Panomax images. Three of the large-scale ice-breakup events occurred between.

Benn 3, Felix Bernsteiner 1, Philipp Krisch 1, and Christian Ziesler 1.

Geodynamik (ZAMG), Vienna, Austria 3 School of Geography and Sustainable Development, University of St Andrews, St.

August 2019. We identified a sequence of processes: glacier recession into a.

The formation of proglacial lakes is important because they can pose.

Harrison et al., 2018), increase rates of ice mass loss, and alter the dynamic.

Liu et al., 2020).

However, detailed descriptions of proglacial lake formation.

Heckmann (2017) pointed out that there is an urgent need for inventories of.

Water bodies at the glacier surface form initially as supraglacial lakes which.

In this study, we analysed rates and processes of glacier recession and.

This glacier covered 26.5 km 2 during the LIA.

Glockner Mountains, the Hohe Tauern range, at 47 05 N, 12 43 E (Fig.

The gently sloping, 4.5 km long glacier.

Figure 2 Evolution of the proglacial area at Pasterze Glacier.

Maat Hydro Series Of Length

The longest time series of length changes at Austrian glaciers has been.

Pasterze Glacier receded by 1550 m, 3 times the mean value for all.

Glacier is characterized by annual mean recession rates in the order of magnitude of.

An automatic weather station is located close to the study area operated by.

VERBUND Hydro Power GmbH since 1982 (AWS in Fig.

The coldest calendar year.

GNSS technique was applied using different handheld Garmin devices (geometric.

Kellerer-Pirklbauer, 2019) or 1:200 (201819; this study).

The.

Sect. 3.4). TLS data from 2010 to 2019 (13 September 2010, 27 September.

KAGIS is the GIS Service of the Regional Government of Carinthia; BEV is the Federal Office of Metrology and Surveying.

The assumption of long-term lake-level variations of m during the summer months (seasonal amplitude).

Maat Hydro Crack