我国周边国家和地区的CO2本底浓度及对比分析

大气与环境光学学报 ›› 2017, Vol. 12 ›› Issue (2): 120-127.

我国周边国家和地区的CO2本底浓度及对比分析

贾小芳1, 张晓春1,2,3*, 赵亚南1,4, 王缅1, 靳军莉1

（1.中国气象局气象探测中心，北京 100081;
2.中国气象科学研究院,北京 100081;
3.中国科学院大学, 北京 100049;
4.中国气象局气象干部培训学院,北京 100081）

收稿日期:2015-08-13 修回日期:2015-09-07 出版日期:2017-03-28 发布日期:2017-03-23
通讯作者: 贾小芳 (1986-)，女，山西人，工程师，硕士，主要从事大气成分观测方面的研究。 E-mail:xczhang@camscma.cn
作者简介:贾小芳 (1986-)，女，山西人，工程师，硕士，主要从事大气成分观测方面的研究。
基金资助:
Supported by National Key Scientific Instrument and Equipment Development Project（国家重大科学仪器设备开发专项, 2013YQ220643）, China Special Fund for Meteorological Research in the Public Interest（公益性行业（气象）科研专项, GYHY201206037）, China Meteorological Administration Climate Change Project（中国气象局气候变化专项, CCSF201335）

Comparative Analysis of CO2 Background Concentration Between China Mainland and Neighboring Countries and Regions

JIA Xiaofang1, ZHANG Xiaochun1,2,3*, ZHAO Yanan1,4, WANG Mian1, JIN Junli1

（1. Meteorological Observation Center of China Meteorological Administration, Beijing 100081;
2. Chinese Academy of Meteorological Sciences, Beijing 100081;
3. University of the Chinese Academy of Sciences, Beijing 100049;
4. China Meteorological Administration Meteorological Training Center, Beijing 100081)

Received:2015-08-13 Revised:2015-09-07 Published:2017-03-28 Online:2017-03-23

摘要/Abstract

摘要：

利用世界温室气体数据中心（WDCGG）数据资料和WMO资料，对中国大陆及周边国家和地区的主要温室气体CO2浓度等进行了初步分析。分析结果表明：总体而言，中国大陆瓦里关全球大气本底站与中国香港、日本、俄罗斯、韩国等周边国家和地区CO2浓度水平相近，变化趋势一致；中国香港和韩国CO2的浓度较高，日本、俄罗斯和中国瓦里关的浓度较低。多年观测数据的研究分析显示，北半球CO2平均浓度呈现逐年升高态势，且CO2平均年变化幅度与观测站所处海拔高度成反比。中国瓦里关全球本底站与美国Mauna Loa、Barrow、Trinidad Head全球大气本底站CO2浓度水平和变化趋势较为一致，年际变化幅度略高于Mauna Loa站，低于Barrow站。中国上甸子区域大气本底站CO2浓度变化比瓦里关及美国Mauna Loa、Barrow、Trinidad Head站剧烈，显示出上甸子站受区域排放影响较强的特性。

关键词: 温室气体, CO2, 本底浓度, 对比分析

Abstract:

Using the data of World Data Center for Greenhouse Gases (WDCGG), the concentrations of the main greenhouse gas CO2 in China and its surrounding countries and regions are preliminarily analyzed. The results show that: the CO2 concentrations in China Mainland are close to Hong Kong in China, Japan, Russia, and South Korea; they all have the same trends. Higher CO2 concentrations are found in Hong Kong and South Korea, while lower CO2 concentrations in Japan, Russia, Waliguanin China. The results of many years observation show that the average concentration of CO2 in the northern hemisphere is increasing year by year, and the average annual variation of CO2 concentration is inversely proportional to the altitude of the observation station. The concentration and variation trend of CO2 in Waliguan global station is consistent with that in the Mauna Loa, Barrow, Trinidad Head global station. But the annual variation in Waliguan is slightly higher than in Mauna Loa and lower than in Barrow. The changes of CO2 concentration in Shangdianzi regional background station in China are more violent than in Waliguan, Mauna Loa, Barrow, Trinidad Head station, which shows that Shangdianzi station is affected by the strong regional emissions.

Key words: greenhouse gases, CO2, background concentration comparative analysis

中图分类号:

P413

贾小芳张晓春赵亚南王缅靳军莉. 我国周边国家和地区的CO2本底浓度及对比分析[J]. 大气与环境光学学报, 2017, 12(2): 120-127.

JIA Xiao-Fang, ZHANG Xiao-Chun, ZHAO Ya-Na, WANG Mian, JIN Jun-Li. Comparative Analysis of CO2 Background Concentration Between China Mainland and Neighboring Countries and Regions[J]. Journal of Atmospheric and Environmental Optics, 2017, 12(2): 120-127.

