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Surface mass balance of small glaciers on James Ross Island, north-eastern Antarctic Peninsula, during 2009-2015

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F18%3A10380394" target="_blank" >RIV/00216208:11310/18:10380394 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216224:14310/18:00101230

  • Result on the web

    <a href="https://doi.org/10.1017/jog.2018.17" target="_blank" >https://doi.org/10.1017/jog.2018.17</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1017/jog.2018.17" target="_blank" >10.1017/jog.2018.17</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Surface mass balance of small glaciers on James Ross Island, north-eastern Antarctic Peninsula, during 2009-2015

  • Original language description

    Two small glaciers on James Ross Island, the north-eastern Antarctic Peninsula, experienced surface mass gain between 2009 and 2015 as revealed by field measurements. A positive cumulative surface mass balance of 0.57 +/- 0.67 and 0.11 +/- 0.37 m w.e. was observed during the 2009-2015 period on Whisky Glacier and Davies Dome, respectively. The results indicate a change from surface mass loss that prevailed in the region during the first decade of the 21st century to predominantly positive surface mass balance after 2009/10. The spatial pattern of annual surface mass-balance distribution implies snow redistribution by wind on both glaciers. The mean equilibrium line altitudes for Whisky Glacier (311 +/- 16 m a.s.l.) and Davies Dome (393 +/- 18m a.s.l.) are in accordance with the regional data indicating 200-300 m higher equilibrium line on James Ross and Vega Islands compared with the South Shetland Islands. The mean accumulation-area ratio of 0.68 +/- 0.09 and 0.44 +/- 0.09 determined for Whisky Glacier and Davies Dome, respectively, is similar to the value reported for Vega Island and within the range of typical values for high-latitude glaciers.

  • 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

    10508 - Physical geography

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2018

  • 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 Glaciology

  • ISSN

    0022-1430

  • e-ISSN

  • Volume of the periodical

    64

  • Issue of the periodical within the volume

    245

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    13

  • Pages from-to

    349-361

  • UT code for WoS article

    000434777300001

  • EID of the result in the Scopus database

    2-s2.0-85045658570