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Zeitschriftenartikel zum Thema „Stubai“

Autor: Grafiati

Veröffentlicht am 24. Juni 2021

Zuletzt aktualisiert am 29. Juli 2025

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1

Schulz, Bernhard, Joachim Krause, and Robert Zimmermann. "Electron microprobe petrochronology of monazite-bearing garnet micaschists in the Oetztal-Stubai Complex (Alpeiner Valley, Stubai)." Swiss Journal of Geosciences 112, no. 2-3 (2019): 597–617. http://dx.doi.org/10.1007/s00015-019-00351-4.

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2

Mogessie, A., F. Purtscheller, and R. Tessadri. "Chromite and chrome spinel occurrences from metacarbonates of the Oetztal–Stubai Complex (Northern Tyrol, Austria)." Mineralogical Magazine 52, no. 365 (1988): 229–36. http://dx.doi.org/10.1180/minmag.1988.052.365.09.

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AbstractChromite inclusions in uvarovite-chrome garnet, chemically zoned chromite-chrome spinel and chrome spinel-olivine pairs from metacarbonates of the Oetztal-Stubai Complex (northern Tyrol, Austria) are described in terms of their textural occurrences and chemical compositions. Their genetic relationship in relation to the polymetamorphism of the region is discussed.

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3

Vavtar, F. "Das Zinn-Kupfer-Erzvorkommen am Gl�cksgrat (Stubai-Kristallin)." TMPM Tschermaks Mineralogische und Petrographische Mitteilungen 35, no. 4 (1986): 287–98. http://dx.doi.org/10.1007/bf01191992.

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4

Purtscheller, F., and R. Tessadri. "Zirconolite and baddeleyite from metacarbonates of the Oetzstal–Stubai Complex (northern Tyrol, Austria)." Mineralogical Magazine 49, no. 353 (1985): 523–29. http://dx.doi.org/10.1180/minmag.1985.049.353.05.

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AbstractZirconolite and baddeleyite from polymetamorphosed metacarbonates of the Oetztal-Stubai complex (northern Tyrol, Austria) are described in terms of their paragenetic relationship and chemical compositions. For the first time an analysis of a chemically zoned niobian zirconolite (high Nb and low Ti in core, low Nb and high Ti at rim) is presented. Genetic possibilities for the origin of the metacarbonates are discussed in the light of zirconolite- and baddeleyite-formation.

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5

Mogessie, Aberra, Fridolin Purtscheller, and Richard Tessadri. "Geochemistry of amphibolites from the Ötztal—Stubai Complex (northern Tyrol, Austria)." Chemical Geology 51, no. 1-2 (1985): 103–13. http://dx.doi.org/10.1016/0009-2541(85)90090-7.

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6

Krois, Peter, Volkmar Stingl, and Fridolin Purtscheller. "Metamorphosed weathering horizon from the Oetztal-Stubai crystalline complex (Eastern Alps, Austria)." Geology 18, no. 11 (1990): 1095. http://dx.doi.org/10.1130/0091-7613(1990)018<1095:mwhfto>2.3.co;2.

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7

Hammerle, A., A. Haslwanter, U. Tappeiner, A. Cernusca, and G. Wohlfahrt. "Leaf area controls on energy partitioning of a temperate mountain grassland." Biogeosciences 5, no. 2 (2008): 421–31. http://dx.doi.org/10.5194/bg-5-421-2008.

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Abstract. Using a six year data set of eddy covariance flux measurements of sensible and latent heat, soil heat flux, net radiation, above-ground phytomass and meteorological driving forces energy partitioning was investigated at a temperate mountain grassland managed as a hay meadow in the Stubai Valley (Austria). The main findings of the study were: (i) Energy partitioning was dominated by latent heat, followed by sensible heat and the soil heat flux; (ii) When compared to standard environmental forcings, the amount of green plant matter, which due to three cuts varied considerably during th

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8

Hammerle, A., A. Haslwanter, U. Tappeiner, A. Cernusca, and G. Wohlfahrt. "Leaf area controls on energy partitioning of a mountain grassland." Biogeosciences Discussions 4, no. 5 (2007): 3607–38. http://dx.doi.org/10.5194/bgd-4-3607-2007.

