2025
Variability of solar radiation and cloud cover in the Antarctic Peninsula region
SZYMSZOVÁ, Simona; Kamil LÁSKA; Seong-Joong KIM a Sang-Jong PARKZákladní údaje
Originální název
Variability of solar radiation and cloud cover in the Antarctic Peninsula region
Autoři
SZYMSZOVÁ, Simona; Kamil LÁSKA; Seong-Joong KIM a Sang-Jong PARK
Vydání
Atmospheric Research, Amsterdam, Elsevier Ltd, 2025, 0169-8095
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10508 Physical geography
Stát vydavatele
Nizozemské království
Utajení
není předmětem státního či obchodního tajemství
Impakt faktor
Impact factor: 4.400 v roce 2024
Označené pro přenos do RIV
Ano
Kód RIV
RIV/00216224:14310/25:00141942
Organizační jednotka
Přírodovědecká fakulta
UT WoS
EID Scopus
Klíčová slova anglicky
Solar radiation; Cloud cover; Cloud modification factor; James Ross Island; King George Island; Antarctic Peninsula
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 5. 9. 2025 13:49, Mgr. Marie Novosadová Šípková, DiS.
Anotace
V originále
Solar radiation is a key driver of many physical, chemical and biological processes in Antarctic ecosystems and the main component of the surface energy budget. The downward shortwave radiation (DSR) flux varies greatly in the Antarctic Peninsula region due to cloud cover changes, resulting from climate differences between eastern and western coasts. The DSR intensity was measured using A-class pyranometers at the J.G. Mendel (JGM) station located on the northeastern part of the Antarctic Peninsula and at the King Sejong (KSJ) station located on the western part for the period 2011-2016. The influence of the cloud cover on the DSR flux was evaluated using the cloud modification factor calculated for both stations. The effect of surface pressure, water vapour, albedo, cloud cover, ozone and solar zenith angle was examined using partial correlation. We found a 29 %-higher DSR intensity at the JGM station, while the cloud cover was higher at the KSJ station, with a 28 %-lower cloud modification factor compared with the JGM station. At both stations, the DSR variability was affected mainly by the solar zenith angle, followed by cloud cover at the JGM station, whereas the influence of cloud cover and water vapour was similar at the KSJ station. The effect of the albedo was significant for most of the year at the JGM station but only in the winter at the KSJ station. These results reveal significant differences in climate conditions between the western and eastern coasts, which are reflected in local atmospheric and cryospheric processes.
Návaznosti
| GA20-20240S, projekt VaV |
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| MUNI/A/1469/2023, interní kód MU |
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| VAN 2024, interní kód MU |
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