Planning activities for the Ninth International Conference on Permafrost (NICOP) included the review of 625 abstracts and over 400 manuscripts. A meeting of an international review team met at the U.S. Geological Survey, Menlo Park, California, in December 2007.


In addition to paper and poster sessions, a series of 20 plenary presentations will cover topics on Alaskan permafrost, global thermal state of permafrost, engineering challenges, hydrologic and terrestrial processes, and polar and alpine periglacial processes. See for late-breaking conference news and field trip registration. The U.S. Permafrost Association (), with over 200 individual and corporate members, is providing the administrative support for NICOP. The USPA Board and members meet annually at the AGU in San Francisco to elect new officers and conduct the Association’s other business.

The 2007 Fall Meeting of the American Geophysical Union was held in San Francisco, California, December 10–14, 2007. There were 392 abstracts presented in 29 Cryosphere sessions, as well as 14 IPY presentations in two Union sessions and a number of permafrost and carbon abstracts in Biogeosciences. Reports and posters covered cold region hydrology, surface and subsurface processes including permafrost, seasonally frozen ground, interactions between snow cover and soil, as well as periglacial processes. The IPY sessions covered progress in high latitude research. The focus on seasonal frozen ground and permafrost at AGU continues to expand as indicated by the interdisciplinary nature of presentations at the 2007 AGU Fall Meeting.

The 2007 Annual Meeting of the Association of American Geographers was held April 17–21 in San Francisco. The AAG’s Cryosphere Specialty Group (CrSG) sponsored 18 paper sessions on topics including periglacial processes, glaciology, snow science, the effects of climate change on cryospheric environments, and human adaptation in polar regions. The CrSG made two awards for 2007: the F. E. Matthes Award was presented to R. G. Barry (University of Colorado, NSIDC) in recognition of a half-century of contributions to cryospheric science. D. Streletskiy (University of Delaware) received the R. S. Tarr Award for best student paper, titled Monitoring frost heave and thaw subsidence in northern Alaska with differential GPS with coauthors J. Little, N. Shiklomanov, and F. Nelson.

A symposium entitled ‘Permafrost on a Warming Planet’ was organized by J. Brown at the 58th AAAS Arctic Science Conference held in Anchorage, Alaska, September 24–26, 2007. Seven reports were presented on topics of state and fate of permafrost, thermokarst in Alaska, methane emission from lakes, retrogressive thaw slumps, patterned ground distribution, subsea permafrost, and carbon storage in soils. T. Krzewinski, chair of the Technical Council on Cold Regions Engineering (TCCRE) of the American Society of Civil Engineers (ASCE) reported the following:

On October 3, 2007, the University of Colorado’s National Snow and Ice Data Center hosted former U.S. Vice President Al Gore for a private science briefing at the request of Mr. Gore (see photo). After brief presentations by NSIDC scientists concerning the latest research on Arctic sea ice, snow, glaciers, permafrost, and ice sheets, an extensive discussion ensued. Mr. Gore expressed particular interest in climate interactions and changes occurring in our planet’s cold regions, including changes in permafrost.

At the University of Colorado’s National Snow and Ice Data Center (NSIDC) O.W. Frauenfeld, together with T. Zhang and M.C. Serreze, are investigating the interactions between synoptic-scale atmospheric circulation variability and the soil thermal regime (soil temperatures, active layer thickness, and seasonal freeze depths) in the Russian Arctic. This NSF funded project provides a synthesis of observational surface-atmosphere interactions in the high latitudes of Eurasia over the last ~70 years. Feedbacks from the soil thermal regime to the overlying atmosphere are also investigated, using both statistical and modeling approaches.