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Abstract. Using a six year data set of eddy covariance flux measurements of sensible and latent heat, soil heat flux, net radiation, above-ground phytomass and meteorological driving forces energy partitioning was investigated at a temperate mountain grassland managed as a hay meadow in the Stubai Valley (Austria). The main findings of the study were: i) Energy partitioning was dominated by latent heat, followed by sensible heat and the soil heat flux; ii) When compared to standard environmental forcings, the amount of green plant matter, which due to three cuts varied considerably during the

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9

Krainer, Karl, and Wolfram Mostler. "Reichenkar rock glacier: a glacier derived debris-ice system in the western Stubai Alps, Austria." Permafrost and Periglacial Processes 11, no. 3 (2000): 267–75. http://dx.doi.org/10.1002/1099-1530(200007/09)11:3<267::aid-ppp350>3.0.co;2-e.

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10

Denoth, A., and A. Foglar. "Measurements of Daily Variations in the Subsurface Wetness Gradient." Annals of Glaciology 6 (1985): 254–55. http://dx.doi.org/10.3189/s026030550001051x.

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A flat condenser in strip-line technique has been developed to measure the gradient in liquid water content near the snow surface. This dielectric sensor is connected to a twin-T-bridge with an operating frequency of 27 MHz. The special design of the sensor allows the non-destructive measurement of the mean dielectric constant of underlying material at two different depths of 0 to 2 cm, and of 2 to 4 cm below the snow surface. Based on the model of Polder and van Santen, changes in the gradient of liquid water content can be calculated from measured changes in the dielectric constant in differ

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11

Denoth, A., and A. Foglar. "Measurements of Daily Variations in the Subsurface Wetness Gradient." Annals of Glaciology 6 (1985): 254–55. http://dx.doi.org/10.1017/s026030550001051x.

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A flat condenser in strip-line technique has been developed to measure the gradient in liquid water content near the snow surface. This dielectric sensor is connected to a twin-T-bridge with an operating frequency of 27 MHz. The special design of the sensor allows the non-destructive measurement of the mean dielectric constant of underlying material at two different depths of 0 to 2 cm, and of 2 to 4 cm below the snow surface. Based on the model of Polder and van Santen, changes in the gradient of liquid water content can be calculated from measured changes in the dielectric constant in differ

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12

Mair, Rudolf, and Michael Kuhn. "Temperature and movement measurements at a bergschrund." Journal of Glaciology 40, no. 136 (1994): 561–65. http://dx.doi.org/10.1017/s0022143000012442.

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AbstractThe highest, nearly stationary crevasse that occurs on most alpine glaciers is commonly called a bergschrund. It has often been believed to form when the main ice body below slides downward and thus separates from the thin, steep ice above, which is supposed to remain frozen to its bed. In order to verify or refute this assumption, temperatures and ice motion were recorded at several points in and around a bergschrund on Daunferner, a glacier in the Stubai Alps in Tyrol, Austria. Both measurements and observations indicated that the ice above the bergschrund was sliding as well and tha

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13

Mair, Rudolf, and Michael Kuhn. "Temperature and movement measurements at a bergschrund." Journal of Glaciology 40, no. 136 (1994): 561–65. http://dx.doi.org/10.3189/s0022143000012442.

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AbstractThe highest, nearly stationary crevasse that occurs on most alpine glaciers is commonly called a bergschrund. It has often been believed to form when the main ice body below slides downward and thus separates from the thin, steep ice above, which is supposed to remain frozen to its bed. In order to verify or refute this assumption, temperatures and ice motion were recorded at several points in and around a bergschrund on Daunferner, a glacier in the Stubai Alps in Tyrol, Austria. Both measurements and observations indicated that the ice above the bergschrund was sliding as well and tha

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14

Achammer, TH, and A. Denoth. "Snow dielectric properties: from DC to microwave X-band." Annals of Glaciology 19 (1994): 92–96. http://dx.doi.org/10.3189/s0260305500011034.

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Broadband measurements of dielectric properties of natural snow samples near or at 0°C are reported. Measurement quantities are: dielectric permittivity, loss factor and complex propagation factor for electromagnetic waves. X-band measurements were made in a cold room in the laboratory; measurements at low and intermediate frequencies were carried out both in the field (Stubai Alps, 3300 m; Hafelekar near Innsbruck, 2100 m) and in the cold room. Results show that in the different frequency ranges the relative effect on snow dielectric properties of the parameters: density, grain-size and shape

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15

Achammer, TH, and A. Denoth. "Snow dielectric properties: from DC to microwave X-band." Annals of Glaciology 19 (1994): 92–96. http://dx.doi.org/10.1017/s0260305500011034.

