Knowledge Transfer by the Global Terrestrial Network for Permafrost (GTN-P)

Chapter
Part of the SpringerBriefs in Earth System Sciences book series (BRIEFSEARTHSYST)

Abstract

Permafrost ecosystems occupy a quarter of the land surface in the Northern Hemisphere. Ongoing rapid temperature change in these areas causes permafrost warming in the Arctic and thawing in the Subarctic regions (Romanovsky et al. Permafr Periglac Process 21:106–116 2010).

Notes

Acknowledgements

We thank ESKP for providing one year financial support to develop the visualization products of GTN-P Database. We thank Karl Dzuba for assisting with proof-reading the ESKP articles on permafrost research highlights. We also thank Jean-Pierre Lanckman, Malek Kaderi and Anseok Joo (Arctic Portal), and Almut Dressler and Saskia Bacher (AWI) for data management.

References

  1. Biskaborn, B. K., Lanckman, J. P., Lantuit, H., Elger, K., Streletskiy, D. A., Cable, W. L., et al. (2015). The new database of the Global Terrestrial Network for Permafrost (GTN-P). Earth System Science Data, 7, 245–259.CrossRefGoogle Scholar
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  3. Romanovsky, V. E., Smith, S. L., & Christiansen, H. H. (2010). Permafrost thermal state in the polar northern hemisphere during the international polar year 2007–2009: A synthesis. Permafrost and Periglacial Processes, 21, 106–116.  https://doi.org/10.1002/ppp.689.CrossRefGoogle Scholar
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Copyright information

© The Author(s) 2018

Authors and Affiliations

  1. 1.Alfred Wegener Institute Helmholtz Centre for Polar and Marine ResearchPotsdamGermany

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