J
J. P. Blanchet
Researcher at State University of New York System
Publications - 5
Citations - 1679
J. P. Blanchet is an academic researcher from State University of New York System. The author has contributed to research in topics: Climate change & Sea surface temperature. The author has an hindex of 5, co-authored 5 publications receiving 1612 citations.
Papers
More filters
Journal ArticleDOI
Intercomparison and interpretation of climate feedback processes in 19 atmospheric general circulation models
R. D. Cess,Gerald L. Potter,J. P. Blanchet,George J. Boer,A. D. Del Genio,Michel Déqué,V. P. Dymnikov,V. Galin,W. L. Gates,Steven J. Ghan,Jeffrey T. Kiehl,Andrew A. Lacis,H. Le Treut,Z. X. Li,Xin-Zhong Liang,B. J. McAvaney,V. P. Meleshko,John F. B. Mitchell,Jean-Jacques Morcrette,David A. Randall,L. Rikus,Erich Roeckner,Jean-François Royer,U. Schlese,D. A. Sheinin,A. Slingo,A. P. Sokolov,Karl E. Taylor,Warren M. Washington,R. T. Wetherald,I. Yagai,Minghua Zhang +31 more
TL;DR: In this paper, the authors provided an intercomparison and interpretation of climate feedback processes in 19 atmospheric general circulation models and found that a roughly threefold variation in one measure of global climate sensitivity was found among the 19 models.
Journal ArticleDOI
Interpretation of Cloud-Climate Feedback as Produced by 14 Atmospheric General Circulation Models
R. D. Cess,Gerald L. Potter,J. P. Blanchet,George J. Boer,Steven J. Ghan,Jeffrey T. Kiehl,H. Le Treut,Z. X. Li,Xin-Zhong Liang,John F. B. Mitchell,Jean-Jacques Morcrette,David A. Randall,M. R. Riches,E. Roeckner,U. Schlese,A. Slingo,Karl E. Taylor,Warren M. Washington,R. T. Wetherald,I. Yagai +19 more
TL;DR: An intercomparison of 14 atmospheric general circulation models showed that there was a roughly threefold variation in global climate sensitivity, a result that emphasizes the need for improvements in the treatment of clouds in these models if they are ultimately to be used as climatic predictors.
Journal ArticleDOI
Interpretation of snow-climate feedback as produced by 17 general circulation models.
Robert D. Cess,Gerald L. Potter,Minghua Zhang,J. P. Blanchet,S. Chalita,Robert Colman,D. A. Dazlich,A. D. Del Genio,V. P. Dymnikov,V. Galin,D. Jerrett,E. Keup,Andrew A. Lacis,H. Le Treut,Xin-Zhong Liang,J. F. Mahfouf,B. J. McAvaney,V. P. Meleshko,John F. B. Mitchell,Jean-Jacques Morcrette,P. M. Norris,David A. Randall,L. Rikus,Erich Roeckner,Jean-François Royer,U. Schlese,D. A. Sheinin,Julia Slingo,A. S. Sokolov,Karl E. Taylor,Warren M. Washington,R. T. Wetherald,I. Yagai +32 more
TL;DR: An intercomparison of 17 general circulation models suggests that additional amplification or moderation may be caused both by cloud interactions and longwave radiation.
Journal ArticleDOI
Intercomparison and interpretation of surface energy fluxes in atmospheric general circulation models
David A. Randall,Robert D. Cess,J. P. Blanchet,George J. Boer,D. A. Dazlich,A. D. Del Genio,Michel Déqué,V. P. Dymnikov,V. Galin,Steven J. Ghan,Andrew A. Lacis,H. Le Treut,Z. X. Li,Xin-Zhong Liang,B. J. McAvaney,V. P. Meleshko,John F. B. Mitchell,J.-J. Morcrette,Gerald L. Potter,L. Rikus,Erich Roeckner,Jean-François Royer,U. Schlese,D. A. Sheinin,Julia Slingo,A. P. Sokolov,Karl E. Taylor,Warren M. Washington,R. T. Wetherald,I. Yagai,Minghua Zhang +30 more
TL;DR: In this article, the responses of the surface energy budgets and hydrologic cycles of 19 atmospheric general circulation models to an imposed, globally uniform sea surface temperature perturbation of 4 K were analyzed.
Journal ArticleDOI
Analysis of snow feedbacks in 14 general circulation models
David A. Randall,Robert D. Cess,J. P. Blanchet,S. Chalita,Robert Colman,D. A. Dazlich,A. D. Del Genio,E. Keup,Andrew A. Lacis,H. Le Treut,Xin-Zhong Liang,B. J. McAvaney,Jean-François Mahfouf,V. P. Meleshko,J.-J. Morcrette,P. M. Norris,Gerald L. Potter,L. Rikus,Erich Roeckner,Jean-François Royer,U. Schlese,D. A. Sheinin,A. P. Sokolov,Karl E. Taylor,R. T. Wetherald,I. Yagai,Minghua Zhang +26 more
TL;DR: In this article, the surface energy budgets of 14 atmospheric general circulation models have been analyzed through idealized numerical experiments, and the response of each model is analyzed in detail the responses of one model with a strong positive snow feedback and another with a weak negative snow feedback.