参考文献

[1] Liu Qiang, Wang Yuesi, Wang Mingxing, et al. Trends of greenhouse gases in recent 10 years in Beijing [J]. Chinese Journal of Atmospheric Sciences, 2005, 29(2): 267-270(in Chinese).
刘强, 王跃思, 王明星, 等. 北京大气中主要温室气体近10年变化趋势 [J]. 大气科学, 2005, 29(2): 267-270.
[2] Ramanathan V, Cicerone R J, Singh H B, et al. Trace gas trends and their potential role in climate change [J]. J. Geophys. Res., 1985, 90: 5547-5566.
[3]Esser G. Sensitivity of global climatic impacts [J]. Tellus, 1987, 39B: 245-260.
[4]Brunke E G, Scheel H E, Seilev W. Trends of tropospheric CO, N2O, and CH4 as observed at Cape Point, South Africa [J]. Atmos. Environ., 1990, 24A: 585-595.
[5]IPCC. Climate Change 2001: Synthesis Report [M]. Cambridge, NY, USA: Cambridge University Press, 2001: 5.
[6]IPCC. Climate Change 1995: The Science of Climate Change [M]. Cambridge, NY, USA: CambridgeUniversity Press, 1996: 21-24.
[7]Wang Mingxing. Change of green house gases and its effect on climate change [J]. Climatic and Environmental Research, 2000, 5(3): 329-332(in Chinese).
王明星. 关于温室气体浓度变化及其引起的气候变化的几个问题 [J]. 气候与环境研究, 2000, 5(3): 329-332.
[8]Houghton J. Global Warming [M]. Transl. by Dai Xiaosu, Shi Guangyu, Dong Min, et al. Beijing: Meteorological Publishing House, 1998: 29-51(in Chinese).
Houghton J. 全球变暖 [M]. 戴晓苏, 石广玉, 董敏, 等译. 北京: 气象出版社, 1998: 28-51.
[9]Kong Shaofei, Lu Bing, Han Bin, et al. Seasonal variation analysis of atmospheric CH4, N2O and CO2 in Tianjin offshore area [J]. Science China Earth Sciences, 2010, 40(5): 666-676(in Chinese).
孔少飞, 陆炳, 韩斌, 等. 天津近海大气中CH4, N2O和CO2季节变化分析 [J]. 中国科学: 地球科学, 2010, 40(5): 666-676.
[10]Liu Qiang, Liu Jiaqi, He Huaiyu. Research advances on concentration change of greenhouse gases and their source & sink [J]. Advance in Earth Sciences, 2000, 15(4): 453-460(in Chinese).
刘强, 刘嘉麒, 贺怀宇. 温室气体浓度变化及其源与汇研究进展 [J]. 地球科学进展, 2000, 15(4): 453-460.
[11]Zhou Lingxi, Zhang Xiaochun, Hao Qingju, et al. Study of the Background Greenhouse Gas Observation[J]. 气候变化研究进展, 2006,2(2): 63-67(in Chinese).
周凌晞,张晓春,郝庆菊, 等. 温室气体本底观测研究[J]. 气候变化研究进展, 2006,2(2):63-67.
[12]Qu Jiansheng, Zeng Jingjing, Zhang Zhiqiang. Review of the international main greenhouse gases emission database [J]. Advances in Earth Science, 2008, 23(1): 47-54(in Chinese).
曲建升, 曾静静, 张志强. 国际主要温室气体排放数据集比较分析研究 [J]. 地球科学进展, 2008, 23(1): 47-54.
[13] WDCGG. WMO WDCGG data summary WDCGG No.38 [R]. Japan, Tokyo, Japan meteorological agency in co-operation with WMO, 2014, 38: 75-76.
[14]World Data Centre for Greenhouse Gases [OL]. http://ds.data.jma.go.jp/gmd/wdcgg/cgi-bin/wdcgg/catalogue.cgi.
[15] Zhou L X, White J W C, Conway T J, et al. Long-term record of atmospheric CO2 and stable isotopic ratios at Waliguan Observatory: Seasonally averaged 1991–2002 source/sink signals, and a comparison of 1998–2002 record to the 11 selected sites in the Northern Hemisphere [J]. Global Biogeochem. Cy., 2006, 20: GB2001, doi:10.1029/2004GB002431.
[16]Jing Yuanshu, Jin Wei, Qu Yan, et al. Study on features of greenhouse gas and its changing trends in East Asia from 1991 to 2004 [J]. Research of Environmental Sciences, 2007, 20(6): 67-70(in Chinese).
景元书, 金巍, 曲岩, 等. 1991-2004年东亚温室气体浓度特征及变化趋势 [J]. 环境科学研究, 2007, 20(6): 67-70.
[17]Zhou Lingxi, Zhou Xiuji, Zhang Xiaochun, et al. Progress in the study of background greenhouse gases at Waliguan Observatory [J]. Acta Meteorologica Sinica, 2007, 65(3): 458-468(in Chinese).
周凌晞, 周秀骥, 张晓春, 等. 瓦里关温室气体本底研究的主要进展 [J]. 气象学报, 2007, 65(3): 458-468.