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  • 1
    Online Resource
    Online Resource
    Collingwood :CSIRO Publishing,
    Keywords: Climatic changes-Australia-Congresses. ; Global warming-Congresses. ; Global temperature changes-Congresses. ; Climatic changes-Congresses. ; Climatic changes-Social aspects-Congresses. ; Greenhouse effect, Atmospheric-Australia-Congresses. ; Electronic books.
    Description / Table of Contents: Provides an important snapshot of the issues presented at the Greenhouse 2009 conference.
    Type of Medium: Online Resource
    Pages: 1 online resource (299 pages)
    Edition: 1st ed.
    ISBN: 9780643100176
    DDC: 363.73874
    Language: English
    Note: Intro -- Title -- Copyright -- Foreword -- Contents -- Preface -- List of contributors -- 1. Climate change: are we up to the challenge -- 2. Climate change and the Great Crash of 2008 -- Part 1 Climate change science -- 3. Twenty years of Australian Climate Change Science Program research -- 4. Tropical Australia and the Australian monsoon: general assessment and projected changes -- 5. Recent and projected rainfall trends in south-west Australia and the associated shifts in weather systems -- 6. How human-induced aerosols influence the ocean-atmosphere circulation: a review -- 7. Freshwater biodiversity and climate change -- 8. Causes of changing southern hemisphere weather systems -- Part 2 Impacts and adaptation -- 9. Australian agriculture in a climate of change -- 10. Wheat, wine and pie charts: advantages and limits to using current variability to think about future change in South Australia's climate -- 11. Managing extreme heat in the vineyard: some lessons from the 2009 summer heatwave -- 12. Getting on target: energy and water efficiency in Western Australia's housing -- 13. Sustainable energy as the primary tool to ameliorate climate change -- 14. A national energy efficiency program for low-income households: responding equitably to climate change -- 15. Applying a climate change adaptation decision framework for the Adelaide-Mt Lofty Ranges -- 16. Responding to oil vulnerability and climate change in our cities -- 17. Managing climate risk in human settlements -- 18. Adapting infrastructure for climate change impacts -- 19. A critical look at the state of climate adaptation planning -- Part 3 Communicating climate change -- 20. Rising above hot air: a method for exploring attitudes towards zero-carbon lifestyles. , 21. Investigating the effectiveness of Energymark: changing public perceptions and behaviours using a longitudinal kitchen table approach -- 22. Talking climate change with the bush -- 23. Using Google Earth to visualise climate change scenarios in south-west Victoria -- Index.
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  • 2
    Publication Date: 2022-05-26
    Description: Author Posting. © The Author(s), 2011. This is the author's version of the work. It is posted here by permission of Nature Publishing Group for personal use, not for redistribution. The definitive version was published in Nature Climate Change 2 (2012): 161-166, doi:10.1038/nclimate1353.
    Description: Subtropical western boundary currents are warm, fast flowing currents that form on the western side of ocean basins. They carry warm tropical water to the mid-latitudes and vent large amounts of heat and moisture to the atmosphere along their paths, affecting atmospheric jet streams and mid-latitude storms, as well as ocean carbon uptake. The possibility that these highly energetic and nonlinear currents might change under greenhouse gas forcing has raised significant concerns, but detecting such changes is challenging owing to limited observations. Here, using reconstructed sea surface temperature datasets and newly developed century-long ocean and atmosphere reanalysis products, we find that the post-1900 surface ocean warming rate over the path of these currents is two to three times faster than the global mean surface ocean warming rate. The accelerated warming is associated with a synchronous poleward shift and/or intensification of global subtropical western boundary currents in conjunction with a systematic change in winds over both hemispheres. This enhanced warming may reduce ocean's ability to absorb anthropogenic carbon dioxide over these regions. However, uncertainties in detection and attribution of these warming trends remain, pointing to a need for a long-term monitoring network of the global western boundary currents and their extensions.
    Description: This work is supported by China National Key Basic Research Project (2007CB411800) and National Natural Science Foundation Projects (40788002, 40921004). WC is supported by the Australian Climate Change Science program and the Southeast Australia Climate Initiative. HN is supported in part by the Japanese Ministry of Education, Culture, Sports, Science and Technology through Grant-in-Aid for Scientific Research on Innovative Areas #2205 and by the Japanese Ministry of Environment through Global Environment Research Fund (S-5). MJM is supported by NOAA’s Climate Program Office.
    Description: 2012-07-29
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 3
    Publication Date: 2019-09-23
    Description: Subtropical western boundary currents are warm, fast-flowing currents that form on the western side of ocean basins. They carry warm tropical water to the mid-latitudes and vent large amounts of heat and moisture to the atmosphere along their paths, affecting atmospheric jet streams and mid-latitude storms, as well as ocean carbon uptake1, 2, 3, 4. The possibility that these highly energetic currents might change under greenhouse-gas forcing has raised significant concerns5, 6, 7, but detecting such changes is challenging owing to limited observations. Here, using reconstructed sea surface temperature datasets and century-long ocean and atmosphere reanalysis products, we find that the post-1900 surface ocean warming rate over the path of these currents is two to three times faster than the global mean surface ocean warming rate. The accelerated warming is associated with a synchronous poleward shift and/or intensification of global subtropical western boundary currents in conjunction with a systematic change in winds over both hemispheres. This enhanced warming may reduce the ability of the oceans to absorb anthropogenic carbon dioxide over these regions. However, uncertainties in detection and attribution of these warming trends remain, pointing to a need for a long-term monitoring network of the global western boundary currents and their extensions.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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