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查一下这篇文章是否被EI检索，如果检索，麻烦列出检索的详细信息，谢谢！ Su Xing-tao, Wang Han-jie, Zhou Lin. Simulation on temporal and spatial distribution and direct radiative forcing of carbonaceous aerosols over China. Journal of PLA University of Science and Technology (Natural Science Edition), 2010, 11(3): 365-370. |
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suxingtao(金币+10):非常感谢！ 2011-01-11 12:59:12
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Accession number: 20103013098941 Title: Simulation on temporal and spatial distribution and direct radiative forcing of carbonaceous aerosols over China Authors: Su, Xing-Tao1 ; Wang, Han-Jie2 ; Zhou, Lin1 Author affiliation: 1 Institute of Meteorology, PLA Univ. of Sci. and Tech., Nanjing 211101, China 2 Key Laboratory of Regional Climate-Environment Research for Temperate East Asia, Chinese Academy of Sciences, Beijing 100029, China Corresponding author: Zhou, L. (zhou_lin4458@163.com) Source title: Jiefangjun Ligong Daxue Xuebao/Journal of PLA University of Science and Technology (Natural Science Edition) Abbreviated source title: Jiefangjun Ligong Daxue Xuebao Volume: 11 Issue: 3 Issue date: June 2010 Publication year: 2010 Pages: 365-370 Language: Chinese ISSN: 10093443 Document type: Journal article (JA) Publisher: University of Science and Technology, No.1 Haifuxiang, Nanjing, 210007, China Abstract: To enhance understanding on the carbonaceous aerosols over China, aerosol data from International Center for Theoretical Physics (ICTP) and regional climate model RegCM3 were used to simulate the temporal and spatial distribution and radiative forcing of the carbonaceous aerosols in 2000. The preliminary results show that carbonaceous aerosols are mostly concentrated in the area of the south of Yellow River and the east of Tibetan Plateau. Referring to the seasonal variation characteristics, the simulation indicates that the maximum value of column burden of the carbonaceous aerosols appears in spring, the second value in winter and the minimum in summer. The radiative forcing of the carbonaceous aerosols is positive on the top of atmosphere (TOA) besides eastern littoral and negative on the ground. The complex mutual action exists in different kinds of aerosols, which indicates that experiments on the distribution and climate effects of aerosols should not add the effects of single aerosols. Number of references: 13 Main heading: Atmospheric aerosols Controlled terms: Climate models - Size distribution Uncontrolled terms: Carbonaceous aerosol - Climate effects - Direct radiative forcing - Maximum values - Radiative forcings - Regional climate models - Seasonal variation - Temporal and spatial distribution - Theoretical physics - Tibetan Plateau - Top of atmospheres - Yellow river Classification code: 931.2 Physical Properties of Gases, Liquids and Solids - 922.2 Mathematical Statistics - 921 Mathematics - 804.2 Inorganic Compounds - 804.1 Organic Compounds - 933.1 Crystalline Solids - 801.3 Colloid Chemistry - 451.1 Air Pollution Sources - 443.1 Atmospheric Properties - 443 Meteorology - 423 Non Mechanical Properties and Tests of Building Materials - 531.2 Metallography Database: Compendex Compilation and indexing terms, © 2010 Elsevier Inc. |
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