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Broadband measurements of dielectric properties of natural snow samples near or at 0°C are reported. Measurement quantities are: dielectric permittivity, loss factor and complex propagation factor for electromagnetic waves. X-band measurements were made in a cold room in the laboratory; measurements at low and intermediate frequencies were carried out both in the field (Stubai Alps, 3300 m; Hafelekar near Innsbruck, 2100 m) and in the cold room. Results show that in the different frequency ranges the relative effect on snow dielectric properties of the parameters: density, grain-size and shape

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16

KONZETT, J. "Metamorphic Evolution of Iron-rich Mafic Cumulates from the Otztal-Stubai Crystalline Complex, Eastern Alps, Austria." Journal of Petrology 46, no. 4 (2004): 717–47. http://dx.doi.org/10.1093/petrology/egh095.

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17

Hausmann, H., K. Krainer, E. Brückl, and W. Mostler. "Internal structure and ice content of Reichenkar rock glacier (Stubai Alps, Austria) assessed by geophysical investigations." Permafrost and Periglacial Processes 18, no. 4 (2007): 351–67. http://dx.doi.org/10.1002/ppp.601.

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18

Stingl, Volkmar, and Peter Krois. "Sedimentological investigations of metamorphic clastics: the basal clastic rocks of the Brenner Mesozoic (Stubai Alps, Austria/Italy)." Terra Nova 2, no. 3 (1990): 273–81. http://dx.doi.org/10.1111/j.1365-3121.1990.tb00075.x.

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19

Moran, Andrew P., Susan Ivy Ochs, Marcus Christl, and Hanns Kerschner. "Exposure dating of a pronounced glacier advance at the onset of the late-Holocene in the central Tyrolean Alps." Holocene 27, no. 9 (2017): 1350–58. http://dx.doi.org/10.1177/0959683617690589.

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A two-phased moraine system in the high Alpine valley of Lisenser Längental in the Stubai Alps of western Austria is located in an intermediate morphostratigraphic position constrained by ‘Egesen Stadial’ (Younger Dryas) moraines down valley and ‘Little Ice Age’ (‘LIA’) positions (modern times) up valley. The equilibrium line altitude (ELA) was about 50 m lower than during the ‘LIA’ when applying an accumulation area ratio of 0.67. Exposure dating of boulders with 10Be yields a mean age of 3750 ± 330 years for the more extensive outer moraine system and a single age of 3140 ± 280 years for the

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20

Melcher, Frank, and Peter Krois. "Syngenetic and diagenetic formation of ore deposits in the metamorphosed sediments of the basal Brenner Mesozoic (Stubai Valley, Austria)." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1992, no. 4 (1992): 207–20. http://dx.doi.org/10.1127/njgpm/1992/1992/207.

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21

Angerer, Thomas, Frank Melcher, Peter Onuk, Peter Tropper, Albin Volgger, and Patrick Gasteiger. "High-Tech-Metalle in ostalpinen Buntmetallsulfidvorkommen: geologische Faktoren ihrer Anreicherung, Verteilung und Mobilisation (drei MRI-Projekte 2015–2019)." BHM Berg- und Hüttenmännische Monatshefte 166, no. 4 (2021): 181–92. http://dx.doi.org/10.1007/s00501-021-01103-4.

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ZusammenfassungDie Ergebnisse dreier MRI Projekte 2015–2019 (Leoben und Innsbruck) werden hier zusammenfassend dargestellt. Der Fokus liegt auf den Ergebnissen des Innsbrucker Projekts, in dem sedimentär-exhalative Erze des Ötztal-Stubai-Kristallins (ÖSK) als beispielhaftes Mineralsystem erforscht wurden, um den komplexen Einfluss geologischer Prozesse auf die Anreicherung bzw. mineralogische Verteilung von Spurenelementen zu verdeutlichen.Die umfangreichen Datensätze aus vielen ostalpinen Bergbaurevieren erlauben Aussagen über die Präferenz von Spurenelementen in verschiedenen Typen von Fe-Cu

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22

Bamberger, I., L. Hörtnagl, R. Schnitzhofer, et al. "Long term BVOC fluxes above mountain grassland." Biogeosciences Discussions 7, no. 1 (2010): 83–110. http://dx.doi.org/10.5194/bgd-7-83-2010.

