Abstract
The science on high-mountain proglacial systems is a rather young field of study, but has gained importance since a few years ago. In this context, we investigated a part of the lateral Little Ice Age (LIA) moraine that was built up by the second longest glacier of the Eastern Alps. The Gepatschferner glacier in the Upper Kaunertal, Central Austrian Alps, created up to 150-m-high moraine slopes during its LIA advance that are now prone to paraglacial reworking. To analyse the degree of reworking and to identify the driving forces behind the slope development with both their spatial and temporal variations, we conducted several case studies, mainly based on data acquired by remote sensing techniques (multitemporal TLS and aerial photographs) and their derivatives (DEMs, DoD, orthophotos). First, a medium-term (5 years) overall balance of erosion and deposition of the studied slope is calculated. Second, seasonal variations of the process dynamics are uncovered based on short-term TLS measurements within c. one year. Third, the sediment contributing area (SCA) is delineated to estimate fluvial reworking. Fourth, following paraglacial adjustment studies by Curry et al. (2006), we measured and analysed gully development with time since deglaciation. The case studies lead to the conclusions that paraglacial adjustment of the study slope is still in progress. Extreme events in summer play a dominant role for morphodynamics, followed by processes during winter, whereas springtime offers important preparatory conditions for sediment transport. Fluvial transport is considered to have minor effects on the moraine development compared to gravitational processes. And last but not least, the development of gullies depends more on natural boundary conditions than on time since deglaciation.
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References
Ballantyne CK, Benn DI (1994) Paraglacial slope adjustment and resedimentation following recent glacier retreat, Faabergstolsdalen, Norway. Arct Antarct Alp Res 26:255–269
Ballantyne CK, Benn DI (1996) Paraglacial slope adjustment during recent deglaciation and its implications for slope evolution in formerly glaciated environments. Brooks S, Anderson MG (Eds.) Advances in Hillslope Processes, pp 1173–1195. Wiley, Chichester
Bechet J, Duc J, Loye A, Jaboyedoff M, Mathys N, Malet J-P, Klotz S, Le Bouteiller C, Rudaz B, Travelletti J (2016) Detection of seasonal cycles of erosion processes in a black marl gully from a time series of high-resolution digital elevation models (DEMs). Earth Surf Dynam 4:781–798. https://doi.org/10.5194/esurf-4-781-2016
Becht M (1995) Untersuchungen zur aktuellen Reliefentwicklung in alpinen Einzugsgebieten: Mit 40 Tabellen. Münchener Universitätsschriften, vol 47. Geobuch-Verl., München
Cossart E, Braucher R, Fort M, Bourlès D, Carcaillet J (2008) Slope instability in relation to glacial debuttressing in alpine areas (Upper Durance catchment, southeastern France): evidence from field data and 10Be cosmic ray exposure ages. Geomorphology 95:3–26. https://doi.org/10.1016/j.geomorph.2006.12.022
Curry AM (1999) Paraglacial modification of slope form. Earth Surf Proc Land 24:1213–1228
Curry AM, Cleasby V, Zukowskyj P (2006) Paraglacial response of steep, sediment-mantled slopes to post-Little Ice Age glacier recession in the central Swiss Alps. J Quat Sci 21:211–225. https://doi.org/10.1002/jqs.954
Groß G (1987) Der Flächenverlust der Gletscher in Österreich 1850-1920-1969. Z Gletscherk Glazialgeol 23:131–141