R. Sletten, University of Washington, reports that a special seminar on periglacial processes is planned in honor of Link and Tahoe Washburn at the Quaternary Research Center, February 2008. The NSF-funded Greenland biocomplexity project is completed; however, data logging instrumentation for active layer thermal characteristics, soil creep monitoring, and microclimate is being maintained. A new NSF project focuses on ground ice in Antarctica (R. Sletten, B. Hagedorn, B. Hallet). Two new meteorological stations will be established and permafrost cores will be collected along a transect from sea level to over 2500 m asl. A collaborative in Taylor Valley, using soils and geomorphology to study the history of the West Antarctic Ice Sheet excursion into the valley. A NASA project on remote sensing to study snow cover using microwave, visible spectra, and thermal properties complements the Dry Valley ground ice study (D. Winebrenner, R. Sletten, B. Hallet, J. Putkonen, B. Hagedorn). For further information and research updates visit (

F. Nelson and N. Shiklomanov (University of Delaware Permafrost Group, UDPG) report that the CALM sites in northern Alaska were visited by A. Klene, University of Montana, C. Seybold, U.S. Natural Resources Conservation Service (NRCS), and UD grad students D. Streletskiy, Melanie Schimek, and R. Ippolito. N. Shiklomanov and A. Klene, with students Streletskyi and Wallace (UM), participated in an international permafrost field course in Russia (see Other News). We continued our work with J. Doolittle (NRCS) on applications of three-dimensional ground-penetrating radar (GPR) images of the active layer and shallow permafrost (see Permafrost and Periglacial Processes 18(4)). Doolittle has been working closely with UD graduate student Mark Demitroff on applications of 3D GPR imaging for resolving networks of fossil cryogenic sediment-filled wedges in southern New Jersey. With T. Zhang (NSIDC) and S. Gruber (University of Zurich), F. Nelson was guest editor of a collection of permafrost papers in Journal of Geophysical Research—Earth Surface (2007, 112(F2)). The second International CALM Workshop is being planned, to be held in Barrow in late June 2008. H. French and F. Nelson have completed editing a “lost” book manuscript from the early 1960s written by legendary permafrost scientist Siemon W. Muller (Stanford University). The volume, of great historical interest, is planned to be available at NICOP.

W. Eisner, K. Hinkel, C. Cuomo, and colleagues (K. Peterson, E. Maurer, R. Beck, J. Bockheim, and B. Jones) are continuing a multidisciplinary study of landscape processes on the Arctic Coastal Plain, focusing on the thousands of thaw lakes of northern Alaska. A recent article in JGR-Earth Surface described the comparison of Landsat-1 (MSS) imagery from the mid-1970s to Landsat-7 ETM+ imagery from around 2000; 50 lakes completely or partially drained over the 25-year period which indicates landscape stability. The lake-specific drainage mechanism can be inferred in some cases, but efforts to understand landscape processes and identify drainage events have been enhanced by interviewing Iñupiaq elders and others practicing traditional subsistence lifestyles.

V. Romanovsky and the University of Alaska Fairbanks permafrost group at the Geophysical Institute/ International Arctic Research Center (K. Yoshikawa, S. Marchenko, D. Nicolsky, R. Daanen, G. Grosse, and A. Kholodov) continue to work on permafrost and active layer dynamics in Alaska, the instrumentation of boreholes and acquisition of subsurface temperatures from circum-arctic permafrost regions (IPY TSP project), and modeling permafrost in Alaska, Siberia, and Greenland. Under the NSF-sponsored Russia- United States TSP project, coordinated by A. Kholodov, a network of boreholes was instrumented for long-term temperature observation in the Russian Arctic (48 boreholes in 2006, 50 more in 2007). Observations in the 60+ existing Alaskan permafrost observatories continued. S. Marchenko continued research in the Northern Tien Shan Mountains, Kazakhstan, and with Ghent University (Belgium) and Gorno-Altaisk State University (Russia) in the Altai Mountains, Russia. G. Grosse’s fieldwork in the Kobuk Valley National Park (with NPS Alaska), Yakutsk (with K. Yoshikawa), and in Cherskii (with S. Zimov, Northeast Science Station Cherskii) focuses on thermokarst lake dynamics and landscape processes employing GIS and multi-temporal remote sensing. Grosse is maintaining and developing the Permafrost Young Researchers Network Thesis Bibliography. R. Daanen is collaborating with Danish permafrost researchers at the Technical University of Denmark, Greenlandic permafrost researchers (ASIAQ), and the Danish Meteorological Institute on modeling the Greenland permafrost history using high resolution climate simulations. Field and laboratory studies in Alaska were performed to understand the effects of differential insulation on soil freezing processes and especially on soil movement due to differential ice accumulation.

