A comparison of large-scale atmospheric sulphate aerosol models (COSAM): overview and highlights
The comparison of large-scale sulphate aerosol models study (COSAM) compared the performance of atmospheric models with each other and observations. It involved: (i) design of a standard model experiment for the world wide web, (ii) 10 model simulations of the cycles of sulphur and 222 Rn/ 210 Pb co...
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Veröffentlicht in: | Tellus Series B, Chemical and Physical Meteorology, 53(5):615-645 Chemical and Physical Meteorology, 53(5):615-645, 2001-11, Vol.53 (5), p.615-645 |
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creator | Barrie, L. A. Yi, Y. Leaitch, W. R. Lohmann, U. Kasibhatla, P. Roelofs, G.-J. Wilson, J. McGovern, F. Benkovitz, C. Méliéres, M. A. Law, K. Prospero, J. Kritz, M. Bergmann, D. Bridgeman, C. Chin, M. Christensen, J. Easter, R. Feichter, J. Land, C. Jeuken, A. Kjellström, E. Koch, D. Rasch, P. |
description | The comparison of large-scale sulphate aerosol models study (COSAM) compared the performance of atmospheric models with each other and observations. It involved: (i) design of a standard model experiment for the world wide web, (ii) 10 model simulations of the cycles of sulphur and
222
Rn/
210
Pb conforming to the experimental design, (iii) assemblage of the best available observations of atmospheric SO
=
4
, SO
2
and MSA and (iv) a workshop in Halifax, Canada to analyze model performance and future model development needs. The analysis presented in this paper and two companion papers by Roelofs, and Lohmann and co-workers examines the variance between models and observations, discusses the sources of that variance and suggests ways to improve models. Variations between models in the export of SO
x
from Europe or North America are not sufficient to explain an order of magnitude variation in spatial distributions of SO
x
downwind in the northern hemisphere. On average, models predicted surface level seasonal mean SO
=
4
aerosol mixing ratios better (most within 20%) than SO
2
mixing ratios (over-prediction by factors of 2 or more). Results suggest that vertical mixing from the planetary boundary layer into the free troposphere in source regions is a major source of uncertainty in predicting the global distribution of SO
=
4
aerosols in climate models today. For improvement, it is essential that globally coordinated research efforts continue to address emissions of all atmospheric species that affect the distribution and optical properties of ambient aerosols in models and that a global network of observations be established that will ultimately produce a world aerosol chemistry climatology. |
doi_str_mv | 10.3402/tellusb.v53i5.16642 |
format | Article |
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222
Rn/
210
Pb conforming to the experimental design, (iii) assemblage of the best available observations of atmospheric SO
=
4
, SO
2
and MSA and (iv) a workshop in Halifax, Canada to analyze model performance and future model development needs. The analysis presented in this paper and two companion papers by Roelofs, and Lohmann and co-workers examines the variance between models and observations, discusses the sources of that variance and suggests ways to improve models. Variations between models in the export of SO
x
from Europe or North America are not sufficient to explain an order of magnitude variation in spatial distributions of SO
x
downwind in the northern hemisphere. On average, models predicted surface level seasonal mean SO
=
4
aerosol mixing ratios better (most within 20%) than SO
2
mixing ratios (over-prediction by factors of 2 or more). Results suggest that vertical mixing from the planetary boundary layer into the free troposphere in source regions is a major source of uncertainty in predicting the global distribution of SO
=
4
