IGB

Connexion

(3ChamonixSymposium International. Cavités glaciaires et cryokarst en régions polaires et de haute montagne en Anglais - 1995)

Document title

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

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

Authors(s) and Affiliation(s)

KRAWCZYK W-E (1) ; LESZKIEWICZ J. ;
(1) Faculty of Earth Science, University of Silesia, Sosnowiec, POLOGNE

Abstract

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(t[a]) with hourly discharges and air temperatures was used. The autumn-winter hydrological season was approximated with Maillet's curve

Source

Congrès

Symposium International. Cavités glaciaires et cryokarst en régions polaires et de haute montagne No3, Chamonix , FRANCE (01/11/1994)

published at : Cahiers de géographie de Besançon (Les)

Editor : FRANCE

Millesime : 1995, no 34 [pp. 55-60]

Bibliographic references : 7 ref.

Language

Anglais

Localisation

Laboratoire INTERGEO - Paris

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1997.
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