1999年, 第10卷, 第1期　刊出日期：1999-02-25

  

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  Recent variations of Antarctic temperature, sea-ice and ozone

  ZhouXiuji,周秀骥,LuLonghua,陆龙骅,BianLingen,卞林根,JiaPengqun,贾朋群,ZhangZhengqiu,张正秋

  Advances in Polar Science. 1999, 10(1): 1-9.

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  Study of the MSA, nssSO₄^2- concentration and MSA to nssSO₄^2- ratio in the snow/ice and atmospheric aerosols of the regions surrounding the Weddell Sea

  HanJiankang,韩建康

  Advances in Polar Science. 1999, 10(1): 10-18.

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  Isotopic analysis of the snow cover at an alpine glacier as an indicator of local climatic variations and isotopic homogenization processes

  HeYuanqing,何元庆 1,TheakstoneWH,TheakstoneWH 2

  Advances in Polar Science. 1999, 10(1): 19-24.

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  Biotic weathering of rocks by lichens in Antarctica

  ChenJie,陈杰 1,Hans-PeterBlume,Hans-PeterBlume 2

  Advances in Polar Science. 1999, 10(1): 25-32.

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  Preliminary result of imaging riometer at Zhongshan Station, Antarctica

  LiuYonghua,刘勇华 1,LiuRuiyuan,刘瑞源 1,HeLongsong,贺龙松 1,HuHongqiao,胡红桥 2,MasanoriNishino,MasanoriNishino 3,YasuharuSano,YasuharuSano 4,HisaoYamagishi,HisaoYamagishi 5,NatuoSato,NatuoSato 5

  Advances in Polar Science. 1999, 10(1): 33-40.

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  Trace-element ions in snow, ice and water from Antarctic and Arctic with reference of their water vapor chemistry

  LiuMingxing,刘明星,GuHongkan,顾宏堪

  Advances in Polar Science. 1999, 10(1): 41-44.

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  Trace-element ions in snow,ice and water from Antarctic and Arctic with reference of their water vapor chemistry

  Liu Mingxing,Gu Hongkan

  Advances in Polar Science. 1999, 10(1): 43-46. https://doi.org/cnki:ISSN:1007-7065.0.1999-01-005

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  The some trace elements in the Antarctic and Arctic snow, ice, water were studied using the methodology and theory of water vapor chemistry. The concentrations of ions Zn²⁺, Cd²⁺, Pb²⁺, Cu²⁺, Sn⁴⁺, Bi³⁺ in Antarctic and Arctic snow a significant spatial similarity; they are also close to those defined elsewhere on the basic of studies of water vapor chemistry: on average Zn²⁺ 5.0 μg/L, Cd²⁺ 0.080 μg/L, Pb²⁺ 0.030 μg/L, Cu²⁺ 0.70 μg/L, Sn⁴⁺ 0.99 μg/L, Bi³⁺ 0.18 μg/L. Apparently, the ion concentration in the Antarctic and Arctic region represent natural baseline values and are controlled by natural water cycles.

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  The difference of atmospheric chemical loadings shown by electrical conductivity of snow and ice between Antarctica, Arctic and Qinghai-Tibetan Plateau

  XiaoCunde,效存德,QinDahe,秦大河,YaoTandong,姚檀栋,RenJiawen,任贾文,ShengWenkun,盛文坤

  Advances in Polar Science. 1999, 10(1): 45-50.

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  The relationship between polar sea ice and the precipitation and temperature over China revealed by using SVD method

  LiuJiping,刘骤平,BianLingen,卞林根

  Advances in Polar Science. 1999, 10(1): 51-60.

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  The primary research on the environmental climatic records of the two snow pits recovered from Princess Elizabeth Land, Antarctica

  ZhangMingjun,张明军 1,LiZhongqin,李忠勤 1,QinDahe,秦大河 1,LiJun,李军 2

  Advances in Polar Science. 1999, 10(1): 61-66.

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  Characteristics of change in the Antarctic sea ice area and its relation to SST in the tropical Pacific

  ChenJinnian,陈锦年

  Advances in Polar Science. 1999, 10(1): 67-73.

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