aerosols in climate models today. For improvement, it is essential that globally coordinated research efforts continue to address emissions of all atmospheric species that affect the distribution and optical properties of ambient aerosols in models and that a global network of observations be established that will ultimately produce a world aerosol chemistry climatology.</description><identifier>ISSN: 0280-6509</identifier><identifier>EISSN: 1600-0889</identifier><identifier>DOI: 10.3402/tellusb.v53i5.16642</identifier><identifier>CODEN: TSBMD7</identifier><language>eng</language><publisher>Oxford: Taylor & Francis</publisher><subject>AEROSOLS ; BOUNDARY LAYERS ; CHEMISTRY ; CLIMATE MODELS ; DESIGN ; DISTRIBUTION ; Earth, ocean, space ; ENVIRONMENTAL SCIENCES ; Exact sciences and technology ; EXPORTS ; External geophysics ; Geophysics. Techniques, methods, instrumentation and models ; Meteorology ; MIXING RATIO ; OPTICAL PROPERTIES ; Particles and aerosols ; PHYSICS OF ELEMENTARY PARTICLES AND FIELDS ; SPATIAL DISTRIBUTION ; STANDARD MODEL ; TROPOSPHERE</subject><ispartof>Tellus Series B, Chemical and Physical Meteorology, 53(5):615-645, 2001-11, Vol.53 (5), p.615-645</ispartof><rights>2001 The Author(s). Published by Taylor & Francis. 2001</rights><rights>2002 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3822-22bacd12a0884bce13f7e34c5b772048b7b87e203b0ac3a90334bd7219c482873</citedby><cites>FETCH-LOGICAL-c3822-22bacd12a0884bce13f7e34c5b772048b7b87e203b0ac3a90334bd7219c482873</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.tandfonline.com/doi/pdf/10.3402/tellusb.v53i5.16642$$EPDF$$P50$$Ginformaworld$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.tandfonline.com/doi/full/10.3402/tellusb.v53i5.16642$$EHTML$$P50$$Ginformaworld$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,885,4139,27502,27924,27925,59143,59144</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=14087621$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.osti.gov/biblio/15001732$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Barrie, L. A.</creatorcontrib><creatorcontrib>Yi, Y.</creatorcontrib><creatorcontrib>Leaitch, W. R.</creatorcontrib><creatorcontrib>Lohmann, U.</creatorcontrib><creatorcontrib>Kasibhatla, P.</creatorcontrib><creatorcontrib>Roelofs, G.-J.</creatorcontrib><creatorcontrib>Wilson, J.</creatorcontrib><creatorcontrib>McGovern, F.</creatorcontrib><creatorcontrib>Benkovitz, C.</creatorcontrib><creatorcontrib>Méliéres, M. A.</creatorcontrib><creatorcontrib>Law, K.</creatorcontrib><creatorcontrib>Prospero, J.</creatorcontrib><creatorcontrib>Kritz, M.</creatorcontrib><creatorcontrib>Bergmann, D.</creatorcontrib><creatorcontrib>Bridgeman, C.</creatorcontrib><creatorcontrib>Chin, M.</creatorcontrib><creatorcontrib>Christensen, J.</creatorcontrib><creatorcontrib>Easter, R.</creatorcontrib><creatorcontrib>Feichter, J.</creatorcontrib><creatorcontrib>Land, C.</creatorcontrib><creatorcontrib>Jeuken, A.</creatorcontrib><creatorcontrib>Kjellström, E.</creatorcontrib><creatorcontrib>Koch, D.</creatorcontrib><creatorcontrib>Rasch, P.</creatorcontrib><creatorcontrib>Pacific Northwest National Lab. (PNNL), Richland, WA (United States)</creatorcontrib><title>A comparison of large-scale atmospheric sulphate aerosol models (COSAM): overview and highlights</title><title>Tellus Series B, Chemical and Physical Meteorology, 53(5):615-645</title><description>The comparison of large-scale sulphate aerosol models study (COSAM) compared the performance of atmospheric models with each other and observations. It involved: (i) design of a standard model experiment for the world wide web, (ii) 10 model simulations of the cycles of sulphur and
222
Rn/
210
Pb conforming to the experimental design, (iii) assemblage of the best available observations of atmospheric SO
=
4
, SO
2
and MSA and (iv) a workshop in Halifax, Canada to analyze model performance and future model development needs. The analysis presented in this paper and two companion papers by Roelofs, and Lohmann and co-workers examines the variance between models and observations, discusses the sources of that variance and suggests ways to improve models. Variations between models in the export of SO
