Informace o publikaci

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

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OBU Jaroslav SEBASTIAN Westermann GONCALO Vieira ANDREY Abramov MEGAN Balks ANNETT Bartsch HRBÁČEK Filip ANDREAS Kääb MIGUEL Ramos

Rok publikování 2020
Druh Článek v odborném periodiku
Časopis / Zdroj The Cryosphere
Fakulta / Pracoviště MU

Přírodovědecká fakulta

Citace
www https://www.the-cryosphere.net/14/497/2020/
Popis Abstract: 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?km2 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?°C. The lowest near-surface permafrost temperature of -36?°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?°C for mountainous areas rising above the Antarctic Ice Sheet and between -14 and -8?°C for coastal areas. The model performance was good where snow conditions were modelled realistically, but errors of up to 4?°C occurred at sites with strong wind-driven redistribution of snow.
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