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A standard test for AGCMs including their physical parametrizations. II: Results for The Met Office Model
Affiliation:1. State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China;2. University of Chinese Academy of Sciences, Beijing 100049, China;3. School of Environment, Earth and Ecosystem Sciences, the Open University, Milton Keynes MK7 6AA, UK;4. School of Geographical Sciences, University of Bristol, Bristol BS8 1SS, UK;5. Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla 666303, China;1. Aix Marseille Univ, CNRS, IRD, INRAE, CEREGE, Aix-en-Provence, France;2. IRD, DIADE, University of Montpellier, Montpellier, France;3. Laboratoire des Sciences du Climat et de l''Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, 91191 Gif-sur-Yvette, France;4. Université Paris Cité, Institut de physique du globe de Paris, CNRS, F-75005 Paris, France;5. Department of Geological Engineering, Middle East Technical University, Ankara, Turkey;6. Senckenberg Biodiversity and Climate Research Centre (SBiK-F), Senchenberganlage 25, D-60325 Frankfurt am Main, Germany;7. Géosciences Rennes, UMR CNRS 6118, Univ Rennes, Rennes, France;8. Institute of Geosciences, Potsdam University, Potsdam, Germany;9. Departamento de Geología, Facultad de Ciencias Físicas y Matematicas, Universidad de Chile, Chile;10. Department of Botany and Zoology, Faculty of Science, Masaryk University, Brno, Czech Republic
Abstract:Example results are shown for the proposed aqua-planet experiments using a version of The Met Office Unified Model (UM). The zonal mean circulation exhibits strong sensitivity to the latitudinal distribution of sea-surface temperatures (SST). Longitudinal variation of SST yields information on the linearity and distribution of the convective response.
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