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Abstract. Grasslands comprise natural tropical savannah over managed temperate fields to tundra and cover over a quarter of the Earth's land surface. Plant growth, maintenance and decay result in volatile organic compound (VOCs) emissions to the atmosphere. Furthermore, biogenic VOCs (BVOCs) are emitted due to various environmental stresses including cutting and drying during harvesting. Fluxes of BVOCs were measured with a proton-transfer-reaction – mass-spectrometer (PTR-MS) over temperate mountain grassland in Stubai Valley (Tyrol, Austria) over one growing season (2008). VOC fluxes were ca

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23

Schulz, Bernhard. "Petrochronology of Monazite-Bearing Garnet Micaschists as a Tool to Decipher the Metamorphic Evolution of the Alpine Basement." Minerals 11, no. 9 (2021): 981. http://dx.doi.org/10.3390/min11090981.

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Garnet-bearing metapelites in the Helvetic and Austroalpine pre-Mesozoic polymetamorphic basement are characterised by pressure-temperature path segments reconstructed by microstructurally controlled geothermobarometry, and the Th-U-Pb monazite age distribution pattern revealed by the electron probe microanalyser (EPMA). In the Helvetic Aiguilles Rouges Massif and the Austroalpine Oetztal-Stubai basement to the NW an Ordovician-to-Silurian high temperature event preceded a pressure-dominated Carboniferous metamorphism. In the Austroalpine basement units to the south of the Tauern Window, the m

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Fügenschuh, Bernhard, Neil S. Mancktelow, and Diane Seward. "Cretaceous to Neogene cooling and exhumation history of the Oetztal-Stubai basement complex, eastern Alps: A structural and fission track study." Tectonics 19, no. 5 (2000): 905–18. http://dx.doi.org/10.1029/2000tc900014.

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25

Fleischer, Fabian, Florian Haas, Moritz Altmann, Jakob Rom, Camillo Ressl, and Michael Becht. "Glaciogenic Periglacial Landform in the Making—Geomorphological Evolution of a Rockfall on a Small Glacier in the Horlachtal, Stubai Alps, Austria." Remote Sensing 15, no. 6 (2023): 1472. http://dx.doi.org/10.3390/rs15061472.

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Deglaciation in high mountain areas signifies the transition from glacial to periglacial conditioned landscapes. Due to the reduced melt rate of debris-covered glacier ice, these areas of the glacier may persist long after the surrounding glacier has melted, resulting in the formation of distinct post-glacial landforms. In this study, we examine the geomorphological evolution and potential future development of a 19,267 m3 ± 204 m3 rockfall from the permafrost-affected headwall on the low-elevated Zwieselbachferner in the Horlachtal, Stubai Alps, Austria. The analysis uses multi-epochal remote

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Lerch, Marcel, Tobias Bromm, Clemens Geitner, et al. "Human and livestock faecal biomarkers at the prehistorical encampment site of Ullafelsen in the Fotsch Valley, Stubai Alps, Austria – potential and limitations." Biogeosciences 19, no. 4 (2022): 1135–50. http://dx.doi.org/10.5194/bg-19-1135-2022.

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Abstract. The Ullafelsen at 1869 m above sea level (a.s.l.) in the Tyrolean Stubai Alps next to Innsbruck is an important (geo)archeological reference site for the Mesolithic period. Buried fireplaces on the Ullafelsen plateau were dated at 10.9 to 9.5 ka cal BP and demonstrate together with thousands of flint stone artifacts the presence of hunter-gatherers during the Early Holocene. Grazing livestock has been a predominant anthropozoological impact in the Fotsch Valley presumably since the Bronze Age (4.2–2.8 ka). In order to study the human and/or livestock faeces input on the Ullafelsen, w

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27

Bamberger, I., L. Hörtnagl, R. Schnitzhofer, et al. "BVOC fluxes above mountain grassland." Biogeosciences 7, no. 5 (2010): 1413–24. http://dx.doi.org/10.5194/bg-7-1413-2010.

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Abstract. Grasslands comprise natural tropical savannah over managed temperate fields to tundra and cover one quarter of the Earth's land surface. Plant growth, maintenance and decay result in volatile organic compound (VOCs) emissions to the atmosphere. Furthermore, biogenic VOCs (BVOCs) are emitted as a consequence of various environmental stresses including cutting and drying during harvesting. Fluxes of BVOCs were measured with a proton-transfer-reaction-mass-spectrometer (PTR-MS) over temperate mountain grassland in Stubai Valley (Tyrol, Austria) over one growing season (2008). VOC fluxes

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28

Rode, Sören, Delia Rösel, and Bernhard Schulz. "Constraints on the Variscan P-T evolution by EMP Th-U-Pb monazite dating in the polymetamorphic Austroalpine Oetztal-Stubai basement (Eastern Alps)." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 163, no. 1 (2012): 43–67. http://dx.doi.org/10.1127/1860-1804/2012/0163-0043.

