An Evidence of Aerosol Indirect Effect on Stratus Clouds from the Integrated Ground-Based Measurements at the ARM Shouxian Site
The aerosol effect on clouds was explored using remote sensing of aerosol and cloud data at Shouxian, China. Non-precipitation, ice-free, and overcast clouds were firstly chosen by a combination of sky im- ages from the Total Sky Imager （TSI）, cloud base heights from the Ceilometer, and vertical tem...
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| creator | TANG Jin-Ping WANG Pu-Cai DUAN Min-Zheng CHEN Hong-Bin XIA Xiang-Ao LIAO Hong |
| description | The aerosol effect on clouds was explored using remote sensing of aerosol and cloud data at Shouxian, China. Non-precipitation, ice-free, and overcast clouds were firstly chosen by a combination of sky im- ages from the Total Sky Imager （TSI）, cloud base heights from the Ceilometer, and vertical temperature profiles from the Balloon-Borne Sounding System （BBSS）. Six cases were chosen in summer, and seven in autumn. The averaged cloud effective radii （re）, cloud optical depth （COD）, aerosol total light scattering coefficient （a）, and liquid water path （LWP） are, respectivey, 6.47 μm, 35.4, 595.9 mm-1, 0.19 mm in summer, and 6.07 μm, 96.0, 471.7 mm-1, 0.37 mm in autumn. The correlation coefficient between re and tc was found to change from negative to positive value as LWP increases. |
| doi_str_mv | 10.1080/16742834.2011.11446905 |
| format | Article |
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Non-precipitation, ice-free, and overcast clouds were firstly chosen by a combination of sky im- ages from the Total Sky Imager （TSI）, cloud base heights from the Ceilometer, and vertical temperature profiles from the Balloon-Borne Sounding System （BBSS）. Six cases were chosen in summer, and seven in autumn. The averaged cloud effective radii （re）, cloud optical depth （COD）, aerosol total light scattering coefficient （a）, and liquid water path （LWP） are, respectivey, 6.47 μm, 35.4, 595.9 mm-1, 0.19 mm in summer, and 6.07 μm, 96.0, 471.7 mm-1, 0.37 mm in autumn. The correlation coefficient between re and tc was found to change from negative to positive value as LWP increases.</description><identifier>ISSN: 1674-2834</identifier><identifier>EISSN: 2376-6123</identifier><identifier>DOI: 10.1080/16742834.2011.11446905</identifier><language>eng</language><publisher>Beijing: Routledge</publisher><subject>aerosol ; Aerosols ; ARM ; Autumn ; Balloons ; Clouds ; Correlation coefficient ; effective radius ; Hydrologic data ; Ice ; Light scattering ; liquid water path ; Optical analysis ; optical depth ; Profiles ; Remote sensing ; Scattering coefficient ; Summer ; Temperature ; Temperature profile ; warm cloud ; Water depth ; 化学需氧量 ; 地面测量 ; 寿县 ; 气溶胶 ; 网站 ; 证据 ; 间接效应</subject><ispartof>Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao, 2011, Vol.4 (2), p.65-69</ispartof><rights>Institute of Atmospheric Physics, Chinese Academy of Sciences 2011</rights><rights>Institute of Atmospheric Physics, Chinese Academy of Sciences. 2011</rights><rights>Copyright © Wanfang Data Co. 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Non-precipitation, ice-free, and overcast clouds were firstly chosen by a combination of sky im- ages from the Total Sky Imager （TSI）, cloud base heights from the Ceilometer, and vertical temperature profiles from the Balloon-Borne Sounding System （BBSS）. Six cases were chosen in summer, and seven in autumn. The averaged cloud effective radii （re）, cloud optical depth （COD）, aerosol total light scattering coefficient （a）, and liquid water path （LWP） are, respectivey, 6.47 μm, 35.4, 595.9 mm-1, 0.19 mm in summer, and 6.07 μm, 96.0, 471.7 mm-1, 0.37 mm in autumn. The correlation coefficient between re and tc was found to change from negative to positive value as LWP increases.</description><subject>aerosol</subject><subject>Aerosols</subject><subject>ARM</subject><subject>Autumn</subject><subject>Balloons</subject><subject>Clouds</subject><subject>Correlation coefficient</subject><subject>effective radius</subject><subject>Hydrologic data</subject><subject>Ice</subject><subject>Light scattering</subject><subject>liquid water path</subject><subject>Optical analysis</subject><subject>optical depth</subject><subject>Profiles</subject><subject>Remote sensing</subject><subject>Scattering coefficient</subject><subject>Summer</subject><subject>Temperature</subject><subject>Temperature profile</subject><subject>warm cloud</subject><subject>Water depth</subject><subject>化学需氧量</subject><subject>地面测量</subject><subject>寿县</subject><subject>气溶胶</subject><subject>网站</subject><subject>证据</subject><subject>间接效应</subject><issn>1674-2834</issn><issn>2376-6123</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqFkV9r2zAUxcXYYCHrVxgaexs40x9bth-9kHWFlsG6PQtZuordJlIjyW3ztK8-eWnY40BwEfrdc67OReg9JStKGvKZirpkDS9XjFC6orQsRUuqV2jBeC0KQRl_jRYzVMzUW3QR4x0hhHImasIX6Hfn8OZxNOA0YG9xB8FHv8NXzowBdMIba-fiHb5NQaUp4vXOTyZiG_wepwEymmCbn8Dgy-AnZ4ovKubLDag4BdiDSxGr9Jftftzg28FPz6PKgmOCd-iNVbsIFy91iX593fxcfyuuv19erbvrQpcVSYVm3FIKhvRt2QvDRGsbXbcVhx44I6pifSNonrTUIEoCKp-m1qTVprWmrvgSfTrpPilnldvKOz8Flx2lOQzD8f75vp8TJGzOZok-nuCH4A8TxPSPZoxWrGxb1mZKnCidI4sBrHwI416Fo6REzsuR5-XIWVqel5Mbu1Pj6KwPe_Xkw87IpI47H2xQTo9R8v9qfHgxH7zbHsb8o7M7b2jFqWD8D4DBoU8</recordid><startdate>2011</startdate><enddate>2011</enddate><creator>TANG 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Shouxian Site</atitle><jtitle>Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao</jtitle><addtitle>Atmospheric and Oceanic Science Letters</addtitle><date>2011</date><risdate>2011</risdate><volume>4</volume><issue>2</issue><spage>65</spage><epage>69</epage><pages>65-69</pages><issn>1674-2834</issn><eissn>2376-6123</eissn><abstract>The aerosol effect on clouds was explored using remote sensing of aerosol and cloud data at Shouxian, China. 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| ispartof | Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao, 2011, Vol.4 (2), p.65-69 |
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| language | eng |
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| source | Taylor & Francis Open Access |
| subjects | aerosol Aerosols ARM Autumn Balloons Clouds Correlation coefficient effective radius Hydrologic data Ice Light scattering liquid water path Optical analysis optical depth Profiles Remote sensing Scattering coefficient Summer Temperature Temperature profile warm cloud Water depth 化学需氧量 地面测量 寿县 气溶胶 网站 证据 间接效应 |
| title | An Evidence of Aerosol Indirect Effect on Stratus Clouds from the Integrated Ground-Based Measurements at the ARM Shouxian Site |
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