The geomorphological effectiveness of extreme meteorological phenomena on flysch slopes

2008
journal article
article
dc.abstract.enExtreme events tend to cause large-scale slope system changes. During the last ten years, a series of extreme meteorological events caused considerable transformation of the slopes and valleys in various parts of the Carpathian Mountains. This paper presents the geomorphological effects of extreme rainfall and thaw events on the slopes of two catchments: the Łososina catchment (Beskid Wyspowy) and the Hoczewka catchment with an area around the Solińskie Lake (Bieszczady Niskie). The bulk of the discussion concerns a study carried out in the Łososina catchment after three separate extreme events that were followed by a considerable transformation of the slopes due to landsliding. The studies carried out in the Bieszczady Range, where a single extreme event produced only spatially limited effects, were mainly used for comparison. I he disparity between the responses of the two slope systems was a result of differences between the systems themselves, including their geology, geomorphology and landslide record, and of the difference in the scale of the extreme events.pl
dc.affiliationWydział Biologii i Nauk o Ziemi : Instytut Geografii i Gospodarki Przestrzennejpl
dc.contributor.authorGorczyca, Elżbieta - 128116 pl
dc.date.accession2020-02-25pl
dc.date.accessioned2020-02-25T10:27:36Z
dc.date.available2020-02-25T10:27:36Z
dc.date.issued2008pl
dc.date.openaccess0
dc.description.accesstimew momencie opublikowania
dc.description.additionalBibliogr. s. 26-27pl
dc.description.physical17-27pl
dc.description.versionostateczna wersja wydawcy
dc.description.volume6pl
dc.identifier.eissn2081-5980pl
dc.identifier.issn1429-799Xpl
dc.identifier.projectROD UJ / OPpl
dc.identifier.urihttps://ruj.uj.edu.pl/xmlui/handle/item/150008
dc.identifier.weblinkhttp://geoinfo.amu.edu.pl/sgp/LA/LA06/a017_GORCZYCA.pdfpl
dc.languageengpl
dc.language.containerengpl
dc.rightsUdzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 3.0 Polska*
dc.rights.licenceCC-BY-NC-ND
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/legalcode*
dc.share.typeotwarte czasopismo
dc.subject.enextreme eventspl
dc.subject.enheavy rainfallpl
dc.subject.enlandsliespl
dc.subject.enllysch slopespl
dc.subject.enBeskid Wyspowypl
dc.subject.enBieszczady Niskiepl
dc.subtypeArticlepl
dc.titleThe geomorphological effectiveness of extreme meteorological phenomena on flysch slopespl
dc.title.journalLandform Analysispl
dc.typeJournalArticlepl
dspace.entity.typePublication
dc.abstract.enpl
Extreme events tend to cause large-scale slope system changes. During the last ten years, a series of extreme meteorological events caused considerable transformation of the slopes and valleys in various parts of the Carpathian Mountains. This paper presents the geomorphological effects of extreme rainfall and thaw events on the slopes of two catchments: the Łososina catchment (Beskid Wyspowy) and the Hoczewka catchment with an area around the Solińskie Lake (Bieszczady Niskie). The bulk of the discussion concerns a study carried out in the Łososina catchment after three separate extreme events that were followed by a considerable transformation of the slopes due to landsliding. The studies carried out in the Bieszczady Range, where a single extreme event produced only spatially limited effects, were mainly used for comparison. I he disparity between the responses of the two slope systems was a result of differences between the systems themselves, including their geology, geomorphology and landslide record, and of the difference in the scale of the extreme events.
dc.affiliationpl
Wydział Biologii i Nauk o Ziemi : Instytut Geografii i Gospodarki Przestrzennej
dc.contributor.authorpl
Gorczyca, Elżbieta - 128116
dc.date.accessionpl
2020-02-25
dc.date.accessioned
2020-02-25T10:27:36Z
dc.date.available
2020-02-25T10:27:36Z
dc.date.issuedpl
2008
dc.date.openaccess
0
dc.description.accesstime
w momencie opublikowania
dc.description.additionalpl
Bibliogr. s. 26-27
dc.description.physicalpl
17-27
dc.description.version
ostateczna wersja wydawcy
dc.description.volumepl
6
dc.identifier.eissnpl
2081-5980
dc.identifier.issnpl
1429-799X
dc.identifier.projectpl
ROD UJ / OP
dc.identifier.uri
https://ruj.uj.edu.pl/xmlui/handle/item/150008
dc.identifier.weblinkpl
http://geoinfo.amu.edu.pl/sgp/LA/LA06/a017_GORCZYCA.pdf
dc.languagepl
eng
dc.language.containerpl
eng
dc.rights*
Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 3.0 Polska
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.enpl
extreme events
dc.subject.enpl
heavy rainfall
dc.subject.enpl
landslies
dc.subject.enpl
llysch slopes
dc.subject.enpl
Beskid Wyspowy
dc.subject.enpl
Bieszczady Niskie
dc.subtypepl
Article
dc.titlepl
The geomorphological effectiveness of extreme meteorological phenomena on flysch slopes
dc.title.journalpl
Landform Analysis
dc.typepl
JournalArticle
dspace.entity.type
Publication
Affiliations

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