Gude M, Scherer D (1995) Snowmelt and slush torrents: preliminary report from a field campaign in Karkevagge, Swedish Lappland. Geogr Annaler A 77:199–206. https://doi.org/10.2307/521329
Haas F (2008) Fluviale Hangprozesse in Alpinen Einzugsgebieten der Nördlichen Kalkalpen: Quantifizierung und Modellierungsansätze. Dissertation
Haas F, Heckmann T, Becht M, Cyffka B (2011a) Ground-based laserscanning—a new method for measuring fluvial erosion on steep slopes. In: Hafeez MM (ed) GRACE, remote sensing and ground-based methods in multi-scale hydrology: Proceedings of the symposium JHS01 [entitled: GRACE, remote sensing and ground-based methods in multi-scale hydrology] held during the IUGG GA in Melbourne (28 June–7 July 2011). IAHS Publ, Wallingford, pp 163–168
Haas F, Heckmann T, Wichmann V, Becht M (2011b) Quantification and modeling of fluvial bedload discharge from hillslope channels in two alpine catchments (Bavarian Alps, Germany). Z Geomorph NF 55(Suppl):147–168
Haas F, Heckmann T, Hilger L, Becht M (2012) Quantification and modelling of debris flows in the proglacial area of the Gepatschferner, Austria, using ground-based LiDAR. In: Collins A (ed) Erosion and sediment yields in the changing environment: proceedings of an IAHS International Commission on continental erosion symposium held at the institute of mountain hazards and environment, CAS-Chengdu, China, 11–15 Oct 2012. IAHS Press, Wallingford, pp 293–302
Hagg W, Becht M (2000) Einflüsse von Niederschlag und Substrat auf die Auslösung von Hangmuren in Beispielgebieten der Ostalpen. In: Becht M, Schmidt K-H (eds) Angewandte und vernetzte geomorphologische Prozeßforschung, vol 123. Borntraeger, Berlin, pp 79–92
Hartl L (2010) The Gepatschferner from 1850–2006: changes in length, area and volume in relation to climate. University of Innsbruck
Holm K, Bovis M, Jakob M (2004) The landslide response of alpine basins to post-Little Ice Age glacial thinning and retreat in southwestern British Columbia. Geomorphology 57:201–216
Hugenholtz CH, Moorman B, Barlow J, Wainstein P (2008) Large-scale moraine deformation at the Athabasca Glacier, Jasper National Park, Alberta, Canada. Landslides 5:251–260. https://doi.org/10.1007/s10346-008-0116-5
Carrivick JL, Heckmann T (2017) Short-term geomorphological evolution of proglacial systems. Geomorphology 287:3–28
Kellerer-Pirklbauer A, Proske H, Strasser V (2010) Paraglacial slope adjustment since the end of the last glacial maximum and its long-lasting effects on secondary mass wasting processes: Hauser Kaibling, Austria. Geomorphology 120:65–76. https://doi.org/10.1016/j.geomorph.2009.09.016
Klok E, Oerlemans J (2003) Deriving historical equilibrium-line altitudes from a glacier length record by linear inverse modelling. Holocene 13:343–351. https://doi.org/10.1191/0959683603hl627rp
Lambrecht A, Kuhn M (2007) Glacier changes in the Austrian Alps during the last three decades derived from the new Austrian glacier inventory. Ann Glaciol 46:177–184. https://doi.org/10.3189/172756407782871341
Lane SN, Westaway RM, Murray Hicks D (2003) Estimation of erosion and deposition volumes in a large, gravel-bed, braided river using synoptic remote sensing. Earth Surf Proc Land 28:249–271. https://doi.org/10.1002/esp.483
Matthews JA, Shakesby RA (2004) A twentieth-century neoparaglacial rock topple on a glacier foreland, Ötztal Alps, Austria. Holocene 14:454–458. https://doi.org/10.1191/0959683604hl706rr
McColl ST (2012) Paraglacial rock-slope stability. Geomorphology 153–154:1–16. https://doi.org/10.1016/j.geomorph.2012.02.015
