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A new method to determine the upper boundary condition for a permafrost thermal model : an example from the Qinghai-Tibet Plateau

Author
ZHANG, M1 2 ; MIN, K.-H2 3 ; WU, Q1 ; ZHANG, J1 ; HARBOR, J2
[1] State Key Lab. of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Inst., Chinese Academy of Sciences, Lanzhou, China
[2] Dept. of Earth, Atmospheric, and Planetary Science, Purdue Univ., Lafayette, United States
[3] Center for Atmospheric Remote Sensing, Kyungpook National Univ., Daegu, Korea, Republic of
Source

Permafrost and periglacial processes. 2012, Vol 23, Num 4, pp 301-311, 11 p ; ref : 1 p

CODEN
PEPPED
ISSN
1045-6740
Publisher
Wiley, Chichester
Publication country
United Kingdom
Document type
Article
Language
English
Keyword (fr)
Analyse de régression Changement climatique Climat régional Haute montagne Infrastructure Modèle Pergélisol Plateau Périglaciaire Régime thermique Température de l'air Température du sol Utilisation du sol Zone froide Chine Qinghai Tibet
Keyword (en)
Regression analysis Climatic change Regional climate High mountain Infrastructure Model Permafrost Plateau Periglacial features Thermal regime Air temperature Soil temperature Land use Cold area China Qinghai Tibet
Keyword (es)
Análisis de regresión Cambio climático Clima regional Alta montaña Infraestructura Modelo Pergelisol Meseta Periglaciar Régimen térmico Temperatura del aire Temperatura del suelo Aprovechamiento del suelo Zona fría China Tsinghai Tibet
Classification
Francis
531 Bgi / Prodig / 531-327 Asia / 531-333 China / 531-334 Physical geography

Discipline
Geography
Origin
PRODIG
Database
FRANCIS
INIST identifier
27865246

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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