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Monitoring glacier elevation and volume changes with digital photogrammetry and GIS at Gepatschferner glacier, Austria / A. Keutterling in International Journal of Remote Sensing IJRS, vol 27 n°18 - 19 - 20 (October 2006)  

Public [article]  inInternational Journal of Remote Sensing IJRS > vol 27 n°18 - 19 - 20 (October 2006) . - pp 4371 - 4380 Titre : Monitoring glacier elevation and volume changes with digital photogrammetry and GIS at Gepatschferner glacier, Austria Type de document : Article/Communication Auteurs : A. Keutterling, Auteur ; A. Thomas, Auteur Année de publication : 2006 Article en page(s) : pp 4371 - 4380 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Applications de télédétection [Termes IGN] analyse diachronique [Termes IGN] couple stéréoscopique [Termes IGN] glacier [Termes IGN] modèle numérique de surface [Termes IGN] photogrammétrie numérique [Termes IGN] surveillance hydrologique [Termes IGN] surveillance météorologique [Termes IGN] système d'information géographique [Termes IGN] Tyrol (Autriche) [Termes IGN] volume (grandeur) Résumé : (Auteur) Digital elevation models of Gepatschferner in Northern Tyrol, Austria were obtained with digital photogrammetry from high altitude stereo photo pairs and by digitizing an analogue topographic glacier map, for 1990 and 1971, respectively. A difference map was calculated to identify regions of glacier elevation increases and decreases corresponding to glacier mass gain and loss. While the glacier tongue below 2600 m showed mainly increases in glacier surface elevation as compared to 1971, the remaining glacier thickness experienced both increases and decreases. The accumulation zone above 3200 m contained several extreme cases of morphological features with altitude changes>+30 m. While the increased ice thickness of the glacier tongue can be traced to a well documented period of mass accumulation in the 1970s, changes in glacier surface elevation in the higher zones may be linked either to the morphology of the glacier bed or to differences in insolation on the glacier surface. Between 1971 and 1990 the glacier experienced a net loss of 26*106 m3 corresponding to approximately 0.9% of the entire glacier volume. Copyright Taylor & Francis Numéro de notice : A2006-465 Affiliation des auteurs : non IGN Thématique : IMAGERIE Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1080/01431160600851819 En ligne : https://doi.org/10.1080/01431160600851819 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=28189 [article]

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