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.
| Item Type: | Journal article |
|---|---|
| Keywords: | Central Asia; climate change; glacier hydrology; runoff modelling |
| Faculties: | Geosciences > Department of Geography > Geography and Landscape Ecology |
| Subjects: | 900 History and geography > 910 Geography and travel |
| URN: | urn:nbn:de:bvb:19-epub-13563-6 |
| ISSN: | 0029-1277 |
| Language: | English |
| Item ID: | 13563 |
| Date Deposited: | 12. Jul 2012 13:47 |
| Last Modified: | 04. Nov 2020 12:54 |

