Rhenodanubian Flyschzone, Bavarian Alps

2011 ◽  
pp. 51-73 ◽  
Author(s):  
Reinhard Hesse
Keyword(s):  
Bavarian Alps

Climate and glacier fluctuations in the Bavarian Alps in the past 120 years

Erdkunde ◽  
2012 ◽  
pp. 121-142 ◽  
Author(s):  
Wilfried Hagg ◽  
Christoph Mayer ◽  
Elisabeth Mayr ◽  
Achim Heilig
Keyword(s):  
The Past ◽  
Glacier Fluctuations ◽  
Bavarian Alps

scholarly journals Forest fire danger rating in complex topography – results from a case study in the Bavarian Alps in autumn 2011

2013 ◽  
Vol 13 (9) ◽  
pp. 2157-2167 ◽  
Author(s):  
C. Schunk ◽  
C. Wastl ◽  
M. Leuchner ◽  
C. Schuster ◽  
A. Menzel
Keyword(s):  
Forest Fire ◽  
Temperature Inversion ◽  
Fire Danger ◽  
Complex Topography ◽  
Pressure System ◽  
Drought Period ◽  
Bavarian Alps ◽  
Forest Fire Danger ◽  
Fire Danger Indices

Abstract. Forest fire danger rating based on sparse meteorological stations is known to be potentially misleading when assigned to larger areas of complex topography. This case study examines several fire danger indices based on data from two meteorological stations at different elevations during a major drought period. This drought was caused by a persistent high pressure system, inducing a pronounced temperature inversion and its associated thermal belt with much warmer, dryer conditions in intermediate elevations. Thus, a massive drying of fuels, leading to higher fire danger levels, and multiple fire occurrences at mid-slope positions were contrasted by moderate fire danger especially in the valleys. The ability of fire danger indices to resolve this situation was studied based on a comparison with the actual fire danger as determined from expert observations, fire occurrences and fuel moisture measurements. The results revealed that, during temperature inversion, differences in daily cycles of meteorological parameters influence fire danger and that these are not resolved by standard meteorological stations and fire danger indices (calculated on a once-a-day basis). Additional stations in higher locations or high-resolution meteorological models combined with fire danger indices accepting at least hourly input data may allow reasonable fire danger calculations under these circumstances.

scholarly journals A willow drawing from 1786: the earliest depiction of intraspecific trait variation in plants?

2020 ◽  
Author(s):  
Ulrich E Stegmann
Keyword(s):  
Environmental Conditions ◽  
18Th Century ◽  
Elevation Gradient ◽  
Experimental Studies ◽  
Fourth Century ◽  
Trait Variation ◽  
Intraspecific Trait Variation ◽  
Bavarian Alps ◽  
In The Wild ◽  
Unidentified Species

Abstract Background and Aims The study of intraspecific trait variation (ITV) in plants has a long history, dating back to the fourth century BC. Its existence was widely acknowledged by the end of the 18th century, although systematic and experimental studies commenced only a century later. However, the historiography of ITV has many gaps, especially with regard to early observations and visual documents. This note identifies an early depiction of plant ITV. Methods The botanical works of Johann Wolfgang von Goethe (1749–1832), a German writer and naturalist, were subjected to close reading. This included all publications and unpublished sources related to botany between 1785 and 1832 (e.g. notes, drafts, diaries, letters, drawings). This material is accessible in the multi-volume historical-critical edition of Goethe’s studies in natural science (Leopoldina-Ausgabe). Key Results A diary entry from 9 September 1786 described changes in leaf morphology along an elevation gradient in the Bavarian Alps. The leaves of an unidentified species of willow (Spix sp.) and gentian (Gentiana sp.) were said to become narrower with increasing elevation; leaves also stood further apart on twigs, and the latter became thinner. A crude drawing of two willow twigs illustrated the differences. Goethe conjectured that the differences were due to environmental conditions. Conclusions Goethe’s notes were anecdotal, and it is unclear whether the observed plant individuals actually belonged to the same species. Nevertheless, the notes represent an early and clear articulation of the hypothesis that changes in environmental conditions can cause ITV in a natural plant population. The drawing may be the earliest visual record of environmentally caused plant ITV in the wild.

The Mesolithic site Ullafelsen in the Fotsch Valley (Tyrol, Austria) – a biomarker perspective

2020 ◽  
Author(s):  
Michael Zech ◽  
Marcel Lerch ◽  
Marcel Bliedtner ◽  
Clemens Geitner ◽  
Dieter Schäfer ◽  
...  
Keyword(s):  
Environmental History ◽  
Analytical Data ◽  
Late Glacial ◽  
Swiss Alps ◽  
Peat Bogs ◽  
High Mountain ◽  
Hunter Gatherers ◽  
Alpine Regions ◽  
Bavarian Alps ◽  
History Of

<p>The archaeology of high mountain regions got high attention since the discovery of the copper age mummy called "Ötzi" in the Ötztaler Alps in 1991. Results of former archaeological research projects show that mesolithic hunter-gatherers lived in Alpine regions since the beginning of the Holocene, 11,700 years ago (Cornelissen & Reitmaier 2016). Amongst others, the Mesolithic site Ullafelsen (1860 m a.s.l.) and surroundings represent a very important archaeological reference site in the Fotsch Valley (Stubaier Alps, Tyrol) (Schäfer 2011). Many archaeological artifacts and fire places were found at different places in the Fotschertal, which provides evidence for the presence and the way of living of our ancestor. The "Mesolithic project Ullafelsen" includes different scientific disciplines ranging from high mountain archaeology over geology, geomorphology, soil science, sedimentology, petrography to palaeobotany (Schäfer 2011). Within an ongoing DFG project we aim at addressing questions related to past vegetation and climate, human history as well as their influence on pedogenesis from a biomarker and stable isotope perspective (cf. Zech et al. 2011). Our results for instance suggest that (i) the dominant recent and past vegetation can be chemotaxonomically differentiated based on leaf wax-derived <em>n</em>-alkane biomarkers, (ii) there is no evidence for buried Late Glacial topsoils being preserved on the Ullafelsen as argued by Geitner et al. (2014), rather humic-rich subsoils were formed as B<sub>h</sub>-horizons by podsolisation and (iii) marked vegetations changes likely associated with alpine pasture activities since the Bronce Age are documented in Holocene peat bogs in the Fotsch Valley. Nevertheless, there remain some challenges by joining all analytical data in order to get a consistent overall picture of human-environmental history of this high mountain region.</p><p>Cornelissen & Reitmaier (2016): Filling the gap: Recent Mesolithic discoveries in the central and south-eastern Swiss Alps. In: Quaternary International, 423.</p><p>Geitner, C., Schäfer, D., Bertola, S., Bussemer, S., Heinrich, K. und J. Waroszewski (2014): Landscape archaeological results and discussion of Mesolithic research in the Fotsch valley (Tyrol). In: Kerschner, H., Krainer, K. and C. Spötl: From the foreland to the Central Alps – Field trips to selected sites of Quaternary research in the Tyrolean and Bavarian Alps (DEUQUA EXCURSIONS), Berlin, 106-115.</p><p>Schäfer (2011): Das Mesolithikum-Projekt Ullafelsen (Teil 1). Mensch und Umwelt im Holozän Tirols (Band 1). 560 p., Innsbruck: Philipp von Zabern.</p><p>Zech, M., Zech, R., Buggle, B., Zöller, L. (2011): Novel methodological approaches in loess research - interrogating biomarkers and compound-specific stable isotopes. In: E&G Quaternary Science Journal, 60.</p>

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