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  • 1
    Keywords: Sea ice ; Climatic changes ; Environmental impact analysis ; Arctic regions Climate ; Konferenzschrift ; Arktis ; Arktische Zone ; Meereis ; Eisscholle ; Glaziologie ; Reduktion ; Nordpolarmeer ; Packeis ; Treibeis ; Meereskunde
    Type of Medium: Book
    Pages: VIII, 269 S. , Ill., graph. Darst., Kt.
    ISBN: 9780875904450
    Series Statement: Geophysical monograph 180
    DDC: 551.34/3091632
    RVK:
    Language: English
    Note: This book grew out of a special session at the 2006 annual meeting of the American Geophysical Union titled "Rapid transition from perennial to seasonal Arctic sea ice"
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  • 2
    Online Resource
    Online Resource
    Newark :American Geophysical Union,
    Keywords: Climatic changes--Environmental aspects--Arctic regions. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (279 pages)
    Edition: 1st ed.
    ISBN: 9781118671580
    Series Statement: Geophysical Monograph Series ; v.180
    DDC: 551.34/3091632
    Language: English
    Note: Intro -- Title Page -- Contents -- Preface -- Arctic Sea Ice Decline: Introduction -- Section I: Arctic Sea Ice in the Instrumented and Paleo-Proxy Records -- Recent Trends in Arctic Sea Ice and the Evolving Role of Atmospheric Circulation Forcing, 1979-2007 -- Reconstructing Sea Ice Conditions in the Arctic and Sub-Arctic Prior to Human Observations -- Section II: Factors in Sea Ice Sensitivity -- Arctic Cloud Properties and Radiative Forcing From Observations and Their Role in Sea Ice Decline Predicted by the NCAR CCSM3 Model During the 21st Century -- Some Aspects of Uncertainty in Predicting Sea Ice Thinning -- Sensitivity of Arctic Sea Ice Thickness to Intermodel Variations in the Surface Energy Budget -- The Atmospheric Response to Realistic Reduced Summer Arctic Sea Ice Anomalies -- Section III: Rapid Loss Versus Abrupt Transition -- Sea Ice-Albedo Feedback and Nonlinear Arctic Climate Change -- The Role of Natural Versus Forced Change in Future Rapid Summer Arctic Ice Loss -- Multiple Equilibria and Abrupt Transitions in Arctic Summer Sea Ice Extent -- What Is the Trajectory of Arctic Sea Ice? -- Analysis of Arctic Sea Ice Anomalies in a Coupled Model Control Simulation -- Section IV: The Threat to Polar Bears From Sea Ice Decline -- A Bayesian Network Modeling Approach to Forecasting the 21st Century Worldwide Status of Polar Bears -- Index.
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  • 3
    Publication Date: 2020-06-02
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 4
    Publication Date: 2022-05-25
    Description: Author Posting. © American Meteorological Society 2006. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Climate 19 (2006): 2122–2143, doi:10.1175/JCLI3761.1.
    Description: The Community Climate System Model version 3 (CCSM3) has recently been developed and released to the climate community. CCSM3 is a coupled climate model with components representing the atmosphere, ocean, sea ice, and land surface connected by a flux coupler. CCSM3 is designed to produce realistic simulations over a wide range of spatial resolutions, enabling inexpensive simulations lasting several millennia or detailed studies of continental-scale dynamics, variability, and climate change. This paper will show results from the configuration used for climate-change simulations with a T85 grid for the atmosphere and land and a grid with approximately 1° resolution for the ocean and sea ice. The new system incorporates several significant improvements in the physical parameterizations. The enhancements in the model physics are designed to reduce or eliminate several systematic biases in the mean climate produced by previous editions of CCSM. These include new treatments of cloud processes, aerosol radiative forcing, land–atmosphere fluxes, ocean mixed layer processes, and sea ice dynamics. There are significant improvements in the sea ice thickness, polar radiation budgets, tropical sea surface temperatures, and cloud radiative effects. CCSM3 can produce stable climate simulations of millennial duration without ad hoc adjustments to the fluxes exchanged among the component models. Nonetheless, there are still systematic biases in the ocean–atmosphere fluxes in coastal regions west of continents, the spectrum of ENSO variability, the spatial distribution of precipitation in the tropical oceans, and continental precipitation and surface air temperatures. Work is under way to extend CCSM to a more accurate and comprehensive model of the earth's climate system.
    Description: We would like to acknowledge the substantial contributions to and support for the CCSM project from the National Science Foundation (NSF), the Department of Energy (DOE), the National Oceanic and Atmospheric Administration, and the National Aeronautics and Space Administration.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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