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Consequences of permafrost degradation for Arctic infrastructure - Bridging the model gap between regional and engineering scales [期刊论文]
Cryosphere, 2021-01-01, 15 (5
Schneider Von Deimling T.;  Lee H.;  Ingeman-Nielsen T.;  Westermann S.;  Romanovsky V.;  Lamoureux S.;  Walker D.A.;  Chadburn S.;  Trochim E.;  Cai L.;  Nitzbon J.;  Jacobi S.;  Langer M.
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Soil respiration of alpine meadow is controlled by freeze-Thaw processes of active layer in the permafrost region of the Qinghai-Tibet Plateau [期刊论文]
Cryosphere, 2020-01-01, 14 (9
Wang J.;  Wu Q.;  Yuan Z.;  Kang H.
View/Download:4/0
 
ADAPTATIONAN IMPORTANT TECHNOLOGY IN THE DEVELOPMENT OF RUSSIA'S SUBARCTIC TERRITORIES [期刊论文]
HERALD OF THE RUSSIAN ACADEMY OF SCIENCES, 2019-01-01, 89 (1) : 65-71
Osipov, V., I;  Aksyutin, O. E.;  Ishkov, A. G.;  Grachev, V. A.;  Sergeev, D. O.
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Resolution capacity of geophysical monitoring regarding permafrost degradation induced by hydrological processes [期刊论文]
Cryosphere, 2017-01-01, 11 (6
Mewes B;  , Hilbich C;  , Delaloye R;  , Hauck C
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疏勒河上游不同退化类型冻土可培养细菌数量变化 [期刊论文]
生态学杂志, 2017-01-01, 36 (10) : 4088-4098
张宝贵;  刘晓娇;  刘敏;  章高森;  张威;  伍修锟;  陈拓;  刘光琇
View/Download:4/0
 
Importance of soil thermal regime in terrestrial ecosystem carbon dynamics in the circumpolar north [期刊论文]
Global and Planetary Change, 2016-01-01, 142
Jiang Y.;  Zhuang Q.;  Sitch S.;  O'Donnell J.A.;  Kicklighter D.;  Sokolov A.;  Melillo J.
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Weichselian permafrost depth in the Netherlands: A comprehensive uncertainty and sensitivity analysis [期刊论文]
Cryosphere, 2016-01-01, 10 (6
Govaerts J;  , Beerten K;  , Ten Veen J
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Comparison of effects of cold-region soil/snow processes and the uncertainties from model forcing data on permafrost physical characteristics [期刊论文]
Journal of Advances in Modeling Earth Systems, 2016-01-01, 8 (1
Barman R;  , Jain A;  K
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Riparian shrub expansion: Linkages to permafrost, hydrology and soil microbes [项目]
Anna Liljedahl
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青藏铁路沿线多年冻土区气温和多年冻土变化特征 [期刊论文]
岩石力学与工程学报, 2016-01-01, 35 (7) : 2647-2652
蔡汉成;  李勇;  杨永鹏;  唐彩梅;  程丽彬;  刘锟
View/Download:4/0
 

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