Analytical Studies of the Cloud Droplet Spectral Dispersion Influence on the First Indirect Aerosol Effect
Atmospheric aerosols （acting as cloud condensation nuclei） can enhance the cloud droplet number concentration and reduce the cloud droplet size, and in turn affect the cloud optical depth, as well as the cloud albedo, and thereby exert a radiative influence on climate （the first indirect aerosol eff...
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| Veröffentlicht in: | Advances in atmospheric sciences 2013-09, Vol.30 (5), p.1313-1319 |
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| description | Atmospheric aerosols （acting as cloud condensation nuclei） can enhance the cloud droplet number concentration and reduce the cloud droplet size, and in turn affect the cloud optical depth, as well as the cloud albedo, and thereby exert a radiative influence on climate （the first indirect aerosol effect）. In this paper, based on various relationships between cloud droplet spectral dispersion （c） and cloud droplet number concentration （Nc）, we analytically derive the corresponding expressions of the cloud radiative forcing induced by changes in the cloud droplet number concentration. Further quantitative evaluation indicates that the cloud radiative forcing induced by aerosols for the different ~-Nc relationships varies from -29.1% to 25.2%, compared to the case without considering spectral dispersion （e = 0）. Our results suggest that an accurate description of e - Nc relationships helps to reduce the uncertainty of the first indirect aerosol effect and advances our scientific understanding of aerosol-cloud-radiation interactions. |
| doi_str_mv | 10.1007/s00376-012-2141-5 |
| format | Article |
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In this paper, based on various relationships between cloud droplet spectral dispersion （c） and cloud droplet number concentration （Nc）, we analytically derive the corresponding expressions of the cloud radiative forcing induced by changes in the cloud droplet number concentration. Further quantitative evaluation indicates that the cloud radiative forcing induced by aerosols for the different ~-Nc relationships varies from -29.1% to 25.2%, compared to the case without considering spectral dispersion （e = 0）. Our results suggest that an accurate description of e - Nc relationships helps to reduce the uncertainty of the first indirect aerosol effect and advances our scientific understanding of aerosol-cloud-radiation interactions.</description><identifier>ISSN: 0256-1530</identifier><identifier>EISSN: 1861-9533</identifier><identifier>DOI: 10.1007/s00376-012-2141-5</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Aerosols ; Albedo ; Atmospheric Sciences ; Atmospherics ; Clouds ; Dispersions ; Droplets ; Earth and Environmental Science ; Earth Sciences ; Geophysics/Geodesy ; Mathematical analysis ; Meteorology ; Optical analysis ; Radiative forcing ; Spectra ; 云凝结核 ; 云滴谱 ; 云辐射强迫 ; 光谱 ; 大气气溶胶 ; 数浓度 ; 色散 ; 间接</subject><ispartof>Advances in atmospheric sciences, 2013-09, Vol.30 (5), p.1313-1319</ispartof><rights>Chinese National Committee for International Association of Meteorology and Atmospheric Sciences, Institute of Atmospheric Physics, Science Press and Springer-Verlag Berlin Heidelberg 2013</rights><rights>Copyright © Wanfang Data Co. 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Atmos. Sci</addtitle><addtitle>Advances in Atmospheric Sciences</addtitle><description>Atmospheric aerosols （acting as cloud condensation nuclei） can enhance the cloud droplet number concentration and reduce the cloud droplet size, and in turn affect the cloud optical depth, as well as the cloud albedo, and thereby exert a radiative influence on climate （the first indirect aerosol effect）. In this paper, based on various relationships between cloud droplet spectral dispersion （c） and cloud droplet number concentration （Nc）, we analytically derive the corresponding expressions of the cloud radiative forcing induced by changes in the cloud droplet number concentration. Further quantitative evaluation indicates that the cloud radiative forcing induced by aerosols for the different ~-Nc relationships varies from -29.1% to 25.2%, compared to the case without considering spectral dispersion （e = 0）. Our results suggest that an accurate description of e - Nc relationships helps to reduce the uncertainty of the first indirect aerosol effect and advances our scientific understanding of aerosol-cloud-radiation interactions.