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Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model
The continued increase in the atmospheric concentration of carbon dioxide due to anthropogenic emissions is predicted to lead to significant changes in climate. About half of the current emissionsExpand
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Climate-carbon cycle feedback analysis: Results from the C
Eleven coupled climate–carbon cycle models used a common protocol to study the coupling between climate change and the carbon cycle. The models were forced by historical emissions and theExpand
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Couplings between changes in the climate system and biogeochemistry
The Earth's climate is determined by a number of complex connected physical, chemical and biological processes occurring in the atmosphere, land and ocean. The radiative properties of the atmosphere,Expand
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Description of the "TRIFFID" Dynamic Global Vegetation Model
  • P. Cox
  • Environmental Science
  • 2001
This note describes the terrestrial carbon cycle component of the Hadley Centre's coupled climate-carbon cycle model (Cox et al (2000)). \TRIFFID (Top-down Representation of Interactive Foliage andExpand
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Global response of terrestrial ecosystem structure and function to CO2 and climate change: results from six dynamic global vegetation models
The possible responses of ecosystem processes to rising atmospheric CO2 concentration and climate change are illustrated using six dynamic global vegetation models that explicitly represent theExpand
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The Joint UK Land Environment Simulator (JULES), model description – Part 1: Energy and water fluxes
This manuscript describes the energy and water components of a new community land surface model called the Joint UK Land Environment Simulator (JULES). Expand
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The Joint UK Land Environment Simulator (JULES), model description – Part 2: Carbon fluxes and vegetation dynamics
The Joint UK Land Environment Simulator (JULES) is a process-based model that simulates the fluxes of carbon, water, energy and momentum between the land surface and the atmosphere. Expand
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Indirect radiative forcing of climate change through ozone effects on the land-carbon sink
The evolution of the Earth’s climate over the twenty-first century depends on the rate at which anthropogenic carbon dioxide emissions are removed from the atmosphere by the ocean and land carbonExpand
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Amazonian forest dieback under climate-carbon cycle projections for the 21st century
SummaryThe first GCM climate change projections to include dynamic vegetation and an interactive carbon cycle produced a very significant amplification of global warming over the 21st century. UnderExpand
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Detection of a direct carbon dioxide effect in continental river runoff records
Continental runoff has increased through the twentieth century despite more intensive human water consumption. Possible reasons for the increase include: climate change and variability,Expand
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