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 = 10(15) 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 al...
The effects of increasing carbon dioxide (CO2) and climate on net carbon storage in terrestrial ecos...
International audienceThe terrestrial carbon sink has been large in recent decades, but its size and...
Atmospheric CO2 inversions estimate surface carbon fluxes from an optimal fit to atmospheric CO2 mea...
International audienceFor the period 1980–89, we estimate a carbon sink in the coterminous United St...
The evolution of the Earth\u27s terrestrial carbon sinks from 1980 to 2005 was investigated by using...
We estimate the northern hemisphere (NH) terrestrial carbon sink by comparing four recent atmospheri...
We estimate the northern hemisphere (NH) terrestrial carbon sink by comparing four recent atmospheri...
There is general agreement that terrestrial systems in the Northern Hemisphere provide a significant...
We present an estimate of net CO2 exchange between the terrestrial biosphere and the atmosphere acro...
There is general agreement that terrestrial systems in the Northern Hemisphere provide a significant...
Scientific understanding of the global carbon cycle is required for developing national and internat...
The magnitude and location of terrestrial carbon sources and sinks remains subject to large uncertai...
Atmospheric CO2 inversions estimate surface carbon fluxes from an optimal fit to atmospheric CO2 mea...
International audienceThe global land and ocean carbon sinks have increased proportionally with incr...
The effects of increasing carbon dioxide (CO2) and climate on net carbon storage in terrestrial ecos...
International audienceThe terrestrial carbon sink has been large in recent decades, but its size and...
Atmospheric CO2 inversions estimate surface carbon fluxes from an optimal fit to atmospheric CO2 mea...
International audienceFor the period 1980–89, we estimate a carbon sink in the coterminous United St...
The evolution of the Earth\u27s terrestrial carbon sinks from 1980 to 2005 was investigated by using...
We estimate the northern hemisphere (NH) terrestrial carbon sink by comparing four recent atmospheri...
We estimate the northern hemisphere (NH) terrestrial carbon sink by comparing four recent atmospheri...
There is general agreement that terrestrial systems in the Northern Hemisphere provide a significant...
We present an estimate of net CO2 exchange between the terrestrial biosphere and the atmosphere acro...
There is general agreement that terrestrial systems in the Northern Hemisphere provide a significant...
Scientific understanding of the global carbon cycle is required for developing national and internat...
The magnitude and location of terrestrial carbon sources and sinks remains subject to large uncertai...
Atmospheric CO2 inversions estimate surface carbon fluxes from an optimal fit to atmospheric CO2 mea...
International audienceThe global land and ocean carbon sinks have increased proportionally with incr...
The effects of increasing carbon dioxide (CO2) and climate on net carbon storage in terrestrial ecos...
International audienceThe terrestrial carbon sink has been large in recent decades, but its size and...
Atmospheric CO2 inversions estimate surface carbon fluxes from an optimal fit to atmospheric CO2 mea...