Conditions and morphogenetic role of the 2018 and 2021 debris flows in Starorobociański Cirque, Western Tatra Mts.

2023
journal article
article
dc.abstract.enIn this study we used geomorphologic mapping, precipitation analysis and archival photomaps to study debris flows in the Starorobociański Cirque, which were renewed in 2018 and 2021. Debris flow in 2021 was most likely the largest single flow recorded in the Polish Western Tatras in the twenty first century. It reached a length of about 870 m and it covered an area of 0.62 to 0.65 ha. We set July 14, 2021, as the date of debris flow initiation and 52.1 $mm·d^{−1}$ as its threshold value. This is one of the lowest values provided in the literature for such flows in the Western Tatra Mts. On the contrary, debris flow which occurred July 18, 2018 was linked to threshold value of 150.5 $mm·d^{−1}$. On the basis of former debris flow occurrence as well as precipitation analysis we interpret the appearance of debris flow in 2021 as an effect of short and intense rainfall.
dc.affiliationSzkoła Doktorska Nauk Ścisłych i Przyrodniczych
dc.affiliationWydział Geografii i Geologii : Instytut Geografii i Gospodarki Przestrzennej
dc.contributor.authorSiemek, Dawid - 454407
dc.contributor.authorGorczyca, Elżbieta - 128116
dc.date.accession2024-04-16
dc.date.accessioned2024-04-17T10:08:39Z
dc.date.available2024-04-17T10:08:39Z
dc.date.issued2023
dc.date.openaccess0
dc.description.accesstimew momencie opublikowania
dc.description.additionalBibliogr. s. 74-75
dc.description.physical63-75
dc.description.versionostateczna wersja wydawcy
dc.description.volume42
dc.identifier.doi10.12657/landfana-042-005
dc.identifier.eissn2081-5980
dc.identifier.issn1429-799X
dc.identifier.urihttps://ruj.uj.edu.pl/handle/item/328969
dc.identifier.weblinkhttp://geoinfo.amu.edu.pl/sgp/LA/LA42/landfana-042-005.pdf
dc.languageeng
dc.language.containereng
dc.rightsUdzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 3.0
dc.rights.licenceCC-BY-NC-ND
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/legalcode
dc.share.typeotwarte czasopismo
dc.subject.endebris flow
dc.subject.enrainfall threshold
dc.subject.enStarorobociańska Valley
dc.subject.enWestern Tatra Mts.
dc.subtypeArticle
dc.titleConditions and morphogenetic role of the 2018 and 2021 debris flows in Starorobociański Cirque, Western Tatra Mts.
dc.title.journalLandform Analysis
dc.typeJournalArticle
dspace.entity.typePublicationen
dc.abstract.en
In this study we used geomorphologic mapping, precipitation analysis and archival photomaps to study debris flows in the Starorobociański Cirque, which were renewed in 2018 and 2021. Debris flow in 2021 was most likely the largest single flow recorded in the Polish Western Tatras in the twenty first century. It reached a length of about 870 m and it covered an area of 0.62 to 0.65 ha. We set July 14, 2021, as the date of debris flow initiation and 52.1 $mm·d^{−1}$ as its threshold value. This is one of the lowest values provided in the literature for such flows in the Western Tatra Mts. On the contrary, debris flow which occurred July 18, 2018 was linked to threshold value of 150.5 $mm·d^{−1}$. On the basis of former debris flow occurrence as well as precipitation analysis we interpret the appearance of debris flow in 2021 as an effect of short and intense rainfall.
dc.affiliation
Szkoła Doktorska Nauk Ścisłych i Przyrodniczych
dc.affiliation
Wydział Geografii i Geologii : Instytut Geografii i Gospodarki Przestrzennej
dc.contributor.author
Siemek, Dawid - 454407
dc.contributor.author
Gorczyca, Elżbieta - 128116
dc.date.accession
2024-04-16
dc.date.accessioned
2024-04-17T10:08:39Z
dc.date.available
2024-04-17T10:08:39Z
dc.date.issued
2023
dc.date.openaccess
0
dc.description.accesstime
w momencie opublikowania
dc.description.additional
Bibliogr. s. 74-75
dc.description.physical
63-75
dc.description.version
ostateczna wersja wydawcy
dc.description.volume
42
dc.identifier.doi
10.12657/landfana-042-005
dc.identifier.eissn
2081-5980
dc.identifier.issn
1429-799X
dc.identifier.uri
https://ruj.uj.edu.pl/handle/item/328969
dc.identifier.weblink
http://geoinfo.amu.edu.pl/sgp/LA/LA42/landfana-042-005.pdf
dc.language
eng
dc.language.container
eng
dc.rights
Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 3.0
dc.rights.licence
CC-BY-NC-ND
dc.rights.uri
http://creativecommons.org/licenses/by-nc-nd/3.0/legalcode
dc.share.type
otwarte czasopismo
dc.subject.en
debris flow
dc.subject.en
rainfall threshold
dc.subject.en
Starorobociańska Valley
dc.subject.en
Western Tatra Mts.
dc.subtype
Article
dc.title
Conditions and morphogenetic role of the 2018 and 2021 debris flows in Starorobociański Cirque, Western Tatra Mts.
dc.title.journal
Landform Analysis
dc.type
JournalArticle
dspace.entity.typeen
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