Terrestrial Carbon Cycle Dynamics under Recent and Future Climate Change
- 15 May 2005
- journal article
- Published by American Meteorological Society in Journal of Climate
- Vol. 18 (10), 1609-1628
- https://doi.org/10.1175/jcli3359.1
Abstract
The behavior of the terrestrial carbon cycle under historical and future climate change is examined using the University of Victoria Earth System Climate Model, now coupled to a dynamic terrestrial vegetation and global carbon cycle model. When forced by historical emissions of CO2 from fossil fuels and land-use change, the coupled climate–carbon cycle model accurately reproduces historical atmospheric CO2 trends, as well as terrestrial and oceanic uptake for the past two decades. Under six twenty-first-century CO2 emissions scenarios, both terrestrial and oceanic carbon sinks continue to increase, though terrestrial uptake slows in the latter half of the century. Climate–carbon cycle feedbacks are isolated by comparing a coupled model run with a run where climate and the carbon cycle are uncoupled. The modeled positive feedback between the carbon cycle and climate is found to be relatively small, resulting in an increase in simulated CO2 of 60 ppmv at the year 2100. Including non-CO2 greenhouse ... Abstract The behavior of the terrestrial carbon cycle under historical and future climate change is examined using the University of Victoria Earth System Climate Model, now coupled to a dynamic terrestrial vegetation and global carbon cycle model. When forced by historical emissions of CO2 from fossil fuels and land-use change, the coupled climate–carbon cycle model accurately reproduces historical atmospheric CO2 trends, as well as terrestrial and oceanic uptake for the past two decades. Under six twenty-first-century CO2 emissions scenarios, both terrestrial and oceanic carbon sinks continue to increase, though terrestrial uptake slows in the latter half of the century. Climate–carbon cycle feedbacks are isolated by comparing a coupled model run with a run where climate and the carbon cycle are uncoupled. The modeled positive feedback between the carbon cycle and climate is found to be relatively small, resulting in an increase in simulated CO2 of 60 ppmv at the year 2100. Including non-CO2 greenhouse ...Keywords
This publication has 42 references indexed in Scilit:
- Amazonian forest dieback under climate-carbon cycle projections for the 21st centuryTheoretical and Applied Climatology, 2004
- Tropical forests and the global carbon cycle: impacts of atmospheric carbon dioxide, climate change and rate of deforestationPhilosophical Transactions Of The Royal Society B-Biological Sciences, 2004
- Modelling the impact of future changes in climate, CO2 concentration and land use on natural ecosystems and the terrestrial carbon sinkGlobal Environmental Change, 2004
- On the magnitude of positive feedback between future climate change and the carbon cycleGeophysical Research Letters, 2002
- Global temperature change and its uncertainties since 1861Geophysical Research Letters, 2001
- Carbon balance of the terrestrial biosphere in the Twentieth Century: Analyses of CO2, climate and land use effects with four process‐based ecosystem modelsGlobal Biogeochemical Cycles, 2001
- Simulating the ice‐thickness distribution in a coupled climate modelJournal of Geophysical Research: Oceans, 2001
- Estimating historical changes in global land cover: Croplands from 1700 to 1992Global Biogeochemical Cycles, 1999
- The variability in the carbon sinks as reconstructed for the last 1000 yearsGeophysical Research Letters, 1999
- Climate‐chemical interactions and effects of changing atmospheric trace gasesReviews of Geophysics, 1987