Permafrost

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Bending properties monitored in full-scale childed gas pipeline experiment in discontinuous permafrost Theme 3-1: Climate and environmental controls of the cryosphere (Location: No.1 Conference-room of Zhongxiaolou Building) Chairs: Jef Vandenberghe, Xiaoping Yang Diekmann, B., Andreev, A.A., Gerasimova, M., Lüpfert, H., Nazarova, L., Pestryakova, L., Popp, S., Siegert, C., Subetto, D.A. Periglacial lake environments in eastern Siberia Xiaoping Yang Ice wedge landforms as indicators for quantitative reconstruction of palaeoclimates in desert regions of China Sergei Marchenko, Vladimir Romanovsky Temporal and spatial changes of permafrost distribution in the Tien Shan Mountains during the Last Millennia Ronald S. Sletten, Birgit Hagedorn, Warren W. Dickinson, Bernard Hallet Origin and stability of ground ice in the Dry Valleys, Antarctica Michelle Koutnik, Ronald S. Sletten, Bernard Hallet, and Shawn Marshall Relationship between permafrost and past ice cover on the Qinghai-Tibet Platea Theme 4-1: <strong>Permafrost</strong> hydrology (Location: Multifunctional-hall of VIP Building) Chairs: Daqing Yang, Oliver Frauenfeld David M. Lawrence Andrew G. Slater Arctic hydrological feedbacks associated with a global climate model projection of severe degradation of near-surface permafrost Daqing Yang, Tingjun Zhang, Baozhong Liu, Baisheng Ye Impact of frozen ground change on stream flow hydrology over the Siberian Lena basin Yong-chao Lan, Zhi Wei*, Hui-jun Jin, Jun-jie Chang, Xiao-hu Huo, Ye-xin Xu Possible change of runoff in the Upper Yellow River Basin under global warming scenarios Erica H. Hofstee, Megan R. Balks * , David I. Campbell, Jackie Aislabie Hydrological characteristics of Seabee Hook, Cape Hallett, Antarctica 10:10–10:30 Coffee Break 10:30–12:10 Oral session Theme 1-2: Engineering: Frozen ground properties and models (Location: Small Hall of North Building) Chairs: Douglas Kane, Wei Ma Norbert I. Kömle, Roman Wawrzaszek, He Ping, Bing Hui, Feng Wenjie Thermal conductivity measurements of road construction material in frozen and unfrozen states 7
S.B.Tataurov, Petrikey A.L. Cryogenic physical and chemical technologies of ore dressing and processing of minerals of natural and technogenic deposits of gold Simon Wang, Osamu Sano Soil insulation by styrofoam extruded polystyrene foam Fujun Niu, Guodong Cheng, Jianjun Li, Wei Ma Monitoring study on the boundary thermal conditions and temperature fields of duct-ventilated embankment in permafrost regions Keli Wang, Guodong Cheng, Hao Jiang, Dayong Wang * Thermodynamic Model of the Ground Surface and Embankment Surface along the Qinghai-Tibet Railway: Results in the Cloud-Free Condition Theme 3-2: Climate and environmental controls of the cryosphere (Location: No.1 Conference-room of Zhongxiaolou Building) Chairs: Hans-W. Hubberten, Thomas Osterkamp Bernd Wuennemann Periglacial and glacial processes in Ladakh, India - Influences on the Holocene history of the Tso Kar lake basin. Max C. Brewer, Huijun Jin No thawing of the cold permafrost has occurred in northern Alaska during the last one-half century Alexander Fedorov, Masami Fukuda, Pavel Konstantinov, Nikolai Bosikov, Go Iwahana Present-day thermokarst development in Central Yakutia R. Shirokov, I. Streletskaya Quaternary sediments of Kara Sea coast and their cryogenic structure Andrey Shmakin Evaluation of permafrost seasonal variations at several Asian sites in 21st century Theme: 4-2: Land use and management (Location: Multifunctional-hall of VIP Building) Chairs:N.C. Doubleday, Arlan Tussing N.C. Doubleday Applying the adaptive cycle to modeling environmental and anthropogenic cryospheric changes and linking problems of human adaptation and mitigation Jan Otto Larsen Sustainability of the transport sector in Norwegain Arctic to climate change Zhaohui Yang Transportion infrastructure on degrading permafrost Anna Kurchatova West Serbia permafrost observatories and educations activities 12:10–14:20 Lunch 14:20–16:00 Oral session 8
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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
Page 182 and 183: associated soil surface temperature
Page 184 and 185: variations in different parts. Keyw
Page 186 and 187: disturbed landscapes, thaw subsiden
Page 188 and 189: ⎛ ⎜ 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 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 240 and 241: Experimental research on thermal co
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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