TY - JOUR
T1 - Projecting the future of the U.S. carbon sink
AU - Hurtt, G. C.
AU - Pacala, Stephen Wilson
AU - Moorcroft, P. R.
AU - Caspersen, J.
AU - Shevliakova, E.
AU - Houghton, R. A.
AU - Moore, B.
PY - 2002/2/5
Y1 - 2002/2/5
N2 - Atmospheric and ground-based methods agree on the presence of a carbon sink in the coterminous United States (the United States minus Alaska and Hawaii), and the primary causes for the sink recently have been identified. Projecting the future behavior of the sink is necessary for projecting future net emissions. Here we use two models, the Ecosystem Demography model and a second simpler empirically based model (Miami Land Use History), to estimate the spatio-temporal patterns of ecosystem carbon stocks and fluxes resulting from land-use changes and fire suppression from 1700 to 2100. Our results are compared with other historical reconstructions of ecosystem carbon fluxes and to a detailed carbon budget for the 1980s. Our projections indicate that the ecosystem recovery processes that are primarily responsible for the contemporary U.S. carbon sink will slow over the next century, resulting in a significant reduction of the sink. The projected rate of decrease depends strongly on scenarios of future land use and the long-term effectiveness of fire suppression.
AB - Atmospheric and ground-based methods agree on the presence of a carbon sink in the coterminous United States (the United States minus Alaska and Hawaii), and the primary causes for the sink recently have been identified. Projecting the future behavior of the sink is necessary for projecting future net emissions. Here we use two models, the Ecosystem Demography model and a second simpler empirically based model (Miami Land Use History), to estimate the spatio-temporal patterns of ecosystem carbon stocks and fluxes resulting from land-use changes and fire suppression from 1700 to 2100. Our results are compared with other historical reconstructions of ecosystem carbon fluxes and to a detailed carbon budget for the 1980s. Our projections indicate that the ecosystem recovery processes that are primarily responsible for the contemporary U.S. carbon sink will slow over the next century, resulting in a significant reduction of the sink. The projected rate of decrease depends strongly on scenarios of future land use and the long-term effectiveness of fire suppression.
UR - http://www.scopus.com/inward/record.url?scp=0037022310&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0037022310&partnerID=8YFLogxK
U2 - 10.1073/pnas.012249999
DO - 10.1073/pnas.012249999
M3 - Article
C2 - 11830663
AN - SCOPUS:0037022310
SN - 0027-8424
VL - 99
SP - 1389
EP - 1394
JO - Proceedings of the National Academy of Sciences of the United States of America
JF - Proceedings of the National Academy of Sciences of the United States of America
IS - 3
ER -