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Pan-Antarctic map of near-surface permafrost temperatures at 1 km2 scale

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F20%3A00115673" target="_blank" >RIV/00216224:14310/20:00115673 - isvavai.cz</a>

  • Result on the web

    <a href="https://www.the-cryosphere.net/14/497/2020/" target="_blank" >https://www.the-cryosphere.net/14/497/2020/</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.5194/tc-14-497-2020" target="_blank" >10.5194/tc-14-497-2020</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Pan-Antarctic map of near-surface permafrost temperatures at 1 km2 scale

  • Original language description

    Permafrost is present within almost all of the Antarctic's ice-free areas, but little is known about spatial variations in permafrost temperatures except for a few areas with established ground temperature measurements. We modelled a temperature at the top of the permafrost (TTOP) for all the ice-free areas of the Antarctic mainland and Antarctic islands at 1 km(2) resolution during 2000-2017. The model was driven by remotely sensed land surface temperatures and downscaled ERA-Interim climate reanalysis data, and subgrid permafrost variability was simulated by variable snow cover. The results were validated against in situ-measured ground temperatures from 40 permafrost boreholes, and the resulting root-mean-square error was 1.9 degrees C. The lowest near-surface permafrost temperature of -36 degrees C was modelled at Mount Markham in the Queen Elizabeth Range in the Transantarctic Mountains. This is the lowest permafrost temperature on Earth, according to global-scale modelling results. The temperatures were most commonly modelled between -23 and -18 degrees C for mountainous areas rising above the Antarctic Ice Sheet and between -14 and -8 degrees C for coastal areas. The model performance was good where snow conditions were modelled realistically, but errors of up to 4 degrees C occurred at sites with strong wind-driven redistribution of snow.

  • 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

    <a href="/en/project/LM2015078" target="_blank" >LM2015078: Czech Polar Research Infrastructure</a><br>

  • Continuities

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

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

    The Cryosphere

  • ISSN

    1994-0416

  • e-ISSN

    1994-0424

  • Volume of the periodical

    14

  • Issue of the periodical within the volume

    2

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    23

  • Pages from-to

    497-519

  • UT code for WoS article

    000513070900001

  • EID of the result in the Scopus database

    2-s2.0-85079389383