Analyzing glacier retreat and mass balances using aerial and UAV photogrammetry in the Ötztal Alps, Austria

• Published in: The cryosphere 2021-08, Vol.15 (8), p.3699-3717
• Main Authors: Geissler, Joschka, Mayer, Christoph, Jubanski, Juilson, Münzer, Ulrich, Siegert, Florian
• Format: Article
• Language: English
• Subjects: Ablation; Aerial photography; Aerial surveys; Altitude; Analysis; Climate change; Climatic analysis; Crevasses; Datasets; Digital imaging; Drone aircraft; Geodetic surveys; Glacial drift; Glacier retreat; Glaciers; Glaciological data; High resolution; Ice; Ice cover; Image acquisition; Image resolution; Imagery; Mass; Mass balance; Methods; Photogrammetry; Resolution; Spatial discrimination; Spatial resolution; Surveying; Surveys; Unmanned aerial vehicles
• ISSN: 1994-0424; 1994-0416; 1994-0424; 1994-0416
• DOI: 10.5194/tc-15-3699-2021

We use high-resolution aerial photogrammetry to investigate glacier retreat in great spatial and temporal detail in the Ötztal Alps, a heavily glacierized area in Austria. Long-term in situ glaciological observations are available for this region as well as a multitemporal time series of digital aerial images with a spatial resolution of 0.2 m acquired over a period of 9 years. Digital surface models (DSMs) are generated for the years 2009, 2015, and 2018. Using these, glacier retreat, extent, and surface elevation changes of all 23 glaciers in the region, including the Vernagtferner, are analyzed. Due to different acquisition dates of the large-scale photogrammetric surveys and the glaciological data, a correction is successfully applied using a designated unmanned aerial vehicle (UAV) survey across a major part of the Vernagtferner. The correction allows a comparison of the mass balances from geodetic and glaciological techniques – both quantitatively and spatially. The results show a clear increase in glacier mass loss for all glaciers in the region, including the Vernagtferner, over the last decade. Local deviations and processes, such as the influence of debris cover, crevasses, and ice dynamics on the mass balance of the Vernagtferner, are quantified. Since those local processes are not captured with the glaciological method, they underline the benefits of complementary geodetic surveying. The availability of high-resolution multi-temporal digital aerial imagery for most of the glaciers in the Alps provides opportunities for a more comprehensive and detailed analysis of climate-change-induced glacier retreat and mass loss.