An attempt to model outflow from the Werenskiold Glacier basin (SW Spitsbergen)

3e Symposium International. Cavités glaciaires et cryokarst en régions polaires et de haute montagne. Actes

Auteur(s) et Affiliation(s)

KRAWCZYK, W-E

Faculty of Earth Science, University of Silesia, Sosnowiec, Pologne

Description :
The lack of data as well as technical problems with water stage recording in Glacier River during polar spring and autumn (river freezing) are the main reasons for attempts to obtain the model of outflow from the Werenskiold Glacier basin. For the spring hydrological season the simple regression Q=f(ta) with hourly discharges and air temperatures was used. The autumn-winter hydrological season was approximated with Maillet's curve.

Type de document :
Congrès

Source :
Symposium International. Cavités glaciaires et cryokarst en régions polaires et de haute montagne, 3, Chamonix, France, 1994-11-01, Cahiers de géographie de Besançon (Les), 1995, n°. 34, p. 55-60, Collation : Illustration, Références bibliographiques : 7 ref.

Date :
1995

Editeur :
Pays édition : France

Langue :
Anglais