Return to search

Global mean cloud feedbacks in idealized climate change experiments

Global mean cloud feedbacks in ten atmosphere-only climate models are estimated in perturbed sea surface temperature (SST) experiments and the results compared to doubled CO2 experiments using mixed-layer ocean versions of these same models. The cloud feedbacks in any given
model are generally not consistent: the sign of the net cloud radiative feedback may vary according to the experimental design. However, both sets of experiments indicate that the variation of the total climate feedback across the models depends primarily on the variation of the net cloud feedback. Changes in different cloud types show much greater consistency between the two experiments for any individual model and amongst the set of models analyzed here. This suggests that the SST perturbation experiments may provide useful information on the processes associated with cloud changes which is not evident when analysis is
restricted to feedbacks defined in terms of the change in cloud radiative forcing.

Identiferoai:union.ndltd.org:DRESDEN/oai:qucosa:de:qucosa:13964
Date January 2006
CreatorsRinger, Mark A., McAvaney, Bryant J., Andronova, Natasha, Buja, Lawrence E., Esch, Monika, Ingram, William J., Li, Bin, Quaas, Johannes, Roeckner, Erich, Senior, Catherine Ann, Soden, Brian J., Volodin, Evgeny M., Webb, Mark J., Williams, Keith D.
ContributorsHadley Centre, Meteorology Research Centre, University of Michigan, National Center for Atmospheric Research, Max-Planck-Institut für Meteorologie, University of Oxford, University of Ilinois, University of Miami, Russian Academy of Sciences
PublisherWiley
Source SetsHochschulschriftenserver (HSSS) der SLUB Dresden
LanguageEnglish
Detected LanguageEnglish
Typedoc-type:article, info:eu-repo/semantics/article, doc-type:Text
SourceGeophysical research letters (2006), 33, L07718
Rightsinfo:eu-repo/semantics/openAccess

Page generated in 0.0018 seconds