x
from Europe or North America are not sufficient to explain an order of magnitude variation in spatial distributions of SO
x
downwind in the northern hemisphere. On average, models predicted surface level seasonal mean SO
=
4
aerosol mixing ratios better (most within 20%) than SO
2
mixing ratios (over-prediction by factors of 2 or more). Results suggest that vertical mixing from the planetary boundary layer into the free troposphere in source regions is a major source of uncertainty in predicting the global distribution of SO
=
4
aerosols in climate models today. For improvement, it is essential that globally coordinated research efforts continue to address emissions of all atmospheric species that affect the distribution and optical properties of ambient aerosols in models and that a global network of observations be established that will ultimately produce a world aerosol chemistry climatology.</description><subject>AEROSOLS</subject><subject>BOUNDARY LAYERS</subject><subject>CHEMISTRY</subject><subject>CLIMATE MODELS</subject><subject>DESIGN</subject><subject>DISTRIBUTION</subject><subject>Earth, ocean, space</subject><subject>ENVIRONMENTAL SCIENCES</subject><subject>Exact sciences and technology</subject><subject>EXPORTS</subject><subject>External geophysics</subject><subject>Geophysics. Techniques, methods, instrumentation and models</subject><subject>Meteorology</subject><subject>MIXING RATIO</subject><subject>OPTICAL PROPERTIES</subject><subject>Particles and aerosols</subject><subject>PHYSICS OF ELEMENTARY PARTICLES AND FIELDS</subject><subject>SPATIAL DISTRIBUTION</subject><subject>STANDARD MODEL</subject><subject>TROPOSPHERE</subject><issn>0280-6509</issn><issn>1600-0889</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2001</creationdate><recordtype>article</recordtype><sourceid>0YH</sourceid><recordid>eNqFkU9v1DAQxS1EJZaWT8DFEgLBIcv4T2KHQ6XVipZKRT0AZ-M4TmPkxMH2btVvj9tdxI0eRiONfm9m9B5CrwmsGQf6MVvvd6lb72vm6jVpGk6foRVpACqQsn2OVkAlVE0N7Qv0MqVfAMDrtlmhnxtswrTo6FKYcRiw1_HWVslob7HOU0jLaKMzOO38MupchjaGFDyeQm99wu-3N982Xz98wmFv497ZO6znHo_udvSlcjpDJ4P2yb469lP04-Lz9-2X6vrm8mq7ua4Mk5RWlHba9ITq8i_vjCVsEJZxU3dCUOCyE50UlgLrQBumW2CMd72gpDVcUinYKXpz2BtSdioZl60ZTZhna7IiNQARjBbq3YFaYvi9symrySVT3NOzDbukaNPULWPiSZBI1hAq6wKyA2iKLSnaQS3RTTreKwLqIRx1DEc9hqMewymqt8f1-sHqIerZuPRPykGKhpLCnR84Nw8hTvouRN-rrO99iH9F7H-H_gBOEabS</recordid><startdate>20011101</startdate><enddate>20011101</enddate><creator>Barrie, L. 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A. ; Law, K. ; Prospero, J. ; Kritz, M. ; Bergmann, D. ; Bridgeman, C. ; Chin, M. ; Christensen, J. ; Easter, R. ; Feichter, J. ; Land, C. ; Jeuken, A. ; Kjellström, E. ; Koch, D. ; Rasch, P.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3822-22bacd12a0884bce13f7e34c5b772048b7b87e203b0ac3a90334bd7219c482873</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2001</creationdate><topic>AEROSOLS</topic><topic>BOUNDARY LAYERS</topic><topic>CHEMISTRY</topic><topic>CLIMATE MODELS</topic><topic>DESIGN</topic><topic>DISTRIBUTION</topic><topic>Earth, ocean, space</topic><topic>ENVIRONMENTAL SCIENCES</topic><topic>Exact sciences and technology</topic><topic>EXPORTS</topic><topic>External geophysics</topic><topic>Geophysics. Techniques, methods, instrumentation and models</topic><topic>Meteorology</topic><topic>MIXING RATIO</topic><topic>OPTICAL PROPERTIES</topic><topic>Particles and aerosols</topic><topic>PHYSICS OF ELEMENTARY PARTICLES AND FIELDS</topic><topic>SPATIAL DISTRIBUTION</topic><topic>STANDARD MODEL</topic><topic>TROPOSPHERE</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Barrie, L. A.</creatorcontrib><creatorcontrib>Yi, Y.</creatorcontrib><creatorcontrib>Leaitch, W. R.</creatorcontrib><creatorcontrib>Lohmann, U.</creatorcontrib><creatorcontrib>Kasibhatla, P.</creatorcontrib><creatorcontrib>Roelofs, G.-J.</creatorcontrib><creatorcontrib>Wilson, J.</creatorcontrib><creatorcontrib>McGovern, F.</creatorcontrib><creatorcontrib>Benkovitz, C.</creatorcontrib><creatorcontrib>Méliéres, M. 