Permafrost

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Guo Jian-wen -------177 Guo Jian-Wen -----------190 Guo Yong-fu -------------72 Gureva O M ------------86 Guryanov I E --------30 Haeberli W -----------10 Hagedorn B ------------138 Haizhou M -----------------142 Hallam C A -----------175 Hallet B ----------131, 138 Han U --------201 Han Xu-jun ----------204 Hananov V V ----------------58 Harada K ----------------148, 171 Harbor J ------------142 Haritashya U ------94, 106 Harris S A ---------106 Hatano R. -----------111,113 Hättestrand C -----------------142 He Ping –43, 55 He Rui-xia ---------172 Heggem, E S F ---------194 Helm C W---------211 Herzschuh U ---------120 Heyman J -------------142 Hiemstra C A--------170 Hintzman L D -----------3, 148 Hofstee E H --------------146 Hou Zhong-jie Hou -----25 Hu Ming-jian ---40 Hu Z---------205 Huang Ming-kui ---40 Huang S ----53, 37 Huang Shi-jing ----------20 Hubberten H- W -----------6 Humlum O ------------171 Huo Xiao-hu -------------157 Ikeda A -----------159, 199 Iospa A V -----------11 Isaev V S --------101 Isaksen K -------------171 Ishi T --------------159, 199
Ishikawa H ---------151, 171, 181, 205. 207 Istratov V A-------------155 Iudin M M---39 Ivanova N V ----21 Ivanova R N ------------102 Iwahana G --------113, 116, 171, 179 Jackie A --------------------------146 Jakovlev A O ----44 Jambaljav Ya -----------------163, 206 Jeong S ---------201 Ji Yan-jun --------172 Ji Zhi-qiang ----------17, 77 Jiang F Q --------22 Jin Hui-jun ---------129, 131, 157, 172 Jin Rui -------------191, 204 Kadota T-------151, 207 Kamalov A M ------42 Kane D L---------------3 Kang Jia-mei ------28, 43 Kanie S ----53, 54 Katamura F ----------99 Katayanagi N -----------111 Kaverin D ---------------169 Khomenko I -----------124 Kim K ------37, 53 Kimoto M ----------180 Kistanov O G -----------11 Klene A E ----------165 Klinova G I -----------11 Koike T --------205 Kolesnikov A B--------------107 Komarov I A ------------87, 101 Kömle N I ------43 Konchenko L A ------------168 Kondratiev V G -----------------57, 58, 59, 60 Konstantinov P -----------116, 135 Koroteev A --------------80 Kraev G-------------126 Kramer A ---------120 Krivov D N -----------11, 96 Kuchmin A -----------------155
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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
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Mountain permafrost study in the Ru
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Permafrost Distribution and Thickne
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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 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 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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