Mots-clés
Années 1960-2009 ; Changement climatique ; Chine ; Donnée ; Glacier ; Montagne ; Précipitation ; Recul du glacier ; Température ; Tendance du climat ; Tien ChanChina ; Climatic change ; Climatic trend ; Data ; Glacier ; Glacier retreat ; Mountain ; Precipitation ; Temperature ; Tien ShanCambio climático ; China ; Dato ; Helero ; Montaña ; Precipitación ; Retroceso del glaciar ; Temperatura ; Tendencia del clima ; Tien ShanGlacier area variation and climate change in the Chinese Tianshan Mountains since 1960
Auteur(s) et Affiliation(s)
WANG, S.
College of Geography and Environment Science, Northwest Normal Univ., Lanzhou, Chine
ZHANG, M.
College of Geography and Environment Science, Northwest Normal Univ., Lanzhou, Chine
State Key Lab. of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Inst., CAS, Lanzhou, Chine
LI, Z.
State Key Lab. of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Inst., CAS, Lanzhou, Chine
College of Geography and Environment Science, Northwest Normal Univ., Lanzhou, Chine
WANG, F.
State Key Lab. of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Inst., CAS, Lanzhou, Chine
LI, H.
State Key Lab. of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Inst., CAS, Lanzhou, Chine
LI, Y.
College of Geography and Environment Science, Northwest Normal Univ., Lanzhou, Chine
HUANG, X.
College of Geography and Environment Science, Northwest Normal Univ., Lanzhou, Chine
Description :
Based on the statistics of glacier area variation measured in the Chinese Tianshan Mountains since 1960, the response of glacier area variation to climate change is discussed systematically. According to the 14 meteorological stations in the Chinese Tianshan Mountains, both the temperature and precipitation display a marked increasing tendency from 1960 to 2009. The temperature in the dry seasons (from November to March) increases rapidly but the precipitation grows slowly while the results are inverse in the wet seasons. The annual and seasonal climatic trends accelerate the retreat of glaciers.
Type de document :
Article de périodique
Source :
Journal of geographical sciences. Acta geographica sinica, issn : 1009-637X, 2011, vol. 21, n°. 2, p. 263-273, nombre de pages : 11, Références bibliographiques : 38 ref.
Date :
2011
Editeur :
Pays édition : Chine
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)