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자료유형
학술저널
저자정보
Jin-Yong Lee (Kangwon National University) Hyoun Soo Lim (Pusan National University) Ho Il Yoon (Korea Polar Research Institute)
저널정보
한국지질과학협의회 Geosciences Journal Geosciences Journal Vol.20 No.4
발행연도
2016.1
수록면
503 - 516 (14page)

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초록· 키워드

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Soil temperatures, water temperatures, and weather parameters were monitored at a variety of locations in the vicinity of King Sejong station, King George Island, Antarctica, during summer 2010–2011. Thermal characteristics of soil and water were analysed using time-series analyses, apparent thermal diffusivity (ATD), and active layer thickness. The temperatures of pond water and nearby seawater showed the distinctive diurnal variations and correlated strongly with solar radiation (r = 0.411–0.797). Soil temperature (0.1–0.3 m depth) also showed diurnal fluctuations that decreased with depth and were directly linked to air temperature (r = 0.513–0.783) rather than to solar radiation; correlation decreased with depth and the time lag in the response increased by 2–3 hours per 0.1 m of soil depth. Owing to the lack of snow cover, summertime soil temperature was not decoupled from air temperature. Estimated ATD was between 0.022 and 29.209 mm2/sec, showed temporal and spatial variations, and correlated strongly with soil moisture content. The maximum estimated active layer thickness in the study area was a 41–70 cm, which is consistent with values reported in the previous work.

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