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Ski piste snow ablation versus potential infiltration (Veporic Unit, Western Carpathians)

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43310%2F20%3A43917606" target="_blank" >RIV/62156489:43310/20:43917606 - isvavai.cz</a>

  • Result on the web

    <a href="https://doi.org/10.2478/johh-2019-0026" target="_blank" >https://doi.org/10.2478/johh-2019-0026</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.2478/johh-2019-0026" target="_blank" >10.2478/johh-2019-0026</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Ski piste snow ablation versus potential infiltration (Veporic Unit, Western Carpathians)

  • Original language description

    Snow production results in high volume of snow that is remaining on the low-elevation ski pistes after snow-melt of natural snow on the off-piste sites. The aim of this study was to identify snow/ice depth, snow density, and snow water equivalent of remaining ski piste snowpack to calculate and to compare snow ablation water volume with potential infiltration on the ski piste area at South-Central Slovak ski center Kosutka (Inner Western Carpathians; temperate zone). Snow ablation water volume was calculated from manual snow depth and density measurements, which were performed at the end of five winter seasons 2010-2011 to 2015-2016, except for season 2013-2014. The laser diffraction analyzes were carried out to identify soil grain size and subsequently the hydraulic conductivity of soil to calculate the infiltration. The average rate of water movement through soil was seven times as high as five seasons&apos; average ablation rate of ski piste snowpack; nevertheless, the ski piste area was potentially able to infiltrate only 47% of snow ablation water volume on average. Limitation for infiltration was frozen soil and ice layers below the ski piste snowpack and low snow-free area at the beginning of the studied ablation period.

  • 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

    10510 - Climatic research

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2020

  • 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 Hydrology and Hydromechanics

  • ISSN

    0042-790X

  • e-ISSN

  • Volume of the periodical

    68

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    SK - SLOVAKIA

  • Number of pages

    10

  • Pages from-to

    28-37

  • UT code for WoS article

    000514680600004

  • EID of the result in the Scopus database

    2-s2.0-85082050167