UNIVERSI
TÄ
TS-
BIBLIOTHEK
P
ADERBORN
Anmelden
Menü
Menü
Start
Hilfe
Blog
Weitere Dienste
Neuerwerbungslisten
Fachsystematik Bücher
Erwerbungsvorschlag
Bestellung aus dem Magazin
Fernleihe
Einstellungen
Sprache
Deutsch
Deutsch
Englisch
Farbschema
Hell
Dunkel
Automatisch
Sie befinden Sich nicht im Netzwerk der Universität Paderborn. Der Zugriff auf elektronische Ressourcen ist
gegebenenfalls
nur via VPN oder Shibboleth (DFN-AAI) möglich.
mehr Informationen...
Universitätsbibliothek
Katalog
Suche
Details
Zur Ergebnisliste
Datensatz exportieren als...
BibTeX
Rapid decrease of mass balance observed in the Xiao (Lesser) Dongkemadi Glacier, in the central Tibetan Plateau
Hydrological processes, 2008-07, Vol.22 (16), p.2953-2958
Pu, Jianchen
Yao, Tandong
Yang, Meixue
Tian, Lide
Wang, Ninlian
Ageta, Yutaka
Fujita, Koji
2008
Details
Autor(en) / Beteiligte
Pu, Jianchen
Yao, Tandong
Yang, Meixue
Tian, Lide
Wang, Ninlian
Ageta, Yutaka
Fujita, Koji
Titel
Rapid decrease of mass balance observed in the Xiao (Lesser) Dongkemadi Glacier, in the central Tibetan Plateau
Ist Teil von
Hydrological processes, 2008-07, Vol.22 (16), p.2953-2958
Ort / Verlag
Chichester, UK: John Wiley & Sons, Ltd
Erscheinungsjahr
2008
Link zum Volltext
Quelle
Wiley Online Library Journals Frontfile Complete
Beschreibungen/Notizen
The mass balance of the Xiao (Lesser) Dongkemadi Glacier located in the Tanggula Mountains, of the central Qinghai-Tibetan Plateau has been monitored since 1989. The results show that the mass balance of the glacier has recently shown a deficit trend, and that the glacial terminus was also retreating. Positive mass balance of the glacier was dominant during the period 1989-1993, and the accumulated mass balance reached 970 mm. However, negative mass balance of the glacier has occurred since 1994, except for the large positive mass balance year 1997. The mass balance was - 701 mm in 1998, an extremely negative glacier mass balance year. The equilibrium line altitude showed a significant increasing trend. The mass balance of the glacier has changed from a significantly positive mass balance to a strongly negative mass balance since 1994. Meteorological data suggest that the rapid decrease in the mass balance is related to summer season warming. Copyright © 2007 John Wiley & Sons, Ltd.
Sprache
Englisch
Identifikatoren
ISSN: 0885-6087
eISSN: 1099-1085
DOI: 10.1002/hyp.6865
Titel-ID: cdi_proquest_miscellaneous_34023426
Format
–
Schlagworte
Earth sciences
,
Earth, ocean, space
,
Exact sciences and technology
,
External geophysics
,
glacier retreat
,
Hydrology
,
Hydrology. Hydrogeology
,
mass balance
,
Snow. Ice. Glaciers
,
Tibetan Plateau
,
Xiao Dongkemadi Glacier
Weiterführende Literatur
Empfehlungen zum selben Thema automatisch vorgeschlagen von
bX