Consistent Land- and Atmosphere-Based U.S. Carbon Sink Estimates. Pacala, S. W., Hurtt, G. C., Baker, D., Peylin, P., Houghton, R. A., Birdsey, R. A., Heath, L., Sundquist, E. T., Stallard, R. F., Ciais, P., Moorcroft, P., Caspersen, J. P., Shevliakova, E., Moore, B., Kohlmaier, G., Holland, E., Gloor, M., Harmon, M. E., Fan, S. M., Sarmiento, J. L., Goodale, C. L., Schimel, D., & Field, C. B. 292(5525):2316–2320.
Consistent Land- and Atmosphere-Based U.S. Carbon Sink Estimates [link]Paper  doi  abstract   bibtex   
For the period 1980-89, we estimate a carbon sink in the coterminous United States between 0.30 and 0.58 petagrams of carbon per year (petagrams of carbon = 1015 grams of carbon). The net carbon flux from the atmosphere to the land was higher, 0.37 to 0.71 petagrams of carbon per year, because a net flux of 0.07 to 0.13 petagrams of carbon per year was exported by rivers and commerce and returned to the atmosphere elsewhere. These land-based estimates are larger than those from previous studies (0.08 to 0.35 petagrams of carbon per year) because of the inclusion of additional processes and revised estimates of some component fluxes. Although component estimates are uncertain, about one-half of the total is outside the forest sector. We also estimated the sink using atmospheric models and the atmospheric concentration of carbon dioxide (the tracer-transport inversion method). The range of results from the atmosphere-based inversions contains the land-based estimates. Atmosphere- and land-based estimates are thus consistent, within the large ranges of uncertainty for both methods. Atmosphere-based results for 1980-89 are similar to those for 1985-89 and 1990-94, indicating a relatively stable U.S. sink throughout the period.
@article{pacalaConsistentLandAtmospherebased2001,
  title = {Consistent Land- and Atmosphere-Based {{U}}.{{S}}. Carbon Sink Estimates},
  author = {Pacala, S. W. and Hurtt, G. C. and Baker, D. and Peylin, P. and Houghton, R. A. and Birdsey, R. A. and Heath, L. and Sundquist, E. T. and Stallard, R. F. and Ciais, P. and Moorcroft, P. and Caspersen, J. P. and Shevliakova, E. and Moore, B. and Kohlmaier, G. and Holland, E. and Gloor, M. and Harmon, M. E. and Fan, S. M. and Sarmiento, J. L. and Goodale, C. L. and Schimel, D. and Field, C. B.},
  date = {2001},
  journaltitle = {Science},
  volume = {292},
  pages = {2316--2320},
  issn = {1095-9203},
  doi = {10.1126/science.1057320},
  url = {https://doi.org/10.1126/science.1057320},
  abstract = {For the period 1980-89, we estimate a carbon sink in the coterminous United States between 0.30 and 0.58 petagrams of carbon per year (petagrams of carbon = 1015 grams of carbon). The net carbon flux from the atmosphere to the land was higher, 0.37 to 0.71 petagrams of carbon per year, because a net flux of 0.07 to 0.13 petagrams of carbon per year was exported by rivers and commerce and returned to the atmosphere elsewhere. These land-based estimates are larger than those from previous studies (0.08 to 0.35 petagrams of carbon per year) because of the inclusion of additional processes and revised estimates of some component fluxes. Although component estimates are uncertain, about one-half of the total is outside the forest sector. We also estimated the sink using atmospheric models and the atmospheric concentration of carbon dioxide (the tracer-transport inversion method). The range of results from the atmosphere-based inversions contains the land-based estimates. Atmosphere- and land-based estimates are thus consistent, within the large ranges of uncertainty for both methods. Atmosphere-based results for 1980-89 are similar to those for 1985-89 and 1990-94, indicating a relatively stable U.S. sink throughout the period.},
  keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14007180,carbon-cycle,forest-resources,uncertainty,united-states},
  number = {5525}
}

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