ZAMAN, İKLİM VE AKARSU GELİŞİMİ

Autor: J. Vandenberghe, Uğur Doğan, C. Erdem Bekaroğlu
Jazyk: English<br />Turkish
Rok vydání: 2005
Předmět:
Zdroj: Coğrafi Bilimler Dergisi, Vol 3, Iss 2, Pp 69-79 (2005)
Druh dokumentu: article
ISSN: 00000000
1303-5851
1308-9765
63517566
DOI: 10.1501/Cogbil_0000000058
Popis: In the long term (glacial/interglacial sequences), river development follows general climatic evolution. However, at the scale of one cold-warm cycle, it appears that the geomorphological effect of river activity is best expressed at times of climatic change. Such periods of pronounced fluvial action last only a short time. In more detail, the internal evolution in a drainage basin after a climatic event results in a delayed response of the morphology and sedimentation pattern. Finally, on the shortest timescale local thresholds may play a decisive role in the reactions of river systems. It is concluded that the relation between fluvial development and climate is not a simple one, but is fundamentally dependant on the timescale
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