HIRETYCS: High Resolution 10 Year Climate Simulations

Textes relatifs à ce projet

 AllemandFrançaisItalienAnglais
Mots-clé
-
-
-
Anzeigen
Autre Numéro de projet
-
-
-
Anzeigen
Programme de recherche
-
-
-
Anzeigen
Description succincte
-
-
-
Anzeigen
Partenaires et organisations internationales
-
-
-
Anzeigen
Résumé des résultats (Abstract)
-
-
-
Anzeigen
Références bases de données
-
-
-
Anzeigen

Textes saisis


CatégorieTexte
Mots-clé
(Anglais)
Global climate; climate modeling; general circulation models
Autre Numéro de projet
(Anglais)
EU project number: ENV4-CT95-0184
Programme de recherche
(Anglais)
EU-programme: 4. Frame Research Programme - 3.1 Environment
Description succincte
(Anglais)
See abstract
Partenaires et organisations internationales
(Anglais)
Météo-France, Hadley Centre, MPI, University of l'Aquila, INM, IRM and UCL, ADG Bologna, LGGE, SMHI
Résumé des résultats (Abstract)
(Anglais)
A comprehensive dataset of direct observations has been used to assess the surface energy fluxes in the GCMs participating in the HIRETYCS project. A number of shortcomings are identified in the models: The absorption of solar radiation at the surface is significantly overestimated in two of the models compared with more than 700 observation sites. A combination of the surface observations with collocated TOA measurements from satellites attributes these overestimates to a lack of absorption of solar radiation in the model atmospheres. This lack of absorption is also found in the cloud-free atmosphere, and is related to an underestimation of water vapour and aerosol absorption. In the longwave, evidence is presented that the longwave downward radiation is underestimated in the models, particularly at higher latitudes. This induces an artificially strong meridional gradient. The most apparent model bias in the non-radiative components of the surface energy balance is an overly small latent heat flux over continents in summer in two of the models, caused by an excessive summer dryness. All of the above biases are not notably reduced with higher resolution,indicating that the parameterization of model physics, rather than horizontal resolution, is the bottleneck on the way to a more reliable reproduction of the surface climate in GCMs.
Références bases de données
(Anglais)
Swiss Database: Euro-DB of the
State Secretariat for Education and Research
Hallwylstrasse 4
CH-3003 Berne, Switzerland
Tel. +41 31 322 74 82
Swiss Project-Number: 95.0640