Snow avalanche activity in Żleb Żandarmerii in a time of climate change (Tatra Mts., Poland)
- Autores
- Gadek, Bogdan; Kaczka, Ryszard J.; Raczkowska, Zofia; Rojan, Elzbieta; Casteller, Alejandro; Bebi, Peter
- Año de publicación
- 2017
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- This paper reports from a survey of the occurrence of large avalanches in Żleb Żandarmerii. This couloir is known to be one of the most hazardous avalanche paths in the Tatra Mountains and has one of the longest histories of avalanche observation. This survey looked at the runout distance, return period, dynamics and geoecological implications of avalanches in the context of current climate change. The study took advantage of the longest record of meteorological data available in the Tatra Mountains, as well as archival avalanche observations, topographical maps, orthophotomaps and a high-resolution digital terrain model. Avalanche data were obtained using geomorphological and dendrogeomorphic methods and through modelling with the RAMMS numerical avalanche dynamics simulation software. The largest avalanches reach the foot of its counter slope. Their length, release volume, flow velocity and pressure can exceed respectively 1000 m, 80 000 m3, 45 m/s and 600 kPa. The results of our study suggest that current climate warming has been accompanied by thinning and shortening of the duration of snow cover, as well as by an upward expansion of the timberline (including in the large-avalanche runout zones) of up to 80 m since the mid-1920s. No distinct temporal trend was identified in the large avalanche return period since 1909, but their mass and intensity have declined. Forests and timberline expansion were found to have no influence on the extent of the avalanches in our study, while ground relief could determine both their downward extent and lateral expansion.
Fil: Gadek, Bogdan. University of Silesi; Polonia
Fil: Kaczka, Ryszard J.. University of Silesi; Polonia
Fil: Raczkowska, Zofia. Polish Academy of Sciences. Institute of Geography and Spatial Organization; Polonia
Fil: Rojan, Elzbieta. Uniwersytet Warszawski; Argentina
Fil: Casteller, Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina. Institute for Snow and Avalanche Research; Suiza
Fil: Bebi, Peter. Institute for Snow and Avalanche Research; Suiza - Materia
-
Climate Change
Snow Avalanches
Tatra Mountains - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/57299
Ver los metadatos del registro completo
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Snow avalanche activity in Żleb Żandarmerii in a time of climate change (Tatra Mts., Poland)Gadek, BogdanKaczka, Ryszard J.Raczkowska, ZofiaRojan, ElzbietaCasteller, AlejandroBebi, PeterClimate ChangeSnow AvalanchesTatra Mountainshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1This paper reports from a survey of the occurrence of large avalanches in Żleb Żandarmerii. This couloir is known to be one of the most hazardous avalanche paths in the Tatra Mountains and has one of the longest histories of avalanche observation. This survey looked at the runout distance, return period, dynamics and geoecological implications of avalanches in the context of current climate change. The study took advantage of the longest record of meteorological data available in the Tatra Mountains, as well as archival avalanche observations, topographical maps, orthophotomaps and a high-resolution digital terrain model. Avalanche data were obtained using geomorphological and dendrogeomorphic methods and through modelling with the RAMMS numerical avalanche dynamics simulation software. The largest avalanches reach the foot of its counter slope. Their length, release volume, flow velocity and pressure can exceed respectively 1000 m, 80 000 m3, 45 m/s and 600 kPa. The results of our study suggest that current climate warming has been accompanied by thinning and shortening of the duration of snow cover, as well as by an upward expansion of the timberline (including in the large-avalanche runout zones) of up to 80 m since the mid-1920s. No distinct temporal trend was identified in the large avalanche return period since 1909, but their mass and intensity have declined. Forests and timberline expansion were found to have no influence on the extent of the avalanches in our study, while ground relief could determine both their downward extent and lateral expansion.Fil: Gadek, Bogdan. University of Silesi; PoloniaFil: Kaczka, Ryszard J.. University of Silesi; PoloniaFil: Raczkowska, Zofia. Polish Academy of Sciences. Institute of Geography and Spatial Organization; PoloniaFil: Rojan, Elzbieta. Uniwersytet Warszawski; ArgentinaFil: Casteller, Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina. Institute for Snow and Avalanche Research; SuizaFil: Bebi, Peter. Institute for Snow and Avalanche Research; SuizaElsevier Science2017-11info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/57299Gadek, Bogdan; Kaczka, Ryszard J.; Raczkowska, Zofia; Rojan, Elzbieta; Casteller, Alejandro; et al.; Snow avalanche activity in Żleb Żandarmerii in a time of climate change (Tatra Mts., Poland); Elsevier Science; Catena; 158; 11-2017; 201-2120341-8162CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.catena.2017.07.005info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0341816217302382info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:52:29Zoai:ri.conicet.gov.ar:11336/57299instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 09:52:30.041CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Snow avalanche activity in Żleb Żandarmerii in a time of climate change (Tatra Mts., Poland) |
title |
Snow avalanche activity in Żleb Żandarmerii in a time of climate change (Tatra Mts., Poland) |
spellingShingle |
Snow avalanche activity in Żleb Żandarmerii in a time of climate change (Tatra Mts., Poland) Gadek, Bogdan Climate Change Snow Avalanches Tatra Mountains |
title_short |
Snow avalanche activity in Żleb Żandarmerii in a time of climate change (Tatra Mts., Poland) |
