Abstract
A conceptual precipitation–runoff model was applied in five glacierized catchments in Central Asia. The model, which was first developed and applied in the Alps, works on a daily time step and yields good results in the more continental climate of the Tien Shan mountains for present-day climate conditions. Runoff scenarios for different climates (doubling of CO2) and glacierization conditions predict an increased flood risk as a first stage and a more complex picture after a complete glacier loss: a higher discharge during spring due to an earlier and more intense snowmelt is followed by a water deficiency in hot and dry summer periods. This unfavourable seasonal redistribution of the water supply has dramatic consequences for the Central Asian lowlands, which depend to a high degree on the glacier melt water for irrigation and already nowadays suffer from water shortages.
Dokumententyp: | Zeitschriftenartikel |
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Keywords: | Central Asia; climate change; glacier hydrology; runoff modelling |
Fakultät: | Geowissenschaften > Department für Geographie > Geographie und Landschaftsökologie |
Themengebiete: | 900 Geschichte und Geografie > 910 Geografie, Reisen |
URN: | urn:nbn:de:bvb:19-epub-13563-6 |
ISSN: | 0029-1277 |
Sprache: | Englisch |
Dokumenten ID: | 13563 |
Datum der Veröffentlichung auf Open Access LMU: | 12. Jul. 2012, 13:47 |
Letzte Änderungen: | 04. Nov. 2020, 12:54 |