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Surface elevation changes on Lachman Crags ice caps (north-eastern Antarctic Peninsula) since 1979 indicated by DEMs and ICESat data

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F19%3A79660" target="_blank" >RIV/60460709:41330/19:79660 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11310/19:10398610

  • Result on the web

    <a href="https://www.cambridge.org/core/journals/journal-of-glaciology/article/surface-elevation-changes-on-lachman-crags-ice-caps-northeastern-antarctic-peninsula-since-1979-indicated-by-dems-and-icesat-data/994340CC93D3AFCFD80B5C47DA44FC19/core-reader" target="_blank" >https://www.cambridge.org/core/journals/journal-of-glaciology/article/surface-elevation-changes-on-lachman-crags-ice-caps-northeastern-antarctic-peninsula-since-1979-indicated-by-dems-and-icesat-data/994340CC93D3AFCFD80B5C47DA44FC19/core-reader</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1017/jog.2019.19" target="_blank" >10.1017/jog.2019.19</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Surface elevation changes on Lachman Crags ice caps (north-eastern Antarctic Peninsula) since 1979 indicated by DEMs and ICESat data

  • Original language description

    The long term warming on the Antarctic Peninsula in the second half of the 20th century prompted rapid retreat of glaciers on the peninsula and surrounding islands. Retreat accelerated until the beginning of the new millennium when the regional warming trend significantly decreased. The response of glaciers to the change in temperature trend has been observed around the northern part of the Antarctic Peninsula but the timing of the shift from the surface lowering to mass gain remains unclear. Using historical aerial photographs, DEMs and satellite altimeter data from ICESat, we estimate areal and surface elevation changes of two small ice caps in the northern part of James Ross Island over the last 39 years. The glacierized area on Lachman Crags decreased from 4,337 to 3,581 km2 between 1979 and 2006 and then increased to 3,597 km2 0,4 until 2016. Surface lowering observed on ice caps after 1979 continued at least until 2008 as indicated by the ICESat data. The change from the lowering trend to incre

  • 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

  • Continuities

    S - Specificky vyzkum na vysokych skolach

Others

  • Publication year

    2019

  • 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

    65

  • Issue of the periodical within the volume

    251

  • Country of publishing house

    CZ - CZECH REPUBLIC

  • Number of pages

    12

  • Pages from-to

    410-421

  • UT code for WoS article

    000470734900005

  • EID of the result in the Scopus database

    2-s2.0-85064891210