title_full |
Snow avalanche activity in Żleb Żandarmerii in a time of climate change (Tatra Mts., Poland) |
title_fullStr |
Snow avalanche activity in Żleb Żandarmerii in a time of climate change (Tatra Mts., Poland) |
title_full_unstemmed |
Snow avalanche activity in Żleb Żandarmerii in a time of climate change (Tatra Mts., Poland) |
title_sort |
Snow avalanche activity in Żleb Żandarmerii in a time of climate change (Tatra Mts., Poland) |
dc.creator.none.fl_str_mv |
Gadek, Bogdan Kaczka, Ryszard J. Raczkowska, Zofia Rojan, Elzbieta Casteller, Alejandro Bebi, Peter |
author |
Gadek, Bogdan |
author_facet |
Gadek, Bogdan Kaczka, Ryszard J. Raczkowska, Zofia Rojan, Elzbieta Casteller, Alejandro Bebi, Peter |
author_role |
author |
author2 |
Kaczka, Ryszard J. Raczkowska, Zofia Rojan, Elzbieta Casteller, Alejandro Bebi, Peter |
author2_role |
author author author author author |
dc.subject.none.fl_str_mv |
Climate Change Snow Avalanches Tatra Mountains |
topic |
Climate Change Snow Avalanches Tatra Mountains |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
This paper reports from a survey of the occurrence of large avalanches in Żleb Żandarmerii. This couloir is known to be one of the most hazardous avalanche paths in the Tatra Mountains and has one of the longest histories of avalanche observation. This survey looked at the runout distance, return period, dynamics and geoecological implications of avalanches in the context of current climate change. The study took advantage of the longest record of meteorological data available in the Tatra Mountains, as well as archival avalanche observations, topographical maps, orthophotomaps and a high-resolution digital terrain model. Avalanche data were obtained using geomorphological and dendrogeomorphic methods and through modelling with the RAMMS numerical avalanche dynamics simulation software. The largest avalanches reach the foot of its counter slope. Their length, release volume, flow velocity and pressure can exceed respectively 1000 m, 80 000 m3, 45 m/s and 600 kPa. The results of our study suggest that current climate warming has been accompanied by thinning and shortening of the duration of snow cover, as well as by an upward expansion of the timberline (including in the large-avalanche runout zones) of up to 80 m since the mid-1920s. No distinct temporal trend was identified in the large avalanche return period since 1909, but their mass and intensity have declined. Forests and timberline expansion were found to have no influence on the extent of the avalanches in our study, while ground relief could determine both their downward extent and lateral expansion. Fil: Gadek, Bogdan. University of Silesi; Polonia Fil: Kaczka, Ryszard J.. University of Silesi; Polonia Fil: Raczkowska, Zofia. Polish Academy of Sciences. Institute of Geography and Spatial Organization; Polonia Fil: Rojan, Elzbieta. Uniwersytet Warszawski; Argentina Fil: Casteller, Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina. Institute for Snow and Avalanche Research; Suiza Fil: Bebi, Peter. Institute for Snow and Avalanche Research; Suiza |
description |
This paper reports from a survey of the occurrence of large avalanches in Żleb Żandarmerii. This couloir is known to be one of the most hazardous avalanche paths in the Tatra Mountains and has one of the longest histories of avalanche observation. This survey looked at the runout distance, return period, dynamics and geoecological implications of avalanches in the context of current climate change. The study took advantage of the longest record of meteorological data available in the Tatra Mountains, as well as archival avalanche observations, topographical maps, orthophotomaps and a high-resolution digital terrain model. Avalanche data were obtained using geomorphological and dendrogeomorphic methods and through modelling with the RAMMS numerical avalanche dynamics simulation software. The largest avalanches reach the foot of its counter slope. Their length, release volume, flow velocity and pressure can exceed respectively 1000 m, 80 000 m3, 45 m/s and 600 kPa. The results of our study suggest that current climate warming has been accompanied by thinning and shortening of the duration of snow cover, as well as by an upward expansion of the timberline (including in the large-avalanche runout zones) of up to 80 m since the mid-1920s. No distinct temporal trend was identified in the large avalanche return period since 1909, but their mass and intensity have declined. Forests and timberline expansion were found to have no influence on the extent of the avalanches in our study, while ground relief could determine both their downward extent and lateral expansion. |
publishDate |
2017 |
dc.date.none.fl_str_mv |
2017-11 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/57299 Gadek, Bogdan; Kaczka, Ryszard J.; Raczkowska, Zofia; Rojan, Elzbieta; Casteller, Alejandro; et al.; Snow avalanche activity in Żleb Żandarmerii in a time of climate change (Tatra Mts., Poland); Elsevier Science; Catena; 158; 11-2017; 201-212 0341-8162 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/57299 |
identifier_str_mv |
Gadek, Bogdan; Kaczka, Ryszard J.; Raczkowska, Zofia; Rojan, Elzbieta; Casteller, Alejandro; et al.; Snow avalanche activity in Żleb Żandarmerii in a time of climate change (Tatra Mts., Poland); Elsevier Science; Catena; 158; 11-2017; 201-212 0341-8162 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.catena.2017.07.005 info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0341816217302382 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Elsevier Science |
publisher.none.fl_str_mv |
Elsevier Science |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
reponame_str |
CONICET Digital (CONICET) |
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CONICET Digital (CONICET) |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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13.13397 |