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Long-term Climate Change: Projections, Commitments and Irreversibility
This chapter assesses long-term projections of climate change for the end of the 21st century and beyond, where the forced signal depends on the scenario and is typically larger than the internalExpand
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On the interpretation of inter-model spread in CMIP5 climate sensitivity estimates
This study diagnoses the climate sensitivity, radiative forcing and climate feedback estimates from eleven general circulation models participating in the Fifth Phase of the Coupled ModelExpand
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Marine boundary layer clouds at the heart of tropical cloud feedback uncertainties in climate models
[1] The radiative response of tropical clouds to global warming exhibits a large spread among climate models, and this constitutes a major source of uncertainty for climate sensitivity estimates. ToExpand
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Potential impact of climate change on marine export production
Future climate change will affect marine productivity, as well as other many components of Earth system. We have investigated the response of marine productivity to global warming with two differentExpand
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How positive is the feedback between climate change and the carbon cycle?
Future climate change induced by atmospheric emissions of greenhouse gases is believed to have a large impact on the global carbon cycle. Several offline studies focusing either on the marine or onExpand
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The GCM‐Oriented CALIPSO Cloud Product (CALIPSO‐GOCCP)
[1] This article presents the GCM-Oriented Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Cloud Product (GOCCP) designed to evaluate the cloudiness simulated by generalExpand
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Impact of the LMDZ atmospheric grid configuration on the climate and sensitivity of the IPSL-CM5A coupled model
The IPSL-CM5A climate model was used to perform a large number of control, historical and climate change simulations in the frame of CMIP5. The refined horizontal and vertical grid of the atmosphericExpand
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Simulated Antarctic precipitation and surface mass balance at the end of the twentieth and twenty-first centuries
The aim of this work is to assess potential future Antarctic surface mass balance changes, the underlying mechanisms, and the impact of these changes on global sea level. To this end, this paperExpand
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An Assessment of the Primary Sources of Spread of Global Warming Estimates from Coupled Atmosphere–Ocean Models
Abstract Climate feedback analysis constitutes a useful framework for comparing the global mean surface temperature responses to an external forcing predicted by general circulation models (GCMs).Expand
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Positive feedback between future climate change and the carbon cycle
Future climate change due to increased atmo- sphericCO 2 may affect land and ocean efficiency to absorb atmosphericCO 2. Here, using climate and carbon three- dimensional models forced by a 1% perExpand
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