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29

Fondevilla, Cristian, M. Àngels Colomer, Federico Fillat, and Ulrike Tappeiner. "Using a new PDP modelling approach for land-use and land-cover change predictions: A case study in the Stubai Valley (Central Alps)." Ecological Modelling 322 (February 2016): 101–14. http://dx.doi.org/10.1016/j.ecolmodel.2015.11.016.

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30

Goločorbin, Stanko. "STATIČKA MKE ANALIZA I ANALIZA OSCILOVANJA STUBA VETROGENERATORA." Zbornik radova Fakulteta tehničkih nauka u Novom Sadu 36, no. 01 (2020): 27–30. http://dx.doi.org/10.24867/11am09golocorbin.

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Stubovi vetrogeneratora su jedni od najkompleksnije opterećenih stubova (tornjeva) koji postoje u građevini. Uzimajući u obzir da promenljiva priroda brzine vetra intenzivno menja opterećenje na stub u vidu ekscentričnog momenta. Cilj ovog istraživanja je dobijanje rezultata statičke MKE analize u vidu napona prema kojoj možemo, shodno najvećim naponima, promeniti dizajn samog modela stuba vetrogeneratora. Takođe istraživanjem oscilacija stuba i pronalaženjem sopstvenih kružnih frekvencija oscilovanja dobijamo zanje o brzini obrtaja rotora koju treba da ograničimo da stub ne bi mogao da uđe u

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31

Goločorbin, Stanko. "STATIČKA MKE ANALIZA I ANALIZA OSCILOVANJA STUBA VETROGENERATORA." Zbornik radova Fakulteta tehničkih nauka u Novom Sadu 36, no. 01 (2020): 27–30. http://dx.doi.org/10.24867/11am09golocorbin.

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Stubovi vetrogeneratora su jedni od najkompleksnije opterećenih stubova (tornjeva) koji postoje u građevini. Uzimajući u obzir da promenljiva priroda brzine vetra intenzivno menja opterećenje na stub u vidu ekscentričnog momenta. Cilj ovog istraživanja je dobijanje rezultata statičke MKE analize u vidu napona prema kojoj možemo, shodno najvećim naponima, promeniti dizajn samog modela stuba vetrogeneratora. Takođe istraživanjem oscilacija stuba i pronalaženjem sopstvenih kružnih frekvencija oscilovanja dobijamo zanje o brzini obrtaja rotora koju treba da ograničimo da stub ne bi mogao da uđe u

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Ruuskanen, T. M., M. Müller, R. Schnitzhofer, et al. "Eddy covariance VOC emission and deposition fluxes above grassland using PTR-TOF." Atmospheric Chemistry and Physics Discussions 10, no. 9 (2010): 21077–108. http://dx.doi.org/10.5194/acpd-10-21077-2010.

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Abstract. Eddy covariance (EC) is the preferable technique for flux measurements since it is the only direct flux determination method. It requires a continuum of high time resolution measurements (e.g. 5–20 Hz). For volatile organic compounds (VOC) soft ionization via proton transfer reaction has proven to be a quantitative method for real time mass spectrometry; here we use a proton transfer reaction time of flight mass spectrometer (PTR-TOF) for 10 Hz EC measurements of full mass spectra up to m/z 315. The mass resolution of the PTR-TOF enabled the identification of chemical formulas and se

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Feng, Zhongyi, Pascal Bohleber, Sven Ebser, et al. "Dating glacier ice of the last millennium by quantum technology." Proceedings of the National Academy of Sciences 116, no. 18 (2019): 8781–86. http://dx.doi.org/10.1073/pnas.1816468116.

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Radiometric dating with 39Ar covers a unique time span and offers key advances in interpreting environmental archives of the last millennium. Although this tracer has been acknowledged for decades, studies so far have been limited by the low abundance and radioactivity, thus requiring huge sample sizes. Atom trap trace analysis, an application of techniques from quantum physics such as laser cooling and trapping, allows us to reduce the sample volume by several orders of magnitude compared with conventional techniques. Here we show that the adaptation of this method to 39Ar is now available fo

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34

Fischer, Andrea, Marc Olefs, and Jakob Abermann. "Glaciers, snow and ski tourism in Austria’s changing climate." Annals of Glaciology 52, no. 58 (2011): 89–96. http://dx.doi.org/10.3189/172756411797252338.

