Permafrost

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Experimental research on thermal conductivity of undisturbed frozen samples from permafrost regions on Qinghai-Tibetan plateau Theme 2. Frost hazards and periglacial environments in mountain/plateau regions Yosuke Yanai Stimulation of N2O production and reduction in soil under frozen condition Vladimir Chernyad΄ev Hazard assessement criteria for development of engineering geological processes during construction in the area occupied by perennially frozen ground Evgeny Chuvilin Relict gas hydrate as possible form of shallow intra permafrost gas existence Reynald Delaloye Application of ERS InSAR for detecting slope movement in a periglacial mountain environment Fumiaki Takakai CH4 emission from a Siberian alas ecosystem near Yakutsk, Russia Theme 3. Climatic, environmental and cryospheric changes Christine Siegert Cryolithological features of Quaternary sediments on the Lena-Kénkémé interfluve,Central Yakutia Anna Kurchatova Reconstruction of paleocryogenic strata through micromorphological indications Roman Desyatkin About role of thermolarst in global balance of carbon Jakob Heyman Paleoglaciology of the Bayan Har Mountain area, eastern Tibetan Plateau Hui-jun Jin Assessment of frozen soils environmental geological conditions along the Qinghai-Tibet engineering corridor from Xidatan, Qinghai to Naqu, Tibet, China Theme 4. Permafrost hydrology and cold regions water resources and land use Nataliya Moskalenko Cryospheric changes in the West Siberia northern taiga Koichiro Harada Permafrost condition after tundra fire in Seward Peninsula, Alaska Baozhong Liu Impacts of an Arctic reservoir’s regulation on downstream thermal regime in open-water Season 15
16 Christopher Warren Helm Developing an Online GIS repository for permafrost data Oliver W. Frauenfeld Permafrost Young Researchers Network (PYRN): An international effort to encourage the involvement of young researchers for the International Polar Year (2007–2008) M.Gude The international geographical union (IGU) commission on “Cold Region Environments” within the context of changing land use effects in northern permafrost areas Theme 5. Monitoring, mapping and modeling of mountain and high-elevation permafrost Atsushi Ikeda Sounding permafrost in the source area of the Yellow River (Northeastern Tibet): degrading or already disappeared? Uk Han Characteristics and significance of the active layer in permafrost affected soils (Dasan Station, Svalbard and Sejong Station, Antarctica) Petru Urdea Patterned ground and permafrost in the southern carpathians (Romania) Inga Shamanova Main features of soil seasonal freezing and thawing in the Timan – Pechora Oil – and –Gas Province Oleg Streletskiy 1. Structure and physical state of the permafrost in western coastal planes of Russian Arctic 2. Thermophisycal characteristics of dispersion soils in a wide range of negative temperatures Nella Shpolyanskaya Specific features of distribution of the perennially and seasonally frozen ground in Transbaikalia Sharkhuu Natsagdorj Mapping of mountain permafrost in Mongolia and Central Asia Kyung Ho Chung Characteristics and significance of the active layer in permafrost affected soils (Dasan Station, Svalbard and Sejong Station, Antarctica) Kazuyuki Saito Change in hydro-thermal regimes in the soil-freezing regions in the Global Warming simulation by a CGCM of moderate- and high-resolution Zhi-wu Zhu The physical mechanism in freezing processes of soil and the constitutive model of frozen soil Jian-wen Guo Mixed environment developing research on the distributed Qinghai-Tibet Railroad GIS J. G. Bockheim
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SEE AUTHOR INDEX AND REVISED PROGRA
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G.М. Dolgih, Dolgih D.G., Okunev S
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Rev I. Gavriliev The thermal conduc
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Xiao-zu Xu,Bin-xiang Sun,Qi Liu,Shu
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Lopez CML, Katamura F, Argunov R, F
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Grebenets V., Kraev G. Nagornov D.