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(PNNL), Richland, WA (United States)</creatorcontrib><collection>Taylor & Francis Open Access</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>OSTI.GOV</collection><jtitle>Tellus Series B, Chemical and Physical Meteorology, 53(5):615-645</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Barrie, L. A.</au><au>Yi, Y.</au><au>Leaitch, W. R.</au><au>Lohmann, U.</au><au>Kasibhatla, P.</au><au>Roelofs, G.-J.</au><au>Wilson, J.</au><au>McGovern, F.</au><au>Benkovitz, C.</au><au>Méliéres, M. A.</au><au>Law, K.</au><au>Prospero, J.</au><au>Kritz, M.</au><au>Bergmann, D.</au><au>Bridgeman, C.</au><au>Chin, M.</au><au>Christensen, J.</au><au>Easter, R.</au><au>Feichter, J.</au><au>Land, C.</au><au>Jeuken, A.</au><au>Kjellström, E.</au><au>Koch, D.</au><au>Rasch, P.</au><aucorp>Pacific Northwest National Lab. (PNNL), Richland, WA (United States)</aucorp><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A comparison of large-scale atmospheric sulphate aerosol models (COSAM): overview and highlights</atitle><jtitle>Tellus Series B, Chemical and Physical Meteorology, 53(5):615-645</jtitle><date>2001-11-01</date><risdate>2001</risdate><volume>53</volume><issue>5</issue><spage>615</spage><epage>645</epage><pages>615-645</pages><issn>0280-6509</issn><eissn>1600-0889</eissn><coden>TSBMD7</coden><abstract>The comparison of large-scale sulphate aerosol models study (COSAM) compared the performance of atmospheric models with each other and observations. It involved: (i) design of a standard model experiment for the world wide web, (ii) 10 model simulations of the cycles of sulphur and
222
Rn/
210
Pb conforming to the experimental design, (iii) assemblage of the best available observations of atmospheric SO
=
4
, SO
2
and MSA and (iv) a workshop in Halifax, Canada to analyze model performance and future model development needs. The analysis presented in this paper and two companion papers by Roelofs, and Lohmann and co-workers examines the variance between models and observations, discusses the sources of that variance and suggests ways to improve models. Variations between models in the export of SO
x
from Europe or North America are not sufficient to explain an order of magnitude variation in spatial distributions of SO
x
downwind in the northern hemisphere. On average, models predicted surface level seasonal mean SO
=
4
aerosol mixing ratios better (most within 20%) than SO
2
mixing ratios (over-prediction by factors of 2 or more). Results suggest that vertical mixing from the planetary boundary layer into the free troposphere in source regions is a major source of uncertainty in predicting the global distribution of SO
=
4
aerosols in climate models today. For improvement, it is essential that globally coordinated research efforts continue to address emissions of all atmospheric species that affect the distribution and optical properties of ambient aerosols in models and that a global network of observations be established that will ultimately produce a world aerosol chemistry climatology.</abstract><cop>Oxford</cop><pub>Taylor & Francis</pub><doi>10.3402/tellusb.v53i5.16642</doi><tpages>31</tpages><oa>free_for_read</oa></addata></record> |
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source | Taylor & Francis Open Access; Co-Action Open Access Journals; Access via Wiley Online Library; EZB-FREE-00999 freely available EZB journals; Alma/SFX Local Collection |
subjects | AEROSOLS BOUNDARY LAYERS CHEMISTRY CLIMATE MODELS DESIGN DISTRIBUTION Earth, ocean, space ENVIRONMENTAL SCIENCES Exact sciences and technology EXPORTS External geophysics Geophysics. Techniques, methods, instrumentation and models Meteorology MIXING RATIO OPTICAL PROPERTIES Particles and aerosols PHYSICS OF ELEMENTARY PARTICLES AND FIELDS SPATIAL DISTRIBUTION STANDARD MODEL TROPOSPHERE |
title | A comparison of large-scale atmospheric sulphate aerosol models (COSAM): overview and highlights |
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