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AbstarctThis study illustrates the relevance of cryospheric changes for, and their impact on, ski tourism in Austria. The results of several case studies on snow reliability, snow production and mass balance in glacier ski resorts in the Ötz and Stubai valleys are summarized. Climate data from Obergurgl (1936ma.s.l.) in the Ötz valley are analyzed with respect to the amount and duration of natural snow cover and the possibility of snow production. A case study on Mittelbergferner focuses on the impacts of glacial recession on a ski resort and possible adaptation measures. From long-term glacie

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Ruuskanen, T. M., M. Müller, R. Schnitzhofer, et al. "Eddy covariance VOC emission and deposition fluxes above grassland using PTR-TOF." Atmospheric Chemistry and Physics 11, no. 2 (2011): 611–25. http://dx.doi.org/10.5194/acp-11-611-2011.

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Abstract. Eddy covariance (EC) is the preferable technique for flux measurements since it is the only direct flux determination method. It requires a continuum of high time resolution measurements (e.g. 5–20 Hz). For volatile organic compounds (VOC) soft ionization via proton transfer reaction has proven to be a quantitative method for real time mass spectrometry; here we use a proton transfer reaction time of flight mass spectrometer (PTR-TOF) for 10 Hz EC measurements of full mass spectra up to m/z 315. The mass resolution of the PTR-TOF enabled the identification of chemical formulas and se

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36

Tenhunen, J., R. Geyer, S. Adiku, et al. "Influences of changing land use and CO2 concentration on ecosystem and landscape level carbon and water balances in mountainous terrain of the Stubai Valley, Austria." Global and Planetary Change 67, no. 1-2 (2009): 29–43. http://dx.doi.org/10.1016/j.gloplacha.2008.12.010.

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Hartl, Lea, Patrick Schmitt, Lilian Schuster, Kay Helfricht, Jakob Abermann, and Fabien Maussion. "Recent observations and glacier modeling point towards near-complete glacier loss in western Austria (Ötztal and Stubai mountain range) if 1.5 °C is not met." Cryosphere 19, no. 3 (2025): 1431–52. https://doi.org/10.5194/tc-19-1431-2025.

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Abstract. Most glaciers in Austria are expected to disappear in the coming decades. The general trend to deglaciation is apparent from observations of past glacier change as well as projections of future glacier evolution in the region. However, the projected timing of ice loss varies considerably between models and data sources. We enhance observations of regional glacier area and volume change with a new inventory for the Ötztal and Stubai range in western Austria and use these data to initialize and calibrate the Open Global Glacier Model (OGGM), generating projections for all glaciers in t

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Kovaleva, Elizaveta, Daniel Harlov, and Urs Klötzli. "Complicated secondary textures in zircon record evolution of the host granitic rocks: Studies from Western Tauern Window and Ötztal-Stubai Crystalline Complex (Eastern Alps, Western Austria)." Lithos 284-285 (July 2017): 381–400. http://dx.doi.org/10.1016/j.lithos.2017.04.018.

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Mair, E., G. Bertoldi, G. Leitinger, S. Della Chiesa, G. Niedrist, and U. Tappeiner. "ESOLIP – estimate of solid and liquid precipitation at sub-daily time resolution by combining snow height and rain gauge measurements." Hydrology and Earth System Sciences Discussions 10, no. 7 (2013): 8683–714. http://dx.doi.org/10.5194/hessd-10-8683-2013.

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Abstract. Measuring precipitation in mountain areas is a demanding task, but essential for hydrological and environmental themes. Especially in small Alpine catchments with short hydrological response, precipitation data with high temporal resolution are required for a better understanding of the hydrological cycle. Since most climate/meteorological stations are situated at the easily accessible bottom of valleys, and the few heated rain gauges installed at higher elevation sites are problematic in winter conditions, an accurate quantification of winter (snow) precipitation at high elevations

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Wu, Donghai, Philippe Ciais, Nicolas Viovy, et al. "Asymmetric responses of primary productivity to altered precipitation simulated by ecosystem models across three long-term grassland sites." Biogeosciences 15, no. 11 (2018): 3421–37. http://dx.doi.org/10.5194/bg-15-3421-2018.

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Abstract. Field measurements of aboveground net primary productivity (ANPP) in temperate grasslands suggest that both positive and negative asymmetric responses to changes in precipitation (P) may occur. Under normal range of precipitation variability, wet years typically result in ANPP gains being larger than ANPP declines in dry years (positive asymmetry), whereas increases in ANPP are lower in magnitude in extreme wet years compared to reductions during extreme drought (negative asymmetry). Whether the current generation of ecosystem models with a coupled carbon–water system in grasslands a

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Meyer, S., J. Leifeld, M. Bahn, and J. Fuhrer. "Free and protected soil organic carbon dynamics respond differently to abandonment of mountain grassland." Biogeosciences Discussions 8, no. 5 (2011): 9943–76. http://dx.doi.org/10.5194/bgd-8-9943-2011.

