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      The unprecedented 2015/16 Tasman Sea marine heatwave

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          Abstract

          The Tasman Sea off southeast Australia exhibited its longest and most intense marine heatwave ever recorded in 2015/16. Here we report on several inter-related aspects of this event: observed characteristics, physical drivers, ecological impacts and the role of climate change. This marine heatwave lasted for 251 days reaching a maximum intensity of 2.9 °C above climatology. The anomalous warming is dominated by anomalous convergence of heat linked to the southward flowing East Australian Current. Ecosystem impacts range from new disease outbreaks in farmed shellfish, mortality of wild molluscs and out-of-range species observations. Global climate models indicate it is very likely to be that the occurrence of an extreme warming event of this duration or intensity in this region is respectively ≥330 times and ≥6.8 times as likely to be due to the influence of anthropogenic climate change. Climate projections indicate that event likelihoods will increase in the future, due to increasing anthropogenic influences.

          Abstract

          The Tasman Sea experienced an unprecedented marine heatwave in 2015/16, with important ecological impacts. Oliver et al. link this event to warm, southwards flowing waters from East Australia and find that climate change has made these events almost seven times more likely.

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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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            The NCEP Climate Forecast System Version 2

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              A hierarchical approach to defining marine heatwaves

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                Author and article information

                Journal
                Nat Commun
                Nat Commun
                Nature Communications
                Nature Publishing Group
                2041-1723
                14 July 2017
                2017
                : 8
                : 16101
                Affiliations
                [1 ]Institute for Marine and Antarctic Studies, University of Tasmania , 20 Castray Esplanade, Battery Point, Private Bag 129, Hobart, Tasmania 7001, Australia
                [2 ]Australian Research Council Centre of Excellence for Climate System Science, University of Tasmania , Private Bag 129, Hobart, Tasmania 7001, Australia
                [3 ]Australian Institute of Marine Science , PMB 3, Townsville MC, Townsville, Queensland 4810, Australia
                [4 ]Antarctic and Climate Ecosystem Cooperative Research Centre, University of Tasmania , Private Bag 80, Hobart, Tasmania 7001, Australia
                [5 ]CSIRO Oceans and Atmosphere , Hobart, Tasmania 7000, Australia
                [6 ]Climate Change Research Centre, University of New South Wales , Gate 11 Botany Street, Library Walk, Level 4, Mathews Building, Sydney, New South Wales 2052, Australia
                [7 ]Australian Research Council Centre of Excellence for Climate System Science, University of New South Wales , Gate 11 Botany Street, Library Walk, Level 4, Mathews Building, Sydney, New South Wales 2052, Australia
                Author notes
                Author information
                http://orcid.org/0000-0002-3523-6254
                Article
                ncomms16101
                10.1038/ncomms16101
                5519980
                28706247
                3dede5fd-0123-4524-ab0f-f8631fd14ee1
                Copyright © 2017, The Author(s)

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

                History
                : 04 January 2017
                : 29 May 2017
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