It is well established that the terrestrial biosphere is currently a net carbon sink, driven by increases in productivity, but the mechanisms involved remain uncertain. Observations indicating large-scale increases in productivity across northern terrestrial ecosystems include aircraft data that show an increase in the amplitude of the seasonal cycle of CO2 (ASC) between 45-90N of 56±9.8% over the last 50 years (1958-61 - 2009-11), and satellite observed greening trends of 0.25-0.5%yr 1 between 30-90N since the 1980s. I analyse output from 13 terrestrial biosphere models taking part in the Multi-scale Synthesis and Terrestrial Model Intercomparison Project (MsTMIP) against these observations, which together provide a powerful benchmarks for...
The carbon cycle strongly interacts with the nitrogen cycle. Several observations show that the effe...
The Global Carbon Project estimates that the terrestrial biosphere has absorbed about one-third of a...
Realistic projection of future climate-carbon (C) cycle feedbacks requires better understanding and ...
Observations show an increasing amplitude in the seasonal cycle of CO2 (ASC) north of 45 degrees N o...
Observations show an increasing amplitude in the seasonal cycle of CO2 (ASC) north of 45°N of 56 ± 9...
International audienceObservations show an increasing amplitude in the seasonal cycle of CO 2 (ASC) ...
Observations show an increasing amplitude in the seasonal cycle of CO₂ (ASC) north of 45°N of 56 ± 9...
The terrestrial biosphere has experienced dramatic changes in recent decades. Estimates of historica...
Atmospheric monitoring of high northern latitudes (> 40°N) has shown an enhanced seasonal cycle of c...
Northern ecosystems contain much of the global reservoir of terrestrial carbon that is potentially r...
Terrestrial ecosystems play a significant role in the global carbon cycle and offset a large fractio...
Precise measurements in air are helping to clarify the fate of CO2 released by human activities. Oxy...
Primary productivity of terrestrial vegetation is expected to increase under the influence of increa...
AbstractPrimary productivity of terrestrial vegetation is expected to increase under the influence o...
LetterInternational audienceThe carbon balance of terrestrial ecosystems is particularly sensitive t...
The carbon cycle strongly interacts with the nitrogen cycle. Several observations show that the effe...
The Global Carbon Project estimates that the terrestrial biosphere has absorbed about one-third of a...
Realistic projection of future climate-carbon (C) cycle feedbacks requires better understanding and ...
Observations show an increasing amplitude in the seasonal cycle of CO2 (ASC) north of 45 degrees N o...
Observations show an increasing amplitude in the seasonal cycle of CO2 (ASC) north of 45°N of 56 ± 9...
International audienceObservations show an increasing amplitude in the seasonal cycle of CO 2 (ASC) ...
Observations show an increasing amplitude in the seasonal cycle of CO₂ (ASC) north of 45°N of 56 ± 9...
The terrestrial biosphere has experienced dramatic changes in recent decades. Estimates of historica...
Atmospheric monitoring of high northern latitudes (> 40°N) has shown an enhanced seasonal cycle of c...
Northern ecosystems contain much of the global reservoir of terrestrial carbon that is potentially r...
Terrestrial ecosystems play a significant role in the global carbon cycle and offset a large fractio...
Precise measurements in air are helping to clarify the fate of CO2 released by human activities. Oxy...
Primary productivity of terrestrial vegetation is expected to increase under the influence of increa...
AbstractPrimary productivity of terrestrial vegetation is expected to increase under the influence o...
LetterInternational audienceThe carbon balance of terrestrial ecosystems is particularly sensitive t...
The carbon cycle strongly interacts with the nitrogen cycle. Several observations show that the effe...
The Global Carbon Project estimates that the terrestrial biosphere has absorbed about one-third of a...
Realistic projection of future climate-carbon (C) cycle feedbacks requires better understanding and ...