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      Catalogue of abrupt shifts in Intergovernmental Panel on Climate Change climate models.

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          Abstract

          Abrupt transitions of regional climate in response to the gradual rise in atmospheric greenhouse gas concentrations are notoriously difficult to foresee. However, such events could be particularly challenging in view of the capacity required for society and ecosystems to adapt to them. We present, to our knowledge, the first systematic screening of the massive climate model ensemble informing the recent Intergovernmental Panel on Climate Change report, and reveal evidence of 37 forced regional abrupt changes in the ocean, sea ice, snow cover, permafrost, and terrestrial biosphere that arise after a certain global temperature increase. Eighteen out of 37 events occur for global warming levels of less than 2°, a threshold sometimes presented as a safe limit. Although most models predict one or more such events, any specific occurrence typically appears in only a few models. We find no compelling evidence for a general relation between the overall number of abrupt shifts and the level of global warming. However, we do note that abrupt changes in ocean circulation occur more often for moderate warming (less than 2°), whereas over land they occur more often for warming larger than 2°. Using a basic proportion test, however, we find that the number of abrupt shifts identified in Representative Concentration Pathway (RCP) 8.5 scenarios is significantly larger than in other scenarios of lower radiative forcing. This suggests the potential for a gradual trend of destabilization of the climate with respect to such shifts, due to increasing global mean temperature change.

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          Most cited references44

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          An Overview of CMIP5 and the Experiment Design

          The fifth phase of the Coupled Model Intercomparison Project (CMIP5) will produce a state-of-the- art multimodel dataset designed to advance our knowledge of climate variability and climate change. Researchers worldwide are analyzing the model output and will produce results likely to underlie the forthcoming Fifth Assessment Report by the Intergovernmental Panel on Climate Change. Unprecedented in scale and attracting interest from all major climate modeling groups, CMIP5 includes “long term” simulations of twentieth-century climate and projections for the twenty-first century and beyond. Conventional atmosphere–ocean global climate models and Earth system models of intermediate complexity are for the first time being joined by more recently developed Earth system models under an experiment design that allows both types of models to be compared to observations on an equal footing. Besides the longterm experiments, CMIP5 calls for an entirely new suite of “near term” simulations focusing on recent decades and the future to year 2035. These “decadal predictions” are initialized based on observations and will be used to explore the predictability of climate and to assess the forecast system's predictive skill. The CMIP5 experiment design also allows for participation of stand-alone atmospheric models and includes a variety of idealized experiments that will improve understanding of the range of model responses found in the more complex and realistic simulations. An exceptionally comprehensive set of model output is being collected and made freely available to researchers through an integrated but distributed data archive. For researchers unfamiliar with climate models, the limitations of the models and experiment design are described.
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            Open-ocean convection: Observations, theory, and models

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              Thermohaline Convection with Two Stable Regimes of Flow

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                Author and article information

                Journal
                Proc. Natl. Acad. Sci. U.S.A.
                Proceedings of the National Academy of Sciences of the United States of America
                Proceedings of the National Academy of Sciences
                1091-6490
                0027-8424
                Oct 27 2015
                : 112
                : 43
                Affiliations
                [1 ] Research and Development, Weather and Climate Modeling, Royal Netherlands Meteorological Institute, 3730AE De Bilt, The Netherlands; National Oceanography Centre Southampton, University of Southampton, Southampton SO14 3ZH, United Kingdom; S.S.Drijfhout@soton.ac.uk.
                [2 ] Department of Environmental Sciences, Wageningen University, 6708PB Wageningen, The Netherlands; The Land in the Earth System, Max Planck Institute for Meteorology, 20146 Hamburg, Germany;
                [3 ] National Oceanography Centre Southampton, University of Southampton, Southampton SO14 3ZH, United Kingdom;
                [4 ] The Land in the Earth System, Max Planck Institute for Meteorology, 20146 Hamburg, Germany;
                [5 ] The Land in the Earth System, Max Planck Institute for Meteorology, 20146 Hamburg, Germany; Center for Earth System Research and Sustainability, Universität Hamburg, 20146 Hamburg, Germany;
                [6 ] Climate System Group, Centre for Ecology and Hydrology, Wallingford OX10 8BB, United Kingdom;
                [7 ] Department of Environmental Sciences, Wageningen University, 6708PB Wageningen, The Netherlands;
                [8 ] Laboratoire des Sciences du Climat et de l'Environnnement, Institut Pierre Simon Laplace, 91191 Gif-sur-Yvette, Paris, France;
                [9 ] Environnements et Paleoenvironnements Oceaniques et Continentaux, University of Bordeaux, 33615 Pessac, France.
                Article
                1511451112
                10.1073/pnas.1511451112
                4629371
                26460042
                ec926399-1b39-4ccc-b599-6dbe670efa15
                History

                abrupt climate change,IPCC,critical transitions,CMIP5,climate change

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