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硫酸盐直接辐射强迫的在线与固定转化率模拟方法的对比研究 被引量:1

COMPARISON OF ON-LINE COUPLED AND CONSTANT TRANS- MISSION SIMULATION METHODS FOR DIRECT RADIATIVE FORCING OF ANTHROPOGENIC SULFATE
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摘要 以2000年1、4、7、10月为例,利用区域气候模式,比较了模拟硫酸盐气溶胶分布和直接辐射强迫的在线模拟方法与固定SO2到硫酸盐转化率方法,并与全球模式的结果进行了对比检验.结果表明:在线模拟得到的主要结果与全球平均结果符合得很好,但固定转化率方法存在明显偏差;两种方法硫酸盐柱含量的差异在-4~12 mg/m2范围内,占在线模拟柱含量的42%以上,7月份差异最显著,1月份差异最小;大气顶辐射强迫差异在-1.8~0.4 W/m2之间,此差别占在线辐射强迫的26%以上;采用36.7%的固定转化率对冬季过大、夏季偏小,只有春秋季的江南部分地区适合.由于固定转化率方法不能反映温度、辐射、水汽、云水等气象要素的季节性变化对硫酸盐生成率的影响,因而对硫酸盐含量和分布的季节变化模拟存在偏差,这是导致上述差异的重要原因. Two methods, on-line coupled and constant transmission, for radiative forcing simulation of anthropogenic sulfate over China area have been compared within Jan., Apr., Jul. and Oct. 2000. The following results can be figured out based on the comparison: (1) The results of on-line coupling are consistent with global averaged results from GCMs. (2) Both column burden and radiative forcing at TOA of anthropogenic sulfate have obvious differences between the two simulation methods. (3) The maximum difference range of sulfate burden is from -4 to 12 mg/m^2. Its maximum emerges in July and minimum value in January. The relative difference to that of on-line sulfate burden is more than 42% on the whole simulated area scale. If partial area averages are compared, their values are more than that of the whole area scale. (4) The difference of radiative forcing at TOA is within -1.8-0.4W/m^2. The relative difference to that of on-line radiative forcing at TOA is more than 26% on the whole simulated area scale. (5) The results of constant transmission method differ from on-line or off-line methods fairly, and it is hard to give the fact of sulfate burden and radiative forcing.
出处 《热带气象学报》 CSCD 北大核心 2005年第6期615-622,共8页 Journal of Tropical Meteorology
基金 国家自然科学基金资助项目(40205016) 云南省自然科学基金资助项目(2003D0011) 中国博士后科学基金(2004036295)联合资助
关键词 硫酸盐气溶胶 辐射强迫 在线模拟 固定转化率模拟 Sulfate aerosol direct radiative forcing on-line simulation constant transmission simulation
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  • 1杨健,吕达仁.2000年北半球平流层、对流层质量交换的季节变化[J].大气科学,2004,28(2):294-300. 被引量:34
  • 2杨健,吕达仁.东亚地区平流层、对流层交换对臭氧分布影响的模拟研究[J].大气科学,2004,28(4):579-588. 被引量:29
  • 3姜大膀,王会军,郎咸梅.SRES A2情景下中国气候未来变化的多模式集合预测结果[J].地球物理学报,2004,47(5):776-784. 被引量:110
  • 4IPCC, Climate Change: The scientific basis, contribution of working group Ⅰ to the third assessment report of the intergovernmental panel on climate change[M].Cambridge: Cambridge University Press. 2001.
  • 5STOTT P A,TETT S F B, JONES G S,et al. Attribution of twentieth century temperature change to natural and anthropogenic causes[J]. Climate Dynamics, 2001, 17: 1-21.
  • 6GAO Xuejie, ZHAO Zongci, DINGYihui. Climate change due to greenhouse effects in China as simulated by a regional climate model[J]. Advance in Atmospheric Science, 2001, 18:1 224-1 230.
  • 7SANTER B D, MIKOLAJEWlCZU, BRUGEMANNW, et al. Ocean variability and its influence on the detectability of greenhouse warming signal [J]. J Geophys Res, 1995, 100:10 693-10 725.
  • 8SANTER B D, WIGLEY T M L, GAFFEN D J, et al. Interpreting differential temperature trends at the surface and in the lower troposphere[J]. Science, 2000a, 287:1 227-1 232.
  • 9HOLTON J R, HAYNES P H, MCLNTYRE M E, et al. Stratosphere-troposphere exchange[J]. Rev of Geophye, 1995, 33: 403-439.
  • 10OLSEN M A, SCHOEBERL M R, DOUGLASS A R. Stratosphere-troposphere exchange of mass and ozone[J]. J Geophys Res, 2004, 109,D24114, doi:10.1029/2004JD005186.

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