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Sea Level Change
Sea Level Change

... Long-term climate change Many aspects of climate change will persist for many centuries even if emissions of greenhouse gases are stopped! •  20% of emitted CO2 will remain in the atmosphere more than 1000 years •  Sea level will continue to rise for many centuries in response to deep ocean warming ...
Global Warming: The Scientific Basis for Anthropogenic Climate
Global Warming: The Scientific Basis for Anthropogenic Climate

... by th the IPCC(2007) tto range ffrom 18 to 59cm by 2100. A further 10 to 20cm may occur due to melting of ice sheets. • However further ice sheet contributions cannot be discounted or at present quantified. • 20,000 yrs BP when temperatures were 4 to 7°C less than present sea level was 120m below pr ...
Addressing the Disparity between Climate Models and
Addressing the Disparity between Climate Models and

... oscillations of atmosphere-ocean systems. They also ignore the huge uncertainties in aerosol forcings (which are absorbed in their choice for climate sensitivity). ...
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... of relatively small changes in the solar output; conversely, if the sensitivity is less than about 1.5 ◦ C, then it is virtually impossible to explain glacial cycling given the forcings of which we are aware. Based on this perspective, then, projections for the 21st century made by the IPCC in earli ...
Assessments of Impacts and Adaptations to Climate Change in
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... change vulnerabilities and adaptation. More than 100 participants from 45 countries attended the vulnerability and adaptation workshop. The format of the workshop was a mixture of plenary lectures given by invited experts, case studies presented by AIACC study team members, computer lab work with se ...
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Carbon Sequestration - Geophysical Laboratory

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... enterprise on the basis of threats, real or perceived, alone (Crichton), incorrect use of economic models for assessing future emissions scenarios (Foster), and finally, an incorrect interpretation of meteorological data from satellite sensors (Foster). I also have NASA Oceans and Ice Branch materia ...
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CMIP5 data provided at the IPCC Data Distribution Centre

... capabilities of forecast systems on decadal time scales, 3) more generally, determining why similarly forced models produce a range of responses, and 4) supplying sample climate futures arising from a range of forcing scenarios that span uncertainties in future climate for application in impact, ada ...
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observed climate change in the caribbean

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The Role of CCS as a Mitigation Option within the IPCC
The Role of CCS as a Mitigation Option within the IPCC

... Prospective areas in sedimentary basins where suitable saline formations, oil or gas fields, or coal beds may be found. Locations for storage in coal beds are only partly included. Prospectivity is a qualitative assessment of the likelihood that a suitable storage location is present in a given area ...
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... warm pool of water with SSTs reaching 33 °C, compared to the present day western Pacific warm pool temperatures of 30 °C. The warmest regions over land occur in the subtropical desert regions. Climate of the last 150,000 Years Carrie Morrill (CCR) is creating a database of high-resolution paleoclima ...
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Criticism of the IPCC Fourth Assessment Report

The IPCC Fourth Assessment Report (AR4) is a report on climate change created with the help of a large number of contributors, both scientists and governmental representatives. There has been considerable political controversy over a small number of errors found in the report, and there have been calls for review of the process used to formulate the report. The overwhelming majority view of scientists with expertise in climate change is that errors, when found, are corrected, and the issues as identified do not undermine the conclusions of the report that the climate system is warming in response to increased levels of greenhouse gases, largely due to human activities.
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