K. Yoshikawa and T. Saito, University of Alaska Fairbanks, have visited 35 native village schools to install shallow (to 6 m depth) permafrost cables and active layer frost tubes. The stations are adjacent to schools in Alaska and several other countries. Monitoring permafrost temperature and seasonal thaw provides students the opportunity to collect, analyze, and share data. In spring 2007, they visited 12 villages along the Yukon River by snow machines, bringing a light-weight rotary percussion drill. All data are shared online: . This outreach project is supported by the University of Alaska’s EPSCoR, NASA, and NSF IPY (TSP) programs.

In support of the TSP project, G. Clow and F. Urban (U.S. Geological Survey) re-measured temperatures in nearly all the deep boreholes in northwestern Alaska. The remaining wells, located in the foothills of the Brooks Range, will be relogged during 2008. The DOI/GTN-P active-layer network was serviced, and a number of improvements were made to the radio telemetry system in the eastern portion of the U.S. National Petroleum Reserve (NPR-A) and in the Arctic National Wildlife Refuge (ANWR). High-resolution dynamical downscaling experiments were initiated using the Weather Research & Forecasting Model (WRF) for federal lands in northern Alaska.

K. Bjella (CRREL Hanover) reports that modifications to the cooling system in the Permafrost Tunnel in Fox, Alaska, are underway. Outdoor air was brought in starting in early February. The forced circulation lowered permafrost temperatures to -4.5 to -3.5°C, depending on the season, which subsequently slowed the creep rate by a factor of three. This will help insure the continued use of the facility for research and outreach into the foreseeable future.

T. Douglas (CRREL Fairbanks) reports that at the Farmer’s Loop permafrost research site near Fairbanks, Alaska, a 3-m borehole was drilled in the late spring of 2007 and 10 thermistors, provided by V. Romanovsky, were installed. A meteorological tower (provided by C. Collins) and a series of snow depth and temperature probes (provided by M. Sturm) were also installed at the site as part of the CALM network. In August 2007 a group lead by K. Yoshikawa and Y. Shur measured electrical resistivity along three lines in the two previously disturbed plots adjacent to the CALM site which was probed again in October. J. Bockheim, University of Wisconsin, continues to work with the New Zealand Antarctic Programme and will spend the austral summer in the Darwin Glacier region.

By using high-resolved simulated soil temperature data (10500 values) N. Mölders and D. P. Mazumder (University of Alaska, Fairbanks) theoretically examined how network density and design affect regional averages of soil temperatures. Permafrost networks that have sites non-randomly distributed may overestimate regional soil temperatures compared to the regional soil temperature determined from all data. Network density also plays a role. Networks with 400 or more sites will capture the regional average and trends well, if they are randomly distributed over the entire region.

Z. Yang, H. Liu, and U. Dutta from the School of Engineering, University of Alaska Anchorage, continued research of seasonally frozen ground effects on the engineering structures in cold regions. With the support of two grants from the Advanced National Seismic System of U.S. Geological Survey, they recently completed instrumentation of a bridge and a high-rise RC-type building in Anchorage, Alaska. State-of-the-art seismic sensors and data acquisition systems were installed in the spring 2007 for collecting building performance data during seismic events. Together with K. Hazirbaba of UAF, they have successfully obtained support from the Alaska University Transportation Center and Alaska DOT & PF to study the effects of permafrost and seasonally frozen ground on the seismic input to infrastructures.

N. and B. Shumaker, BeadedStream, announced a new ultra-rugged portable (handheld) data collector for its temperature acquisition cables (TACs). The TACs are being used throughout Alaska for tundra access studies, refrigerated foundation systems, monitoring permafrost temperatures, and for geotechnical engineering projects, among other applications. The all-digital TACs provide options for Internet access.

Finally, we congratulate J. C. F. Tedrow, Rutgers University, on the celebration of his 90th birthday (April 21, 2007), and we recognize his many past and continuing contributions to polar soil science.

Lynn Everett ( and Oliver W. Frauenfeld (