cris.boxmetadata.label.title
Three Recent and Lesser-Known Glacier-Related Flood Mechanisms in High Mountain Environments
cris.boxmetadata.label.dateissued
01 browse.startsWith.months.january 2022
cris.boxmetadata.label.accesslevel
open access
cris.boxmetadata.label.resourcetype
journal article
cris.boxmetadata.label.authors
Byers A.C.
Shugar D.H.
Chand M.B.
Shrestha M.
Rounce D.R.
Watanabe T.
Civil Engineer and Consultant
cris.boxmetadata.label.publisher
International Mountain Society
cris.boxmetadata.label.abstract
Glacial lake outburst floods, and specifically those triggered by avalanche-induced seiche waves, have been studied in considerable detail during the past several decades. Less attention has been given to other cryospheric flood phenomena, which include floods sourced primarily from englacial conduits, permafrost-linked rockfall and avalanches, and earthquake-Triggered glacial lake floods. The article reviews examples of each phenomenon, based on field sampling and laboratory analyses, that have occurred in the Nepal Himalaya during the past decade, drawing parallels with similar events in other countries throughout the high mountain world. In most cases, the frequency of these events appears to be increasing globally, as is their potential to inflict significant damage downstream. We argue that each type of glacier flood requires more detailed study to develop the most effective prevention, mitigation, and adaptation approaches possible. Such studies will most likely be strengthened if they include a reconnaissance of the event as soon after its occurrence as possible, along with the participation, insights, and experience of local people, in addition to the use of increasingly powerful remote sensing technologies. How scientists can more quickly and effectively share the results of their research with decision-makers, and how decision-makers and governments can deliver more timely mitigation programs, are areas that also require further strengthening.
cris.boxmetadata.label.citationstartpage
A12
cris.boxmetadata.label.citationendpage
A22
cris.boxmetadata.label.volume
42
cris.boxmetadata.label.issue
2
cris.boxmetadata.label.language
English
cris.boxmetadata.label.ocdeknowledgeArea
Investigación climática Oceanografía, Hidrología, Recursos hídricos
cris.boxmetadata.label.doi
cris.boxmetadata.label.scopusidentifier
2-s2.0-85131005909
cris.boxmetadata.label.source
Mountain Research and Development
cris.boxmetadata.label.containerissn
02764741
cris.boxmetadata.label.sponsor
The authors acknowledge the support of the National Science Foundation Dynamics of Coupled Natural and Human Systems (NSF-CNH) Program (award no. 1516912) and the National Geographic Society for their partial support of field and travel costs during the field phases of each glacier event covered in the article. Dan Shugar was supported by NSERC 2020-04207, for which he extends his appreciation. Special thanks are extended to the lodge owners and local communities of the Sagarmatha and Makalu-Barun National Park and Buffer Zones, eastern Nepal, for their generous provision of information related to both historic and recent catastrophic events in their home regions.
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