Articles | Volume 13, issue 8
The Cryosphere, 13, 2087–2110, 2019
The Cryosphere, 13, 2087–2110, 2019
Research article
01 Aug 2019
Research article | 01 Aug 2019

Permafrost variability over the Northern Hemisphere based on the MERRA-2 reanalysis

Jing Tao et al.

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Cited articles

Alexeev, V. A., Nicolsky, D. J., Romanovsky, V. E., and Lawrence, D. M.: An evaluation of deep soil configurations in the CLM3 for improved representation of permafrost, Geophys. Res. Lett., 34, L09502,, 2007. 
Anisimov, O. A. and Reneva, S.: Permafrost and changing climate: The Russian perspective, Ambio, 35, 169–175,[169:Pacctr]2.0.Co;2, 2006. 
Anisimov, O. A.: Potential feedback of thawing permafrost to the global climate system through methane emission, Environ. Res. Lett., 2, 045016,, 2007. 
Anisimov, O. A., Lobanov, V. A., Reneva, S. A., Shiklomanov, N. I., Zhang, T., and Nelson, F. E.: Uncertainties in gridded air temperature fields and effects on predictive active layer modeling, J. Geophys. Res.-Earth, 112, F02S14,, 2007. 
Barman, R. and Jain, A. K.: Comparison of effects of cold-region soil/snow processes and the uncertainties from model forcing data on permafrost physical characteristics, J. Adv. Model. Earth Sy., 8, 453–466, 2016. 
Short summary
The active layer thickness (ALT) in middle-to-high northern latitudes from 1980 to 2017 was produced at 81 km2 resolution by a global land surface model (NASA's CLSM) with forcing fields from a reanalysis data set, MERRA-2. The simulated permafrost distribution and ALTs agree reasonably well with an observation-based map and in situ measurements, respectively. The accumulated above-freezing air temperature and maximum snow water equivalent explain most of the year-to-year variability of ALT.