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V.A. Istratov, A. Kuchmin, A.D. Fro
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Mamoru Ishikawa Mountain permafrost
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ORGANIZING COMMITTEE Co-Chairs Acad
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CO-SPONSORS Chinese Academy of Scie
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curve of the accumulated displaceme
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zone of Tien Shan. Key words: Compl
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negotiations currently under way am
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distribution according to the seaso
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number of freeze-thaw cycles. With
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The Technique of Geoinformation Mod
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Monitoring Study on the Boundary Th
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The Calculation and Control Methods
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observations are presented. Key wor
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frost heave is one typical case of
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whose total water content and poros
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effectively and restrain subgrade d
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Peninsula, Pur and Tar interfluve,
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1-D Numerical Analysis to Predict a
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of the two simulation-analysis meth
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frozen soil. While compared with th
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The maximum vertical deformations a
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dangerous pollutants, including hea
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fact of the rising of artificial pe
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The Thermal Conductivity of Segrega
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discussed in view of geotechnical a
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Numerical modeLling of thawing rail
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experiment for obtaining those para
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lake and in purpose to protect surr
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The Concept of an Engineering-geocr
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Effect of seismic events on the sta
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Electrical Conductivity of Rocks in
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mechanics parameters both in frozen
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influence its temperature change pr
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Experimental and numerical simulati
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signifies that the diffusion action
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Experimental Study on the Influence
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does not spread the energy in the f
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and seismic response of infrastruct
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Cooling effect of crushed rock reve
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The analysis of the data concerning
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the extended duration of freezing p
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Distribution of Rock Glaciers in th
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Methods of Theoretical and Experime
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properties, and is able to move bot
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especially water flooding, could be
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mechanisms during the compression a
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inundations and catastrophic breako
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of quantity of neglected interactio
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Past and present salinization in na
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Temperature Regime of Atmosphere an
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disturbance: conflicting, critical
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Application of ERS InSAR for detect
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critical to melt-water irrigation i
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Features of hydrothermal conditions
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associated with the southwest summe
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Significance of Microtopography and
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Reconstruction of paleocryogenic st
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Dendroclimatic investigations of fo
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anthropogenic disturbance. Despite
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and +38°C in summer. Continuous pe
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asis for palaeolimnological reconst
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eneath a path (34 cm.) In the end o
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can lead to a global ecological cat
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Assessment of Frozen Soils Environm
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No Thawing of the Cold Permafrost H
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Cryospheric changes in the West Sib
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Response of Ice-rich Permafrost to
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About Role of Thermokarst in Global
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presence may be debated since there
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territories have natural and anthro
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will contribute to the resolution o
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Impact of Frozen Ground Change on S
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Antarctica. Key words: Cape Hallett
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The sensitivity of Tibetan Plateau
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infrapermafrost waters that are dis
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Keywords: cryosphere, anthropogenic
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Key words: Alaska, oil exploration,
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Possible Change of Runoff in the Up
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Theme 5. Monitoring, mapping and mo
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Mathematical model for quantitative
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heat transfer model with phase chan
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e.s.l.). In 2005 this mine was equi
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Surface- coupled 3-D Permafrost Mod
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• the territories where the perma
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associated soil surface temperature
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variations in different parts. Keyw
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disturbed landscapes, thaw subsiden
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⎛ ⎜ 1 ⎛ ⎞ ⎜ ε σ = Eε e
Page 190 and 191: Mountain permafrost study in the Ru
Page 192 and 193: Permafrost Distribution and Thickne
Page 194 and 195: Permafrost Distribution and Thickne
Page 196 and 197: studies (Natsagdorj et al. 2000), t
Page 198 and 199: on the basis of determining tempera
Page 200 and 201: models were run using standardized
Page 202 and 203: organized into segments and contact
Page 204 and 205: depends on the microclimate of spec
Page 206 and 207: soundings, borehole temperature mea
Page 208 and 209: In high mountain regions, as well a
Page 210 and 211: ottom at a rate of 4 cm/year and ac
Page 212 and 213: Birch trees (Betula ermanii) are do
Page 214 and 215: Monitoring of the snow cover in the
Page 216 and 217: deterministic model combined with p
Page 218 and 219: We have the map of seasonally froze
Page 220 and 221: approximately with the -5°C mean a
Page 222 and 223: Theme 6. Others Developing an Onlin
Page 224 and 225: The FGDC identifies, archives, docu
Page 226 and 227: Final Revised Program (August 28, 2
Page 228 and 229: Professor Dr. Lin Zhao, CAREERI, CA
Page 230 and 231: Monday, Aug 7, 2006 Location: Ningw
Page 232 and 233: Bending properties monitored in ful
Page 234 and 235: Theme 1-3: Engineering: Frozen grou
Page 236 and 237: Chairs: Bernhard Diekman, Ron Slett
Page 238 and 239: Theme 5-3: Mapping: Permafrost and
Page 242 and 243: A Preliminary Permafrost and Ground
Page 244 and 245: Bulley H----------94 Caffee M W ---
Page 246 and 247: Guo Jian-wen -------177 Guo Jian-We
Page 248 and 249: Kudryavtsev S -------53 Kulish E M
Page 250 and 251: Nefedieva Yu A ----------------87 N
Page 252 and 253: Stauch G -------89 Streletskaya I.
Page 254: Zhang Jian-min --------25 Zhang Jin
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Permafrost

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