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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F14%3A10281683%21RIV15-MSM-11310___
rdf:type
n7:Vysledek skos:Concept
dcterms:description
The Cordillera Blanca (Ancash region, Peru) is the most heavily glacierized tropical range in the world. Due to the global climate change, the retreat and thinning of most of the glaciers has recently increased. Rapid geomorphic changes, especially direct and indirect slope movements, are closely connected with the changing environment. Glacier retreat also leads to the formation and development of all types of potentially hazardous glacial lakes. A sudden water release from a glacial lake irrespective of its cause is called a glacial lake outburst flood (GLOF). The hazard of GLOF is strongly connected with dynamic slope movements (ice-and rock-falls; landslides of steep moraine slopes). About 80 % of the GLOFs in the Cordillera Blanca since the end of the Little Ice Age were caused by dynamic slope movements into the lake. The released water has a high erosion and sediment transport potential and can easily transform into various types of flow movements (e.g. debris or mud flows). These are highly hazardous and significant landscaping processes, by which the high mountainous environment evolves. Using the DesInventar database for the period from 1971 to 2009, debris flows (locally known as aluvión) have been evaluated as the most frequent type of natural hazard in the Ancash region. Several valleys in the Cordillera Blanca are currently being studied, using flood modelling, geomorphological mapping and calculation of slope stability in moraines. Conditions leading to slope movements on moraines include not only moraine properties, such as grain size and sediment structure, but also water infiltration from adjacent slopes. The Cordillera Blanca (Ancash region, Peru) is the most heavily glacierized tropical range in the world. Due to the global climate change, the retreat and thinning of most of the glaciers has recently increased. Rapid geomorphic changes, especially direct and indirect slope movements, are closely connected with the changing environment. Glacier retreat also leads to the formation and development of all types of potentially hazardous glacial lakes. A sudden water release from a glacial lake irrespective of its cause is called a glacial lake outburst flood (GLOF). The hazard of GLOF is strongly connected with dynamic slope movements (ice-and rock-falls; landslides of steep moraine slopes). About 80 % of the GLOFs in the Cordillera Blanca since the end of the Little Ice Age were caused by dynamic slope movements into the lake. The released water has a high erosion and sediment transport potential and can easily transform into various types of flow movements (e.g. debris or mud flows). These are highly hazardous and significant landscaping processes, by which the high mountainous environment evolves. Using the DesInventar database for the period from 1971 to 2009, debris flows (locally known as aluvión) have been evaluated as the most frequent type of natural hazard in the Ancash region. Several valleys in the Cordillera Blanca are currently being studied, using flood modelling, geomorphological mapping and calculation of slope stability in moraines. Conditions leading to slope movements on moraines include not only moraine properties, such as grain size and sediment structure, but also water infiltration from adjacent slopes.
dcterms:title
Natural Hazards in the Cordillera Blanca of Peru During the Time of Global Climate Change Natural Hazards in the Cordillera Blanca of Peru During the Time of Global Climate Change
skos:prefLabel
Natural Hazards in the Cordillera Blanca of Peru During the Time of Global Climate Change Natural Hazards in the Cordillera Blanca of Peru During the Time of Global Climate Change
skos:notation
RIV/00216208:11310/14:10281683!RIV15-MSM-11310___
n3:aktivita
n4:S n4:P n4:I
n3:aktivity
I, P(GAP209/11/1000), S
n3:dodaniDat
n15:2015
n3:domaciTvurceVysledku
n10:3932648 n10:8921768
n3:druhVysledku
n12:C
n3:duvernostUdaju
n19:S
n3:entitaPredkladatele
n20:predkladatel
n3:idSjednocenehoVysledku
31717
n3:idVysledku
RIV/00216208:11310/14:10281683
n3:jazykVysledku
n13:eng
n3:klicovaSlova
climate change; slope movements; natural hazards
n3:klicoveSlovo
n5:natural%20hazards n5:slope%20movements n5:climate%20change
n3:kontrolniKodProRIV
[14E58F91AC94]
n3:mistoVydani
Switzerland
n3:nazevEdiceCisloSvazku
Neuveden
n3:nazevZdroje
Landslide Science for a Safer Geoenvironment
n3:obor
n17:DE
n3:pocetDomacichTvurcuVysledku
2
n3:pocetStranKnihy
493
n3:pocetTvurcuVysledku
4
n3:projekt
n6:GAP209%2F11%2F1000
n3:rokUplatneniVysledku
n15:2014
n3:tvurceVysledku
Novotný, Jan Vilímek, Vít Emmer, Adam Klimeš, Jan
s:numberOfPages
6
n21:doi
10.1007/978-3-319-04999-1_35
n16:hasPublisher
Springer-Verlag
n18:isbn
978-3-319-04999-1
n14:organizacniJednotka
11310