In this study, we used MITgcm-REcoM2 to simulate the stepwise glacial-interglacial atmospheric pCO2 change. A general description of the model can be found in the supporting material for Hauck et al. 2013. There are seven simulations included in this dataset: two control runs for interglacial and glacial conditions (IG_ctl, G_ctl); three region-specific sensitivity runs(IG_Gso, IG_Gna, IG_Gns); and two simulations regarding the glacial iron fertilization in the Southern Ocean. Dissolved Inorganic Carbon (DIC) and Export Production in all runs are included in this study, and the potential temperature (THETA), salinity (SALT), meridional velocity (VVEL), sea ice concentration(SIarea), air-sea surface pCO2 (dpCO2surface) difference are availa...
Model intercomparison studies of coupled carbon-climate simulations have the potential to improve ou...
The ocean thermohaline circulation is important for transports of heat and the carbon cycle. We pres...
∆14Catm has been estimated as 420 ± 80‰ (IntCal09) during the Last Glacial Maximum (LGM) compared to...
The mechanisms of strong glacial-interglacial variations in the atmospheric CO2 concentration and th...
A series of Last Glacial Maximum (LGM) marine carbon cycle sensitivity experiments is conducted to ...
Using the Earth system model of intermediate complexity Bern3D, we transiently simulate changes in a...
Possible mechanisms for the 80 ppm reduction of atmospheric CO2 partial pressure during the last gla...
We use an Earth system model of intermediate complexity, CLIMBER-2, to investigate what recent impro...
During glacial-interglacial cycles, atmospheric CO2 concentration varied by about 100 ppmv in amplit...
Possible mechanisms for the 80 ppm reduction of atmospheric CO2 partial pressure during the last gla...
We have developed and employed an Earth system model to explore the forcings of atmospheric pCO(2) c...
The prevailing hypothesis for lower atmospheric carbon dioxide (CO2) concentrations during glacial p...
[1] The glacial/interglacial rise in atmospheric pCO2 is one of the best known changes in paleoclima...
Possible mechanisms for the 80 ppm reduction of atmospheric CO2 partial pressure during the last gla...
[1] The glacial/interglacial rise in atmospheric pCO2 is one of the best known changes in paleoclima...
Model intercomparison studies of coupled carbon-climate simulations have the potential to improve ou...
The ocean thermohaline circulation is important for transports of heat and the carbon cycle. We pres...
∆14Catm has been estimated as 420 ± 80‰ (IntCal09) during the Last Glacial Maximum (LGM) compared to...
The mechanisms of strong glacial-interglacial variations in the atmospheric CO2 concentration and th...
A series of Last Glacial Maximum (LGM) marine carbon cycle sensitivity experiments is conducted to ...
Using the Earth system model of intermediate complexity Bern3D, we transiently simulate changes in a...
Possible mechanisms for the 80 ppm reduction of atmospheric CO2 partial pressure during the last gla...
We use an Earth system model of intermediate complexity, CLIMBER-2, to investigate what recent impro...
During glacial-interglacial cycles, atmospheric CO2 concentration varied by about 100 ppmv in amplit...
Possible mechanisms for the 80 ppm reduction of atmospheric CO2 partial pressure during the last gla...
We have developed and employed an Earth system model to explore the forcings of atmospheric pCO(2) c...
The prevailing hypothesis for lower atmospheric carbon dioxide (CO2) concentrations during glacial p...
[1] The glacial/interglacial rise in atmospheric pCO2 is one of the best known changes in paleoclima...
Possible mechanisms for the 80 ppm reduction of atmospheric CO2 partial pressure during the last gla...
[1] The glacial/interglacial rise in atmospheric pCO2 is one of the best known changes in paleoclima...
Model intercomparison studies of coupled carbon-climate simulations have the potential to improve ou...
The ocean thermohaline circulation is important for transports of heat and the carbon cycle. We pres...
∆14Catm has been estimated as 420 ± 80‰ (IntCal09) during the Last Glacial Maximum (LGM) compared to...