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
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/57299

id CONICETDig_babdeca38fa841cabdb604dc980216b0
oai_identifier_str oai:ri.conicet.gov.ar:11336/57299
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling 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)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
_version_ 1842269162570776576
score 13.13397