[1] WMO greenhouse gas bulletin. The state of greenhouse gases in the atmosphere based on global observations through 2010[R]. 2011,7(21)
[2] World Meteorological Organization. Global Atmosphere Watch[R].Geneva:WMO,1993,86:1-19
[3] 周秀骥. 中国大气本底基准观象台进展总结报告[M]. 北京:气象科学出版社, 2005:18-19
[4] MÜller G., Hov Øystein, Klausen J, et al. WMO global atmosphere watch (GAW) strategic plan:2008—2015[R]. 2007, No.172. 2
[5] 刘立新,周凌晞,张晓春,等.我国4个国家级本底站大气CO2浓度变化特征[J].中国科学,2009,39(2):222-228
[6] Chen H, Winderlich J, Gerbig C, et al. High-accuracy continuous airborne measurements of greenhouse gases (CO2 and CH4) using the cavity ring-down spectroscopy (CRDS) technique[J]. Atmospheric Measurement Techniques, 2010,3:375-386
[7] 于大江,吴艳玲,宋庆利,等.龙凤山区域大气本底站站址特征及其观测资料[J].气候变化研究快报,2012,1(2):65-73
[8] Crosson E R. A cavity ring-down analyzer for measuring atmospheric levels of methane, carbon dioxide, and water vapor [J]. Applied Physics B, 2008, 92(3):403-408
[9] 臧昆鹏,周凌晞,方双喜,等.新型CO2和CH4混合标气标校流程及方法[J].环境化学,2011,30(2):511-516
[10] 蒋高明,黄银晓,韩兴国. 城市与山地森林地区夏季秋季大气CO2浓度变化初探[J]. 环境科学学报,1998,18(1):108-111
[11] 胡会峰,刘国华.森林管理在全球CO2减排中的作用[J].应用生态学报,2006,17(4):709-714
[12] 温玉璞,汤洁,邵志清,等.瓦里关山大气二氧化碳浓度变化及地表排放影响的研究[J].应用气象学报,1997,8(2):129-136
[13] Zhou L X, Conway T J, White J W C, et al. Long-term record of atmospheric CO2 and stable isotopic ratios at Waliguan Observatory:Background features and possible drivers, 1991-2002[J]. Global Biogeochemical Cycles, 2005, 19, GB3021 1-9, dio:10.1029/2004GB002430
[14] 周凌晞, 汤洁, 张晓春, 等. 气相色谱法观测本底大气中的甲烷和二氧化碳[J]. 环境科学学报, 1998, 18(4):356-361.
[15] 王庚辰,温玉璞,孔琴心,等. 中国大陆上空CO2的本底浓度及其变化[J]. 科学通报,2002,47(10):780-783
[16] Tsutsumi Y, Mori K, Ikegami M, et al. Long-term trends of greenhouse gases in regional and background events observed during 1998-2004 at Yonagunijima located to the east of the Asian continent [J]. Atmospheric Environment, 2006,40:5868-5879
[17] 周凌晞, 汤洁, 温玉璞,等. 地面风对瓦里关山大气CO2本底浓度的影响分析[J]. 环境科学学报, 2002, 22(2):135-139