资源环境科技发展态势分析平台

Studies assessing air temperature variations and their dependence on altitude from the eastern side of the Antarctic Peninsula are sparse. In this paper, we analyse air temperature and near-surface lapse rates from the Ulu Peninsula (James Ross Island, Antarctic Peninsula). The temperature data were acquired from nine sites both in ice-free areas and glaciers of the Ulu Peninsula in 2013-2016. The most important factors influencing air temperature differences were sea-ice conditions, topography and ground surface properties. During the study period, air temperature decreased with height with the mean lapse rate of 0.40 degrees C100m(-1) for the ice-free sites (10-375m a.s.l.) and 0.43 degrees C100m(-1) for the glaciated sites (268-539m a.s.l.). However, the values were lower in winter (ice-free: 0.02 degrees C100m(-1) and glacier: 0.31 degrees C100m(-1)) than in summer (ice-free: 0.62 degrees C100m(-1) and glacier: 0.51 degrees C100m(-1)) for both categories. The air layer between 10 and 56m a.s.l. in the ice-free area revealed an almost year-round air temperature inversion resulting in a mean lapse rate of -0.79 degrees C100m(-1) and an air temperature inversion frequency reaching up to 43%. The temperature inversion frequency was 10% lower for the lowest air layer for the glacier category, which was between 268 and 356m a.s.l. The land surface air temperature was the highest when the wind was from the northwest and lowest when it was from the south-southwest. The near-surface lapse rate-wind direction relationship was the most pronounced for the air layer between 10 and 56m a.s.l. with the lowest mean lapse rate for west-southwest wind (-2.83 degrees C100m(-1)) and the highest for east-northeast wind (0.41 degrees C100m(-1)).