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Abstract. Land-use change (LUC) and management are among the major driving forces of soil carbon (C) storage. Abandonment of mountain grassland promotes accumulation of aboveground biomass and litter, but related responses of soil organic matter (SOM) dynamics are uncertain. To determine SOM-C turnover we sampled 0–10 cm of soils along land-use gradients (hay meadows, grazed pastures and abandoned grasslands) in the European Alps varying in management intensity at Stubai Valley (MAT: 3 °C, P: 1097 mm) in Austria and Matsch Valley (MAT: 6.6 °C, P: 527 mm) in Italy. We determined C input and dec

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Meyer, S., J. Leifeld, M. Bahn, and J. Fuhrer. "Free and protected soil organic carbon dynamics respond differently to abandonment of mountain grassland." Biogeosciences 9, no. 2 (2012): 853–65. http://dx.doi.org/10.5194/bg-9-853-2012.

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Abstract. Land-use change (LUC) and management are among the major driving forces of soil carbon (C) storage. Abandonment of mountain grassland promotes accumulation of aboveground biomass and litter, but related responses of soil organic matter (SOM) dynamics are uncertain. To determine SOM-C turnover we sampled 0–10 cm of soils in the European Alps along two land-use gradients (hay meadows, grazed pastures and abandoned grasslands) of different management intensity. A first land-use gradient was located at Stubai Valley (MAT: 3 °C, MAP: 1097 mm) in Austria and a second at Matsch Valley (MAT:

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Henig, David. "Pohledy z druhého břehu: transnacionalismus, rituál a sociální změna." Sociální studia / Social Studies 6, no. 1 (2009): 175–92. http://dx.doi.org/10.5817/soc2009-1-175.

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Může v globalizovaném a vzájemně propojeném světě, po postmoderním obratu v sociálních vědách nabídnout antropologie nějakou cestu k porozumění komplexitě lidského života a společnosti? Transnacionální studia poskytují mocný soubor nástrojů k produkci vědění a analýze. Přestože tento přístup přinesl řadu cenných příspěvků a vhledů, provází jej i překážky v podobě určitých předpokladů, jež mohou produkci vědění deformovat. V této studii tvrdím, že transnacionální antropologie může představovat přiměřený způsob produkce vědění o transnacionalismu, kombinující zájem jak o mikropolitiku lidského ž

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Zech, Michael, Marcel Lerch, Marcel Bliedtner, et al. "Revisiting the subalpine Mesolithic site Ullafelsen in the Fotsch Valley, Stubai Alps, Austria – new insights into pedogenesis and landscape evolution from leaf-wax-derived <i>n</i>-alkanes, black carbon and radiocarbon dating." E&G Quaternary Science Journal 70, no. 2 (2021): 171–86. http://dx.doi.org/10.5194/egqsj-70-171-2021.

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Abstract. Archaeological research in high mountain regions has gotten a lot more attention since the discovery of the copper age mummy called “Ötzi” in the Ötztaler Alps in 1991. In the Tyrolean Stubai Alps, the Mesolithic site Ullafelsen at 1869 m a.s.l. (above sea level) close to the recent upper timberline in the Fotsch Valley represents, on the one hand, a very important archaeological reference site and offers, on the other hand, intriguing research questions related to, amongst others, pedogenesis. Given that no biomarkers and stable isotopes have been hitherto investigated, we aimed at

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Pinc, Zdeněk. "Mistr Jan Hus v zápase mezi Kristem a Antikristem." Lidé města 9, no. 2-3/21 (2007): 304–15. https://doi.org/10.14712/12128112.3773.

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Předesílám, že jsem o Janu Husovi nepublikoval řádnou odbornou práci, nepokládám se za husovského badatele a tak jsem na Vašem učeném shromáždění možná spíše omylem. S postavou Jana Husa a jeho dílem jsem se blíže seznámil v době hluboké normalizace na přelomu sedmdesátých a osmdesátých let při práci na studii o Emanuelu Rádlovi, jež pak byla publikována v exilovém pařížském časopise Svědectví. V Rádlově Válce Čechů s Němci (1927) je větší část druhé kapitoly věnována Husovi a Dekretu kutnohorskému a tehdy pro mne znamenala objev, protože se Rádlův výklad výrazně odlišoval od všeho, co jsem se

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Hančil, Jan. "Systém a metody : některé aspekty přenosu Stanislavského systému do Spojených států." Theatralia, no. 2 (2023): 30–58. http://dx.doi.org/10.5817/ty2023-2-4.

