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Persistent mass loss of Triangular Glacier, James Ross Island, northeastern Antarctic Peninsula

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F23%3A10447342" target="_blank" >RIV/00216208:11310/23:10447342 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216224:14310/23:00129985

  • Result on the web

    <a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=XqYEZi~-~r" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=XqYEZi~-~r</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1017/jog.2022.42" target="_blank" >10.1017/jog.2022.42</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Persistent mass loss of Triangular Glacier, James Ross Island, northeastern Antarctic Peninsula

  • Original language description

    The retreat rates of Triangular Glacier since 1979 and its mass changes during the period 2014/15-2019/20 indicate the sensitive response of small ice masses on the eastern side of the Antarctic Peninsula to air temperature evolution. This cirque glacier in the northern part of James Ross Island receded rapidly during the period of regional warming in the late 20th century, losing 30.8% of its surface area between 1979 and 2006 (-1.7% a(-1)). The retreat rate then dropped to -0.3% a(-1) following the regional cooling trend, but started to accelerate again (-0.8 to -2.3% a(-1)) with increasing air temperature since the summer 2014/15. Since the glaciological year 2015/16, Triangular Glacier has experienced enhanced snow melt, wind scour and permanent mass loss with annual mass balance ranging from -0.08 +- 0.35 to -0.56 +- 0.25 m w.e. The largest mass loss was observed in the glaciological year 2019/20, which included the warmest summer of the observation period. The cumulative mass balance of -1.66 +- 0.83 m w.e. over the years 2014/15-2019/20 is consistent with the termination of the positive mass-balance period that occurred in the north-eastern Antarctic Peninsula from 2009/10 to 2014/15.

  • 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

    2023

  • 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

    1727-5652

  • Volume of the periodical

    69

  • Issue of the periodical within the volume

    273

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    13

  • Pages from-to

    27-39

  • UT code for WoS article

    000808370600001

  • EID of the result in the Scopus database

    2-s2.0-85148709899