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Strategic Study of CAE >> 2012, Volume 14, Issue 9

The Chinese polar atmospheric sciences observation engineering system

Chinese Academy of Meteorological Sciences, Beijing 100081, China

Funding project:国家自然科学基金面上项目(41076132);“十二五”国家海洋局“南北极环境综合考察与评估”专项(CHINARE2011-2015) Received: 2012-06-25 Available online: 2012-09-25 09:17:42.000

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Abstract

The polar regions are located in the north and south ends on the earth, which are the key areas of global change research. To understand global change, especially the global climate change, it is needed to research on polar atmosphere. Chinese Arctic and Antarctic of scientific investigation started in 80s and 90s of last century. As a national action, by the end of 2011, 28 times Antarctic expeditions and 8 times Antarctic inland expeditions, and 4 time Arctic expeditions were organized. 3 Antarctic bases (Great Wall, Zhongshan and Kunlun) and 1 Arctic base (Yellow River) and 6 automatic weather stations were established. Formed by the manual weather station, automatic weather station and weather observation on the “Xuelong” icebreaker vessel as the main platform of the polar expedition of hardware support system. Chinese polar atmospheric science observation system is gradually formed including the meteorological operational observation and short term investigation study. Chinese polar meteorological expedition and research work has made great progress by the efforts near 30 years.

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References

[ 1 ] GARP,The Physical Basis of Climate and Climate Modeling[M].GARP Publication Series,1975.No:16.WMO/ICSU.

[ 2 ] IGBP.Towards Global Sustainability[M].IGBP Science Series,2001,4:27-29,

[ 3 ] SCAR.Antarctic Climate Change and Environment[M].UK:Scientifice Committee on Antaretic Research Scott Polar Research Institute,2009,

[ 4 ] IPCC.Climate change 2007,the physical scientific basis[C]//Working Group I Contribution to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change,Cambridge.UK:Cambridge University Press,2007.

[ 5 ] 陆龙骅,卞林根,极地对地球系统过程的作用[M]//孙九林,林海,地球系统研究与科学数据,北京:科学出版社,2009:414-433.

[ 6 ] 陆龙骅,卞林根,效存德,等,近20年来中国极地大气科学进展[J].气象学报,2004,62(5)672-691. link1

[ 7 ] 高登义,邹 捍,周立波,等,极地大气科学考察研究与展望[J].大气科学,2008,32(4):882-892. link1

[ 8 ] 魏文良,中国极地考察航线海洋气象研究[M].北京:海洋出版社,2008:1-234.

[ 9 ] 陆龙骅,卡林根, 近30年中国极地气象科学研究进展[J].极地研究,2011,23(1):1-10. link1

[10] 周秀骥,陆危骅,南极与全球气候环境相互作用和影响的研究[M].北京:气象出版社,1996:1-402.

[11] 陈立奇,北极海洋环境与海气相互作用研究[M].北京:海洋出版社,2003:1-339.

[12] 陈立奇,南极地区对全球变化的响应与反馈作用研究[M].北京,海洋出版社,2004;1-611.

[13] 张占海,快速变化中的北极海洋环境[M].北京:海洋出版社,2011:1-504.

[14] 中国首次北极科学考察队,中国首次北极科学考察报告[R].北京:海洋出版社,2000:1-191.

[15] 张占海,中国第二次北极科学考察报告[M].北京:海洋出版社,2004:1-229.

[16] 张海生,中国第三次北极科学考察报告[M].北京:海洋出版社,2009:1-225.

[17] 余兴光中国第四次北极科学考察报告[M].北京:海洋出版社,2011:1-254.

[18] 陆龙骅,卞林根,逮昌贵,等,近20年中国南极科学考察的气象业务进展[J].气象,2005,31(1):3-8. link1

[19] 效存德,秦大河,卞林根,等.东南极Princess Elizabeth地冰盖表面相对高程年内变化过场的精确监测[J].中国科学(D辑),2004,34(7):675-685

[20] 郑向东,周秀聩,陆龙骅,等.1993年中山站南极“臭氧洞”的观测研究[J].科学通报,1995,40(6):533-535. link1

[21] Lu Longhua,Bian Lingen,Cheng Yanje,et al.Surface ozone ob-servation during voyages to the Arctic and Antarctic regions[J].Chinese Science Bulletin,2001,46(23):1995-2000. link1

[22] 卞林根,陆龙骅,贾明群,南极冰盖极星期间近地面满流特征的实验观测[J].中国科学(D),1997,27(5):469-474,

[23] 刘瑞源,杨惠根,中国高空大气物理学观测研究进展[J].极地研究,2011,23(4):241-258. link1

[24] 陆龙骅,卞林根,贾朋群,南极和邻近地区温度的时空变化特征[J].中国科学(D辑),197,27(3):284-288. link1

[25] 周秀骥,陆龙骅,卞林根,等,南极地区温度、海冰、臭氧的变化特征[J].自然科学进展,1997,7(4):460-466. link1

[26] Lu Longhua,Bian Lingen.The characteristics of Antarctie cli-matie change[C].Beijing:Proceedings of ISCC China,2003,251-254.

[27] 陆龙骅,卞林根,张正秋,极地和青藏高原地区的气候变化及其影响[J].极地研究,2011,23(2):82-89. link1

[28] 卞林根,林 忠,张东启,等,南极大气臭氧和温度垂直结构及其季节变化的研究[J].中国科学:地科2,2011,411(12):1762-1770. link1

[29] 陆龙骅,臭氧与臭氧洞[J].自然杂志,2012,34(1):24-28.

[30] 卞林根,高志球,陆龙骅,等,北冰洋夏季开阔洋面和浮冰近地层热通量参数的观测估算[J].中国科学,2003,33(2):139-147.

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