Articles | Volume 14, issue 1
Geosci. Model Dev., 14, 521–542, 2021
https://doi.org/10.5194/gmd-14-521-2021
Geosci. Model Dev., 14, 521–542, 2021
https://doi.org/10.5194/gmd-14-521-2021

Model description paper 27 Jan 2021

Model description paper | 27 Jan 2021

Numerical model to simulate long-term soil organic carbon and ground ice budget with permafrost and ice sheets (SOC-ICE-v1.0)

Kazuyuki Saito et al.

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Cited articles

Alley, R. A., Brook, E. J., and Anandakrishnan, S.: A northern lead in the orbital band: north–south phasing of Ice-Age events, Quaternary Sci. Rev., 21, 431–441, 2002. 
AMAP: Snow, Water, Ice and Permafrost in the Arctic (SWIPA): Climate Change and the Cryosphere, Arctic Monitoring and Assessment Programme (AMAP), Oslo, Norway, 2011. 
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Argus, D. F., Peltier, W. R., Drummond, R., and Moore, A. W.: The Antarctica component of postglacial rebound model ICE-6G_C (VM5a) based upon GPS positioning, exposure age dating of ice thicknesses, and relative sea level histories, Geophys. J. Int., 198, 537–563, https://doi.org/10.1093/gji/ggu140, 2014. 
Beilman, D. W., MacDonald, G. M., Smith, L. C., and Reimer, P. J.: Carbon accumulation in peatlands of West Siberia over the last 2000 years, Global Biogeochem. Cy., 23, GB1012, https://doi.org/10.1029/2007GB003112, 2009. 
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Short summary
Soil organic carbon (SOC) and ground ice (ICE) are essential but under-documented information to assess the circum-Arctic permafrost degradation impacts. A simple numerical model of essential SOC and ICE dynamics, developed and integrated north of 50° N for 125,000 years since the last interglacial, reconstructed the history and 1° distribution of SOC and ICE consistent with current knowledge, together with successful demonstration of climatic and topographical controls on SOC evolution.