dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel Towards the improvement of model internal consistency using water isotope composition measurements in a glacierized basin
VerfasserIn Zhihua He, Katy Unger-Shayesteh, Sergiy Vorogushyn, Abor Gafurov, Stephan Weise, Olga Kalashnikova, Bruno Merz
Konferenz EGU General Assembly 2017
Medientyp Artikel
Sprache en
Digitales Dokument PDF
Erschienen In: GRA - Volume 19 (2017)
Datensatznummer 250152124
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2017-16924.pdf
 
Zusammenfassung
This study developed an approach to model the water stable isotope composition in streamflow in a glaicerized basin. The spatial variability of water isotope composition in precipitation was simulated in a Rayleigh fractionation procedure using spatial temperature and precipitation. The fractionation and mixing processes of water isotope compositions in various water sources were modeled in a glacio-hydrological model, associated with the simulation of runoff generation processes. Observed water isotope composition in streamflow was additionally used for the calibration of model parameters. The model internal consistency was investigated by the model performance in the reproduction of water isotope compositions in various water sources, as well as the simulation of snow cover area fraction and glacier mass balance. Specific questions addressed are three-fold: 1) How does the proposed approach perform in the reproduction of water isotope compositions in various water sources? 2) Do the water isotope composition measurements help to improve the simulations of snow and glacier melt runoff? (3)What a degree the model internal consistency can be improved aided by the water isotope composition measurements? This study is one of the first attempts to simulate the water stable isotope composition in streamflow in glacierized basins. Our findings could shed lights on the application of water isotope composition measurements for model constraining in glacierized basins.