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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

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • 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