Zobrazeno 1 - 10
of 27
pro vyhledávání: '"Moritz Altmann"'
Autor:
Moritz Altmann, Katharina Ramskogler, Sebastian Mikolka-Flöry, Madlene Pfeiffer, Florian Haas, Tobias Heckmann, Jakob Rom, Fabian Fleischer, Toni Himmelstoß, Norbert Pfeifer, Camillo Ressl, Erich Tasser, Michael Becht
Publikováno v:
Geosciences, Vol 13, Iss 4, p 95 (2023)
Aerial photographs of the European Alps usually only reach back to the middle of the 20th century, which limits the time span of corresponding studies that quantitatively analyse long-term surface changes of proglacial areas using georeferenced ortho
Externí odkaz:
https://doaj.org/article/1289a21cb3564560a48376420b7bf04c
Autor:
Jakob Rom, Florian Haas, Florentin Hofmeister, Fabian Fleischer, Moritz Altmann, Madlene Pfeiffer, Tobias Heckmann, Michael Becht
Publikováno v:
Geosciences, Vol 13, Iss 4, p 100 (2023)
High-quality in situ measurements are essential for hazard assessment of debris flow events. However, precise data on debris flow triggering thresholds, accumulation volumes and spatial characteristics of large-scale events on catchment scale are sca
Externí odkaz:
https://doaj.org/article/ccab366330874ae29e24a1cce0f3025e
Publikováno v:
Remote Sensing, Vol 15, Iss 6, p 1472 (2023)
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
Externí odkaz:
https://doaj.org/article/94174483b958434790b24fb7199bc14e
Autor:
Jakob Rom, Florian Haas, Tobias Heckmann, Fabian Dremel, Fabian Fleischer, Moritz Altmann, Manuel Stark, Michael Becht
Publikováno v:
Geografiska Annaler: Series A, Physical Geography. 105:47-63
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6d8f759cafc71d0f99e13e3ca32f0f21
https://doi.org/10.1080/04353676.2023.2187531
https://doi.org/10.1080/04353676.2023.2187531
Publikováno v:
Permafrost and Periglacial Processes. 34:3-21
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d14a3318f6288eb5cd6adb27afc00023
https://doi.org/10.1002/ppp.2178
https://doi.org/10.1002/ppp.2178
Deglaciation in high mountain areas signifies the transition from glacial to periglacial conditioned landscapes. Due to the reduced melt rate of debris coved glacier ice, these parts of the glacier might persist long after the surrounding glacier has
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8b6c71d6552631da31796c374c278055
https://doi.org/10.5194/egusphere-egu23-11971
https://doi.org/10.5194/egusphere-egu23-11971
Autor:
Toni Himmelstoss, Sarah Betz-Nutz, Jakob Rom, Moritz Altmann, Fabian Fleischer, Florian Haas, Michael Becht, Tobias Heckmann
Sediment connectivity is defined as the potential of a catchment to route material through itself. It is a system property that regulates the propagation of geomorphic changes through a catchment and is therefore a factor of its sensitivity to climat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d502e36ab63a2a768a0a428990999025
https://doi.org/10.5194/egusphere-egu23-13468
https://doi.org/10.5194/egusphere-egu23-13468
Autor:
Jakob Rom, Florian Haas, Florentin Hofmeister, Tobias Heckmann, Moritz Altmann, Fabian Fleischer, Madlene Pfeiffer, Michael Becht
In order to calibrate and validate debris flow models, high precision in situ measurements are essential. However, it is quite difficult to acquire detailed information about debris flows, as they only rarely occur during exceptional high precipitati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b21e6ce614969618f06a3eb2ec5dd5bb
https://doi.org/10.5194/egusphere-egu23-6251
https://doi.org/10.5194/egusphere-egu23-6251
Autor:
Sarah Betz-Nutz, Toni Himmelstoß, Moritz Altmann, Jakob Rom, Fabian Fleischer, Florian Haas, Michael Becht, Tobias Heckmann
The system of proglacial streams in the Alps has experienced significant changes since the end of the Little Ice Age. Previous studies showed different patterns of aggradation and degradation in proglacial channels over time. This leads to the questi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7159aad0d7de772a681818ae5abcd80c
https://doi.org/10.5194/egusphere-egu23-14322
https://doi.org/10.5194/egusphere-egu23-14322
Autor:
Moritz Altmann, Florian Haas, Jakob Rom, Fabian Fleischer, Tobias Heckmann, Camillo Ressl, Michael Becht
Since the end of the Little Ice Age around 1850, global warming has led to rapid landscape changes, especially in high mountain areas. The ongoing glacier melt leads to an expansion of the LIA glacier forefields, so-called proglacial areas. The expos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3fd22c529d3edad7bebf0f71d726de9d
https://doi.org/10.5194/egusphere-egu23-2715
https://doi.org/10.5194/egusphere-egu23-2715