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Studie se zaměřuje na přenesení Stanislavského systému do Spojených států prostřednictvím emigrantů z různých souborů a tří emigračních vln a na působení první generace amerických hereckých pedagogů inspirovaných postupy, které emigranti v první polovině 20. století americkým studentům předávali. Autor ve studii shrnuje jak fakta, která jsou dobře známa (například působení American Laboratory Theatre či Group Theatre), tak méně známé linie přenosu formou působení jednotlivých pedagogů, kteří zakládali vlastní herecká studia či školy. Akcentuje vliv Vachtangova, především pozdní fáze jeho divad

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Sokolová, Hana, and Hynek Cígler. "Test cesty: Normativní česká data pro žáky 9. tříd ZŠ až 4. ročníků SŠ." TESTFÓRUM 6, no. 11 (2018): 1–20. http://dx.doi.org/10.5817/tf2018-11-197.

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V předkládané studii jsou uvedena normativní česká data pro neuropsychologickou screeningovou zkoušku Test cesty pro věkovou skupinu dospívajících (15-19 let). Potvrdilo se, že není možné přejímat výsledky Testu cesty z jiného kulturního kontextu. Čeští studenti podali statisticky významně horší výkony ve srovnání s českým manuálem k metodě uváděnými normami ze zahraničí i ve srovnání s daty jiných zahraničních studií. Dále byly identifikovány faktory, které se významně podílejí na výsledku v Testu cesty u skupiny českých adolescentů - typ navštěvované střední školy a ročník studia, v protikla

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Pavlasová, Lenka. "Disertační práce se zaměřením na didaktiku biologie v České republice v letech 2004 – 2013." Scientia in educatione 6, no. 2 (2015): 4–15. http://dx.doi.org/10.14712/18047106.234.

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Disertační práce je důležitým ukazatelem kvality doktorského studia. V předložené studii byl proveden kvalitativní výzkum 19 disertačních prací z didaktiky biologie obhájených v období let 2004–2013 metodou obsahové analýzy. Byly zkoumány tyto ukazatele: oborové téma, stupeň zkoumané školy, metody sběru dat při výzkumu, počet autocitací a jejich kvalita, případný praktický výstup do praxe a jeho charakter. Autory prací byly z 64 % ženy a z 36 % muži. Oborová témata byla zastoupena nevyváženě, některá byla zcela opomíjena (např. biologie hub). V pracích byly zkoumány všechny stupně školy: prepr

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Szymczak Graczyk, Anna. "Metody obliczania studni opuszczanych." Przegląd Budowlany 95, no. 4 (2024): 91–94. http://dx.doi.org/10.5604/01.3001.0054.6393.

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W pracy przedstawiono metody obliczania studniopuszczanych, uwzględniając metody tradycyjne oraz współczesnenumeryczne metody obliczeniowe. Omówione zostały najważniejszezagadnienia, na które należy zwrócić uwagę przy projektowaniustudni, takie jak: zapewnienie studni pogrążalności,w przypadku posadowienia w gruntach nawodnionych, zagwarantowaniestudni stateczności na wypór, zaprojektowanie podwzględem wytrzymałościowym płaszcza studni, noża studni, korkabetonowego studni oraz płyty dennej, jak również uwzględnienietechnologii wykonywania studni.

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Stará, Jana, Tereza Krčmářová, and Juliana Crespo Lopes. "Prožívání státních závěrečných zkoušek studenty a reflexe tohoto prožívání jejich učiteli." Studia paedagogica 29, no. 1 (2025): 107–36. https://doi.org/10.5817/sp2024-1-5.

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Ve studii vycházíme z analýz odpovědí na uzavřené i otevřené otázky dotazníkového šetření provedeného na vzorku 50 studentů učitelství pro 1. stupeň ZŠ na Pedagogické fakultě Univerzity Karlovy bezprostředně po vykonání státní závěrečné zkoušky (SZZ). Vedle zkoumání prožívání SZZ studenty jsme se zaměřili také na to, jak toto prožívání reflektovali jejich zkoušející, a to prostřednictvím analýzy skupinových rozhovorů s 12 vysokoškolskými učiteli. Výsledky ukazují, že většina studentů při SZZ prožívala nervozitu a strach, přičemž značnou část z nich se podařilo examinátorům uklidnit. Studenti p

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