Morche D, Haas F, Baewert H, Heckmann T, Schmidt K-H, Becht M (2012) Sediment transport in the proglacial Fagge River (Kaunertal/Austria). In: Collins A (ed) Erosion and sediment yields in the changing environment: proceedings of an IAHS International Commission on continental erosion symposium held at the institute of mountain hazards and environment, CAS-Chengdu, China, 11–15 Oct 2012. IAHS Press, Wallingford, pp 72–80
Neugirg F (2016) Quantifizierung, Analyse und Modellierung von Erosionsprozessen auf Steilhängen in unterschiedlichen Klimaten durch hochaufgelöste Geländemodellen. Dissertation, Katholische Universität Eichstätt-Ingolstadt
Neugirg F, Kaiser A, Schindewolf M, Becht M, Schmidt J, Haas F (2015) Monitoring and modelling slope dynamics in an Alpine watershed—a combined approach of soil science, remote sensing and geomorphology. Proc IAHS 371:181–187. https://doi.org/10.5194/piahs-371-181-2015
Neugirg F, Stark M, Kaiser A, Vlacilova M, Della Seta M, Vergari F, Schmidt J, Becht M, Haas F (2016a) Erosion processes in calanchi in the Upper Orcia Valley, Southern Tuscany, Italy based on multitemporal high-resolution terrestrial LiDAR and UAV surveys. Geomorphology 269:8–22. https://doi.org/10.1016/j.geomorph.2016.06.027
Neugirg F, Kaiser A, Huber A, Heckmann T, Schindewolf M, Schmidt J, Becht M, Haas F (2016b) Using terrestrial LiDAR data to analyse morphodynamics on steep unvegetated slopes driven by different geomorphic processes. CATENA 142:269–280. https://doi.org/10.1016/j.catena.2016.03.021
Oostwoud Wijdenes DJ, Ergenzinger P (1998) Erosion and sediment transport on steep marly hillslopes, Draix, Haute-Provence, France: an experimental field study. CATENA 33:179–200. https://doi.org/10.1016/S0341-8162(98)00076-9
Patzelt G (1980) The Austrian glacier inventory: status and first results. IAHS Publication 126
Pelletier JD, Orem CA (2014) How do sediment yields from post-wildfire debris-laden flows depend on terrain slope, soil burn severity class, and drainage basin area?: Insights from airborne-LiDAR change detection. Earth Surf Proc Land 39:1822–1832. https://doi.org/10.1002/esp.3570
Schauer T (1999) Beispiele von Erosionsprozessen in Zusammenhang mit den Standortfaktoren Nutzung und Vegetation im Bayerischen Alpenraum. Relief Boden Pal’aoklima 14:117–128
Schiefer E, Gilbert R (2007) Reconstructing morphometric change in a proglacial landscape using historical aerial photography and automated DEM generation. Geomorphology 88:167–178
Schindewolf M, Kaiser A, Neugirg F, Richter C, Haas F, Schmidt J (2016) Seasonal erosion patterns under alpine conditions: benefits and challenges of a novel approach in physically based soil erosion modeling. Zeit fur Geo 60(Supp):109–123. https://doi.org/10.1127/zfg_suppl/2015/s-00185
Wetzel K-F (1992) Abtragsprozesse an Hängen und Feststoffführung der Gewässer. Dargestelllt am Beispiel der pleistozänen Lockergesteine des Lainbachgebietes (Benediktbeuern/ Obb.). Münchener Geographische Abhandlungen B, vol 17. Geobuch-Verlag, München
Zimmermann M (1990) Debris flows 1987 in Switzerland: geomorphological and meteorological aspects. In: Sinniger RO, Monbaron M (eds) Hydrology in mountainous regions II—artificial reservoirs; water and slopes, vol 194, pp 387–393
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Dusik, JM., Neugirg, F., Haas, F. (2019). Slope Wash, Gully Erosion and Debris Flows on Lateral Moraines in the Upper Kaunertal, Austria. In: Heckmann, T., Morche, D. (eds) Geomorphology of Proglacial Systems. Geography of the Physical Environment. Springer, Cham. https://doi.org/10.1007/978-3-319-94184-4_11
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