</description><subject>Aerosols</subject><subject>Albedo</subject><subject>Atmospheric Sciences</subject><subject>Atmospherics</subject><subject>Clouds</subject><subject>Dispersions</subject><subject>Droplets</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geophysics/Geodesy</subject><subject>Mathematical analysis</subject><subject>Meteorology</subject><subject>Optical analysis</subject><subject>Radiative forcing</subject><subject>Spectra</subject><subject>云凝结核</subject><subject>云滴谱</subject><subject>云辐射强迫</subject><subject>光谱</subject><subject>大气气溶胶</subject><subject>数浓度</subject><subject>色散</subject><subject>间接</subject><issn>0256-1530</issn><issn>1861-9533</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNqFkUtv1DAUhSMEEkPhB7AzYkMXAV8_kng5mrZQqRKLtmvLY99MM6Rxxk4E7a_njlJViAWsrGt959zHKYr3wD8D5_WXzLmsq5KDKAUoKPWLYgVNBaXRUr4sVlzoqgQt-eviTc57oo1sYFXs14PrH6bOu55dT3PoMLPYsukO2aaPc2BnKY49Tux6RD8los66PGLKXRzY5dD2Mw4eGRVHyUWX8kTfoUtEszWmmGPPztuWyrfFq9b1Gd89vSfF7cX5zeZbefX96-VmfVV6pcRUNlvExnjUKF1onPGmUltFOwIPymy9MjI4x1UIKKoWatVsZR0E4cI0jXPypDhdfH-6oXXDzu7jnGjLbMPhx6_9o0XBQXJNlsR-WtgxxcOMebL3XfbY927AOGcLVQ2qqWQN_0eVkhRBbTihH_9Cn0cAJRTNqatjb1goT1fKCVs7pu7epQcL3B5DtUuolkK1x1CtJo1YNJnYYYfpD-d_iD48NbqLw-5AuudOqjKgDQj5G5e_rn0</recordid><startdate>20130901</startdate><enddate>20130901</enddate><creator>解小宁 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forcing</topic><topic>Spectra</topic><topic>云凝结核</topic><topic>云滴谱</topic><topic>云辐射强迫</topic><topic>光谱</topic><topic>大气气溶胶</topic><topic>数浓度</topic><topic>色散</topic><topic>间接</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>解小宁 刘晓东</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Military Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One 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Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>解小宁 刘晓东</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Analytical Studies of the Cloud Droplet Spectral Dispersion Influence on the First Indirect Aerosol Effect</atitle><jtitle>Advances in atmospheric sciences</jtitle><stitle>Adv. Atmos. Sci</stitle><addtitle>Advances in Atmospheric Sciences</addtitle><date>2013-09-01</date><risdate>2013</risdate><volume>30</volume><issue>5</issue><spage>1313</spage><epage>1319</epage><pages>1313-1319</pages><issn>0256-1530</issn><eissn>1861-9533</eissn><abstract>Atmospheric aerosols （acting as cloud condensation nuclei） can enhance the cloud droplet number concentration and reduce the cloud droplet size, and in turn affect the cloud optical depth, as well as the cloud albedo, and thereby exert a radiative influence on climate （the first indirect aerosol effect）. In this paper, based on various relationships between cloud droplet spectral dispersion （c） and cloud droplet number concentration （Nc）, we analytically derive the corresponding expressions of the cloud radiative forcing induced by changes in the cloud droplet number concentration. Further quantitative evaluation indicates that the cloud radiative forcing induced by aerosols for the different ~-Nc relationships varies from -29.1% to 25.2%, compared to the case without considering spectral dispersion （e = 0）. Our results suggest that an accurate description of e - Nc relationships helps to reduce the uncertainty of the first indirect aerosol effect and advances our scientific understanding of aerosol-cloud-radiation interactions.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00376-012-2141-5</doi><tpages>7</tpages></addata></record> |
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| ispartof | Advances in atmospheric sciences, 2013-09, Vol.30 (5), p.1313-1319 |
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| subjects | Aerosols Albedo Atmospheric Sciences Atmospherics Clouds Dispersions Droplets Earth and Environmental Science Earth Sciences Geophysics/Geodesy Mathematical analysis Meteorology Optical analysis Radiative forcing Spectra 云凝结核 云滴谱 云辐射强迫 光谱 大气气溶胶 数浓度 色散 间接 |
| title | Analytical Studies of the Cloud Droplet Spectral Dispersion Influence on the First Indirect Aerosol Effect |
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