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Surface ozone variations at the Great Wall Station,Antarctica during austral summer

Advances in Polar Science 2020年第2期31卷 92-102页

作者： Justin SENTIAN Franky HERMAN Mohd Sharul MOHD NADZIR Vivian Kong WAN YEE Climate Change Research Group Faculty of Science and Natural ResourcesUniversiti Malaysia Sabah88400 Kota KinabaluSabahMalaysia Faculty of Science and Technology Universiti Kebangsaan Malaysia43600 UKM BangiSelangorMalaysia

Surface ozone(O3)is a secondary pollutant harmful to human health and a greenhouse gas which is one of the prime climate *** to the clean atmospheric environment of the Antarctic region and given the complexity of O3 chemistry,the observation of surface O3 variability in this region is necessary in the quest to better understand the potential sources and sink of polar surface *** this paper,we highlighted our observations on O3 variability at the Great Wall Station(GWS)during austral summer in December 2018 and January *** continuous surface O3 measurement at the GWS,Antarctica was carried out using the Ecotech Ozone *** understand the roles of the meteorological conditions on the temporal variations of O3,meteorological data was obtained from the conventional auto-observational station at the *** Hybrid Single-Particle Lagrangian Integrated Trajectory(HYSPLIT)model was employed to investigate the air mass transport over the *** observed austral summer surface O3 concentrations at the GWS exhibited variability and were significantly lower than those previously observed at other permanent coastal stations in *** surface ozone variability at the GWS was strongly influenced by the synoptic change of air mass origin although the roles of photochemistry production and destruction were still *** characteristics and stable surface O3 characterized the air masses that reached the *** unique characteristic of surface O3 at the coastal site of GWS was emphasized by its synoptic air mass characteristics,which displayed a significant influence on surface O3 *** mass that traveled over the ocean with relatively shorter distance was linked to the lower O3 level,whereby the marine transport of reactive bromine(Br)species was thought to play a significant role in the tropospheric chemistry that leads to O3 ***,the diurnal variation indicated that the O3 background concentration levels were n

关键词： surface ozone Great wall Station austral summer HYSPLIT

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summer fast ice evolution off Zhongshan Station,Antarctica

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Chinese Journal of Polar Science 2008年第1期19卷 54-62页

作者：雷瑞波李志军张占海程言峰窦银科 State Key Laboratory of Coastal and Offshore Engineering Dalian University of Technology Polar Research Institute of China Institute of Measuring and Controlling Taiyuan University of Technology

Based on the field data acquired in the program of fast ice observation off Zhongshan Station, Prydz Bay, East Antarctica during the austral summer 2005/ 2006, physical properties evolution of fast ice during the ice ablation season is analyzed in detail. Results show that the annual maximum ice thickness in 2005 occurred in later November, and then ice started to reek, and the ablation duration was 62 days; sea water under the ice became warmer synchronously; corresponding to the warming sea ice temperature, a ＂relative cold mid-layer＂ appeared in sea ice; the fast ice marginal line recoiled back to the shore observably, and the recoil distance was 20.9 km from 18 December 2005 through 14 January 2006. In addition, based on the data of sea ice thickness survey along the investigation course of MV Xuelong on December 18 of 2005, the ice thickness distribution paten in the marginal ice zone have been described ： sea ice thickness increased, but the diversity of floe ice thick-ness decreased from open water to fast ice zone distinctly.

关键词： fast ice physical characteristic evolution Antarctica austral summer

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