Relevant bibliographies by topics / Gschnitz

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Academic literature on the topic 'Gschnitz'

Author: Grafiati
Published: 28 July 2024
Last updated: 31 July 2025

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Journal articles on the topic "Gschnitz"

1

Kerschner, Hanns, Susan Ivy-Ochs, and Christian Schlüchter. "Paleoclimatic interpretation of the early Late-glacial glacier in the Gschnitz valley, central Alps, Austria." Annals of Glaciology 28 (1999): 135–40. http://dx.doi.org/10.3189/172756499781821661.

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AbstractThe former glacier at the type locality of the “Gschnitz Stadial” of the Alpine Late-glacial chronology is interpreted from a paleoglaciological and paleoclimatological point of view. The equilibrium-line altitude, ice flux through selected cross sections and mass-balance gradients are calculated from reconstructed glacier topography. They are used to determine total net ablation and accumulation and precipitation under the assumption of steady-state. The former temperature at the ELA and temperature change is estimated using various glacier—climate models. Precipitation was less than
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2

Gschwentner, Philipp, Hanns Kerschner, and Christoph Spötl. "Late Glacial ice advance in the Kellerjoch region near Schwaz (Tyrol, Eastern Alps)." Austrian Journal of Earth Sciences 113, no. 1-2 (2020): 211–27. http://dx.doi.org/10.17738/ajes.2020.0013.

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Abstract The Kellerjoch forms a small isolated massif at the northernmost rim of the central Eastern Alps of Tyrol and shows a number of geomorphological features of glacial and periglacial origin. Mapping yields evidence of two local glaciations postdating the Last Glacial Maximum. Using a simple glaciological approach the palaeoglaciers related to these events were reconstructed. The older glaciation yields an equilibrium line altitude (ELA) ranging from 1660 m for the maximum extent to 1800 m a.s.l. for the innermost moraine. For the younger glaciation, ELAs were reconstructed at 1905 m and
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3

Ribolini, Adriano. "Towards a synchronous Gschnitz glacier stadial (Heinrich Event 1) across the Alps." Quaternary International 279-280 (November 2012): 401–2. http://dx.doi.org/10.1016/j.quaint.2012.08.1272.

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Ivy-Ochs, Susan, Hanns Kerschner, Peter W. Kubik, and Christian Schlüchter. "Glacier response in the European Alps to Heinrich Event 1 cooling: the Gschnitz stadial." Journal of Quaternary Science 21, no. 2 (2006): 115–30. http://dx.doi.org/10.1002/jqs.955.

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Federici, Paolo Roberto, Darryl E. Granger, Adriano Ribolini, Matteo Spagnolo, Marta Pappalardo, and Andrew J. Cyr. "Last Glacial Maximum and the Gschnitz stadial in the Maritime Alps according to10Be cosmogenic dating." Boreas 41, no. 2 (2011): 277–91. http://dx.doi.org/10.1111/j.1502-3885.2011.00233.x.

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6

Lehmann, Benjamin, Frédéric Herman, Pierre G. Valla, et al. "Postglacial erosion of bedrock surfaces and deglaciation timing: New insights from the Mont Blanc massif (western Alps)." Geology 48, no. 2 (2019): 139–44. http://dx.doi.org/10.1130/g46585.1.

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Abstract Since the Last Glacial Maximum, ∼20 k.y. ago, Alpine glaciers have retreated and thinned. This transition exposed bare bedrock surfaces that could then be eroded by a combination of debuttressing or local frost cracking and weathering. Quantification of the respective contributions of these processes is necessary to understand the links between long-term climate and erosion in mountains. Here, we quantified the erosion histories of postglacial exposed bedrock in glacial valleys. Combining optically stimulated luminescence and terrestrial cosmogenic nuclide (TCN) surface exposure datin
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7

Reitner, Jürgen M., Susan Ivy-Ochs, Ruth Drescher-Schneider, Irka Hajdas, and Manfred Linner. "Reconsidering the current stratigraphy of the Alpine Lateglacial: Implications of the sedimentary and morphological record of the Lienz area (Tyrol/Austria)." E&G Quaternary Science Journal 65, no. 2 (2016): 113–44. http://dx.doi.org/10.3285/eg.65.2.02.

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Abstract. Die morphologischen und sedimentären Belege aus dem Raum Lienz liefern starke Argumente gegen die bisher angewandte, fünfgliedrige Stratigraphie des Alpinen Spätglazials (ALG; ca 19–11.7 ka), dem Zeitraum nach dem Würm-Hochglazial (= Alpines Letztes Glaziales Maximum; AlpLGM). Die Resultate einer flächendeckenden geologischen Kartierung (inklusive Erfassung von Massenbewegungen) unterstützt durch geochronologische Methoden sowie Pollenanalysen zeigen, dass sich die ALG-Abfolgen in der Schobergruppe und den Lienzer Dolomiten jeweils in vier „unconformity-bounded units“ im Sinne der Al
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Furrer, G., C. Burga, M. Gamper, H. P. Holzhauser, and M. Maisch. "Zur Gletscher-, Vegetations- und Klimageschichte der Schweiz seit der Späteiszeit." Geographica Helvetica 42, no. 2 (1987): 61–91. http://dx.doi.org/10.5194/gh-42-61-1987.

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Abstract. A Statistical analysis of published and compilated snowline data for the late-glacial Stades of Gschnitz, Clavadel, Daun and Egesen is presented. The calculation of snowline and snowline-depression (compared to the extent of 1850) is based on the 2: 1 -equilibrium line method. The Interpretation does not show significant differences in snowline-depression between the Lower Engadin (Eastern Alps) and the Mont Blanc area (Western Alps). The larger deviations from the averages can be explained by the glacier individuality (morphology, topography of the ice surfaces) and the rarely consi
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9

Stelter, K. "GSCHNITZER, F.: Kleine Schriften zum griechischen und römischen Altertum. Band I. Frühes Griechentum: Historische und sprachwissenschaftliche Beiträge. Hrsg. v. C. Trümpy und T. Schmitt." Kratylos 49, no. 1 (2004): 200–203. http://dx.doi.org/10.29091/kratylos/2004/1/42.

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10

Braumann, Sandra M., Joerg M. Schaefer, Stephanie Neuhuber, and Markus Fiebig. "Moraines in the Austrian Alps record repeated phases of glacier stabilization through the Late Glacial and the Early Holocene." Scientific Reports 12, no. 1 (2022). http://dx.doi.org/10.1038/s41598-022-12477-x.

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AbstractClimate is currently warming due to anthropogenic impact on the Earth’s atmosphere. To better understand the processes and feedbacks within the climate system that underlie this accelerating warming trend, it is useful to examine past periods of abrupt climate change that were driven by natural forcings. Glaciers provide an excellent natural laboratory for reconstructing the climate of the past as they respond sensitively to climate oscillations. Therefore, we study glacier systems and their behavior during the transition from colder to warmer climate phases, focusing on the period bet
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Books on the topic "Gschnitz"

1

Klier, Walter. Stubai - Wipptal mit Gschnitz, Obernberg, Navis, Schmirn, Vals. Bergverlag Rother, 2003.

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2

Klier, Walter. Stubai - Wipptal mit Gschnitz, Obernberg, Navis, Schmirn, Vals. Bergverlag Rother, 2003.

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3

Klier, Walter. Stubai - Wipptal mit Gschnitz, Obernberg, Navis, Schmirn, Vals. Bergverlag Rother, 2003.

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4

Stoffaneller, Thomas. S´hat Gschneit. Blurb, 2017.

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