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Global warming feedbacks on terrestrial carbon uptake under the Intergovernmental Panel on Climate Change (IPCC) Emission Scenarios
Author(s) -
Joos Fortunat,
Prentice I. Colin,
Sitch Stephen,
Meyer Robert,
Hooss Georg,
Plattner GianKasper,
Gerber Stefan,
Hasselmann Klaus
Publication year - 2001
Publication title -
global biogeochemical cycles
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.512
H-Index - 187
eISSN - 1944-9224
pISSN - 0886-6236
DOI - 10.1029/2000gb001375
Subject(s) - radiative forcing , environmental science , atmospheric sciences , greenhouse gas , climatology , climate change , forcing (mathematics) , carbon cycle , biosphere , biosphere model , global warming , temperate climate , carbon sink , climate model , biogeochemical cycle , ecosystem , ecology , oceanography , geology , biology
A coupled physical‐biogeochemical climate model that includes a dynamic global vegetation model and a representation of a coupled atmosphere‐ocean general circulation model is driven by the nonintervention emission scenarios recently developed by the Intergovernmental Panel on Climate Change (IPCC). Atmospheric CO 2 , carbon sinks, radiative forcing by greenhouse gases (GHGs) and aerosols, changes in the fields of surface‐air temperature, precipitation, cloud cover, ocean thermal expansion, and vegetation structure are projected. Up to 2100, atmospheric CO 2 increases to 540 ppm for the lowest and to 960 ppm for the highest emission scenario analyzed. Sensitivity analyses suggest an uncertainty in these projections of −10 to +30% for a given emission scenario. Radiative forcing is estimated to increase between 3 and 8 W m −2 between now and 2100. Simulated warmer conditions in North America and Eurasia affect ecosystem structure: boreal trees expand poleward in high latitudes and are partly replaced by temperate trees and grasses at lower latitudes. The consequences for terrestrial carbon storage depend on the assumed sensitivity of climate to radiative forcing, the sensitivity of soil respiration to temperature, and the rate of increase in radiative forcing by both CO 2 and other GHGs. In the most extreme cases, the terrestrial biosphere becomes a source of carbon during the second half of the century. High GHG emissions and high contributions of non‐CO 2 agents to radiative forcing favor a transient terrestrial carbon source by enhancing warming and the associated release of soil carbon.