Can a dam type of an alpine lake be derived from lake geometry? A negative result
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F21%3A00542595" target="_blank" >RIV/86652079:_____/21:00542595 - isvavai.cz</a>
Alternative codes found
RIV/60460709:41330/21:87011
Result on the web
<a href="https://link.springer.com/content/pdf/10.1007/s11629-020-6003-9.pdf" target="_blank" >https://link.springer.com/content/pdf/10.1007/s11629-020-6003-9.pdf</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s11629-020-6003-9" target="_blank" >10.1007/s11629-020-6003-9</a>
Alternative languages
Result language
angličtina
Original language name
Can a dam type of an alpine lake be derived from lake geometry? A negative result
Original language description
Glacial lake outburst floods (GLOFs) represent one of the most serious hazard and risk in deglaciating high mountain regions worldwide and the need for GLOF hazard and risk assessment is apparent. As a consequence, numerous region- and nation-wide GLOF assessment studies have been published recently. These studies cover large areas and consider hundreds to thousands of lakes, prioritizing the hazard posed by them. Clearly, certain simplification is required for executing such studies, often resulting in neglecting qualitative characteristics which would need manual assignment. Different lake dam types (e.g., bedrock-dammed, moraine-dammed) are often not distinguished, despite they control GLOF mechanism (dam overtopping/dam breach) and thus GLOF magnitude. In this study, we explore the potential of easily measurable quantitative characteristics and four ratios to approximate the lake dam type. Our dataset of 851 lakes of the Cordillera Blanca suggests that while variances and means of these characteristics of individual lake types differ significantly (F-test, t-test), value distribution of different geometrical properties can't be used for the originally proposed purpose along the spectra. The only promising results are obtained for extreme values (selected bins) of the ratios. For instance, the low width to length ratio indicates likely moraine-dammed lake while the high value of ratio indicating round-shape of the lake indicates increased likelihood of bedrock-dammed lake. Overall, we report a negative result of our experiment since there are negligible differences of relative frequencies in most of the bins along the spectra.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10511 - Environmental sciences (social aspects to be 5.7)
Result continuities
Project
<a href="/en/project/LO1415" target="_blank" >LO1415: CzechGlobe 2020 – Development of the Centre of Global Climate Change Impacts Studies</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2021
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Journal of Mountain Science
ISSN
1672-6316
e-ISSN
1993-0321
Volume of the periodical
18
Issue of the periodical within the volume
3
Country of publishing house
CN - CHINA
Number of pages
8
Pages from-to
614-621
UT code for WoS article
000627411100004
EID of the result in the Scopus database
2-s2.0-85102372596