留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

渤海大气二氧化硫浓度分布及陆源输送研究

姜杰 查勇 陈骁强 沈丹

姜杰, 查勇, 陈骁强, 沈丹. 渤海大气二氧化硫浓度分布及陆源输送研究[J]. 海洋学报, 2011, 33(6): 73-78.
引用本文: 姜杰, 查勇, 陈骁强, 沈丹. 渤海大气二氧化硫浓度分布及陆源输送研究[J]. 海洋学报, 2011, 33(6): 73-78.
JIANG Jie, ZHA Yong, CHEN Xiao-qiang, SHEN Dan. Study on concentration and transport characteristics of sulfur dioxide over the Bohai Sea[J]. Haiyang Xuebao, 2011, 33(6): 73-78.
Citation: JIANG Jie, ZHA Yong, CHEN Xiao-qiang, SHEN Dan. Study on concentration and transport characteristics of sulfur dioxide over the Bohai Sea[J]. Haiyang Xuebao, 2011, 33(6): 73-78.

渤海大气二氧化硫浓度分布及陆源输送研究

基金项目: 国家科技支撑计划(2008BAC34B07);江苏省属高校自然科学重大基础研究项目(08KJA170001);江苏高校优势学科建设工程资助项目。

Study on concentration and transport characteristics of sulfur dioxide over the Bohai Sea

  • 摘要: 利用2005年OMI/Aura反演的大气边界层二氧化硫(SO2)垂直柱密度数据,分析了渤海大气SO2浓度分布时空变化特征,并利用FNL气象资料,运用HYSPLIT模型对渤海大气环流后向轨迹进行分析。研究表明:渤海海域大气SO2浓度随季节变化明显,在秋冬季SO2浓度比较高,在冬季高达6.187×1016 cm-2;在春夏季SO2浓度都比较低,夏季是一年中最低的季节,约为3.766×1016 cm-2;在不同季节SO2浓度空间分布极不均衡。通过后向轨迹分析发现,渤海大气SO2浓度主要受环渤海陆上地区影响,在冬季影响最强烈,在夏季相对弱些。
  • GRUBLER A. A review of global and regional sulfur emission scenarios[J]. Mitigation and Adaptation Strategies for Global Change, 1998, 3(2): 383-418.
    SMITH S J, PITCHER H, WIGLEY T M L. Global and regional anthropogenic sulfur dioxide emissions[J]. Global and Planetary Change, 2001, 29(1-2): 99-119.
    DONEY S C, MAHOWALD N, LIMA I, et al. Impact of anthropogenic atmospheric nitrogen and sulfur deposition on ocean acidification and the inorganic carbon system[J]. Proceedings of the National Academy of Sciences of the United States of America, 2007, 104(37): 14580-14585.
    FEELY R A, SABINE C L, HERNANDEZ-AYON J M, et al. Evidence for upwelling of corrosive "acidified" water onto the continental shelf[J]. Science, 2008, 320(5882): 1490-1492.
    王琪, 高忠文. 关于渤海环境综合整治行动的反思[J]. 海洋环境科学, 2007, 26(3): 290-294.
    OHARA T, AKIMOTO H, KUROKAWA J, et al. An Asian emission inventory of anthropogenic emission sources for the period 1980-2020[J]. Atmospheric Chemistry and Physics, 2007, 7(16): 4419-4444.
    DUCE R A, LISS P S, MERRILL J T, et al. The atmospheric input of trace species to the world ocean[J]. Global Biogeochem Cycles, 1991, 5(3): 193-259.
    盛立芳, 高会旺, 张英娟, 等. 夏季渤海NOx、O3、SO2和CO浓度观测特征[J]. 环境科学, 2002, 23(6): 31-35.
    付营. 中国近海大气污染物浓度特征及陆源输送研究 . 青岛: 中国海洋大学, 2006.
    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.
    LEVELT P F, VAN DEN OORD G H J, DOBBER M R, et al. The ozone monitoring instrument[J]. IEEE Transactions on Geoscience and Remote Sensing, 2006, 44(5): 1093-1101.
    KROTKOV N A, CARN S A, KRUEGER A J, et al. Band residual difference algorithm for retrieval of SO2 from the aura ozone monitoring instrument (OMI)[J]. IEEE Transactions on Geoscience and Remote Sensing, 2006, 44(5): 1259-1266.
    YANG K, KROTKOV N A, KRUEGER A J, et al. Retrieval of large volcanic SO2 columns from the aura ozone monitoring instrument: comparison and limitations[J]. J Geophys Res-Atmos, 2007, 112(D24): doi: 10.1029/2007JD008825.
    KROTKOV N A, MCCLURE B, DICKERSON R R, et al. Validation of SO2 retrievals from the ozone monitoring instrument over NE China[J]. J Geophys Res-Atmos, 2008, 113(D16): D16S40, doi: 10.1029/2007JD008818.
    LI C, ZHANG Q, KROTKOV N A, et al. Recent large reduction in sulfur dioxide emissions from Chinese power plants observed by the ozone monitoring instrument[J]. Geophys Res Lett, 2010, 37(8): L08807.
    WITTE J C, SCHOEBERL M R, DOUGLASS A R, et al. Satellite observations of changes in air quality during the 2008 Beijing Olympics and Paralympics[J]. Geophys Res Lett, 2009, 36(17): L17803.
    DRAXLER R R, HESS G D. An overview of the HYSPLIT_4 modeling system for trajectories, dispersion and deposition[J]. Australian Meteorological Magazine, 1998, 47:295-308.
    Air Resources Laboratory. FNL Archive Information . . http://www.arl.noaa.gov/fnl.php.
  • 加载中
计量
  • 文章访问数:  1357
  • HTML全文浏览量:  12
  • PDF下载量:  1406
  • 被引次数: 0
出版历程
  • 收稿日期:  2010-01-16
  • 修回日期:  2011-04-19

目录

    /

    返回文章
    返回