The new database of the Global Terrestrial Network for Permafrost (GTN-P)

Abstract. The Global Terrestrial Network for Permafrost (GTN-P) provides the first dynamic database associated with the Thermal State of Permafrost (TSP) and the Circumpolar Active Layer Monitoring (CALM) programs, which extensively collect permafrost temperature and active layer thickness (ALT) data from Arctic, Antarctic and mountain permafrost regions. The purpose of GTN-P is to establish an early warning system for the consequences of climate change in permafrost regions and to provide standardized thermal permafrost data to global models. In this paper we introduce the GTN-P database and perform statistical analysis of the GTN-P metadata to identify and quantify the spatial gaps in the site distribution in relation to climate-effective environmental parameters. We describe the concept and structure of the data management system in regard to user operability, data transfer and data policy. We outline data sources and data processing including quality control strategies based on national correspondents. Assessment of the metadata and data quality reveals 63 % metadata completeness at active layer sites and 50 % metadata completeness for boreholes. Voronoi tessellation analysis on the spatial sample distribution of boreholes and active layer measurement sites quantifies the distribution inhomogeneity and provides a potential method to locate additional permafrost research sites by improving the representativeness of thermal monitoring across areas underlain by permafrost. The depth distribution of the boreholes reveals that 73 % are shallower than 25 m and 27 % are deeper, reaching a maximum of 1 km depth. Comparison of the GTN-P site distribution with permafrost zones, soil organic carbon contents and vegetation types exhibits different local to regional monitoring situations, which are illustrated with maps. Preferential slope orientation at the sites most likely causes a bias in the temperature monitoring and should be taken into account when using the data for global models. The distribution of GTN-P sites within zones of projected temperature change show a high representation of areas with smaller expected temperature rise but a lower number of sites within Arctic areas where climate models project extreme temperature increase. GTN-P metadata used in this paper are available at doi: 10.1594/PANGAEA.842821 .

[1]  K. Schaefer,et al.  The impact of the permafrost carbon feedback on global climate , 2014 .

[2]  Juergen Kurths,et al.  On the influence of spatial sampling on climate networks , 2014 .

[3]  V. Brovkin,et al.  Expert assessment of vulnerability of permafrost carbon to climate change , 2013, Climatic Change.

[4]  Charles D. Koven,et al.  Analysis of Permafrost Thermal Dynamics and Response to Climate Change in the CMIP5 Earth System Models , 2013 .

[5]  Richard W. Allmendinger,et al.  Spherical projections with OSXStereonet , 2013, Comput. Geosci..

[6]  D. Lawrence,et al.  Diagnosing Present and Future Permafrost from Climate Models , 2012 .

[7]  J. Canadell,et al.  The Northern Circumpolar Soil Carbon Database: spatially distributed datasets of soil coverage and soil carbon storage in the northern permafrost regions , 2012 .

[8]  Annett Bartsch,et al.  The ESA DUE Permafrost project - A service for high latitude research , 2012, 2012 IEEE International Geoscience and Remote Sensing Symposium.

[9]  B. Biskaborn,et al.  Environmental variability in northeastern Siberia during the last ~13,300 yr inferred from lake diatoms and sediment-geochemical parameters , 2012 .

[10]  Guido Grosse,et al.  Vulnerability and feedbacks of permafrost to climate change , 2011 .

[11]  H. Christiansen,et al.  NORPERM, the Norwegian Permafrost Database – a TSP NORWAY IPY legacy , 2010 .

[12]  Jerry Brown Report from the international permafrost association: the IPY permafrost legacy , 2010 .

[13]  L. H. Blikra,et al.  The thermal state of permafrost in the nordic area during the international polar year 2007–2009 , 2010 .

[14]  Vladimir E. Romanovsky,et al.  Thermal state of permafrost in Russia , 2010 .

[15]  Vladimir E. Romanovsky,et al.  Permafrost thermal state in the polar Northern Hemisphere during the international polar year 2007–2009: a synthesis , 2010 .

[16]  Miguel Ramos,et al.  Thermal state of permafrost and active‐layer monitoring in the antarctic: Advances during the international polar year 2007–2009 , 2010 .

[17]  Lin Zhao,et al.  Thermal state of permafrost and active layer in Central Asia during the international polar year , 2010 .

[18]  P. Groisman,et al.  Ongoing climatic change in Northern Eurasia: justification for expedient research , 2009 .

[19]  Donald A. Walker,et al.  The Circumpolar Arctic vegetation map , 2005 .

[20]  F. Nelson,et al.  The circumpolar active layer monitoring (calm) program: Research designs and initial results , 2000 .

[21]  H. French The Periglacial Environment , 1977 .

[22]  Dario Papale,et al.  Database Maintenance, Data Sharing Policy, Collaboration , 2012 .

[23]  Kenji Yoshikawa,et al.  (www.interscience.wiley.com) DOI: 10.1002/ppp.690 Thermal State of Permafrost in North America: A Contribution to the International Polar Year , 2022 .