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Vertical profiles of tropospheric gases: Chemical consequences of stratospheric intrusions
The M.R.F. Hercules aircraft was used to obtain two vertical profiles of minor atmospheric constituents in a stationary low pressure circulation over the N. Atlantic. Results for CFCl 3, CF 2Cl 2, N 2O, C 2H 2, C 2H 6, C 3H 8, C 4H 10 and O 3 are presented, and interpreted by means of air parcel bac...
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| Published in: | Atmospheric environment 1984, Vol.18 (9), p.1759-1766 |
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| Main Authors: | , , , , , |
| Format: | Article |
| Language: | English |
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| cited_by | cdi_FETCH-LOGICAL-c395t-2564bdba3a69eccfd3235254e8bce4fd78aa5c5fe4de77592efb96dc241ea35c3 |
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| cites | cdi_FETCH-LOGICAL-c395t-2564bdba3a69eccfd3235254e8bce4fd78aa5c5fe4de77592efb96dc241ea35c3 |
| container_end_page | 1766 |
| container_issue | 9 |
| container_start_page | 1759 |
| container_title | Atmospheric environment |
| container_volume | 18 |
| creator | Bamber, D.J. Healey, P.G.W. Jones, B.M.R. Penkett, S.A. Tuck, A.F. Vaughan, G. |
| description | The M.R.F. Hercules aircraft was used to obtain two vertical profiles of minor atmospheric constituents in a stationary low pressure circulation over the N. Atlantic. Results for CFCl
3, CF
2Cl
2, N
2O, C
2H
2, C
2H
6, C
3H
8, C
4H
10 and O
3 are presented, and interpreted by means of air parcel back trajectories on isentropic surfaces. Substantial evidence was found for air of stratospheric origin in the upper troposphere on the second flight, and the data from both flights point to an enhancement in OH concentrations, and thus hydrocarbon depletion rates, following mixing between stratospheric and tropospheric air. |
| doi_str_mv | 10.1016/0004-6981(84)90351-2 |
| format | article |
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3, CF
2Cl
2, N
2O, C
2H
2, C
2H
6, C
3H
8, C
4H
10 and O
3 are presented, and interpreted by means of air parcel back trajectories on isentropic surfaces. Substantial evidence was found for air of stratospheric origin in the upper troposphere on the second flight, and the data from both flights point to an enhancement in OH concentrations, and thus hydrocarbon depletion rates, following mixing between stratospheric and tropospheric air.</description><identifier>ISSN: 0004-6981</identifier><identifier>DOI: 10.1016/0004-6981(84)90351-2</identifier><identifier>CODEN: ATENBP</identifier><language>eng</language><publisher>Oxford: Elsevier B.V</publisher><subject>Applied sciences ; Atmospheric pollution ; Exact sciences and technology ; Pollutants physicochemistry study: properties, effects, reactions, transport and distribution ; Pollution</subject><ispartof>Atmospheric environment, 1984, Vol.18 (9), p.1759-1766</ispartof><rights>1984</rights><rights>1985 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c395t-2564bdba3a69eccfd3235254e8bce4fd78aa5c5fe4de77592efb96dc241ea35c3</citedby><cites>FETCH-LOGICAL-c395t-2564bdba3a69eccfd3235254e8bce4fd78aa5c5fe4de77592efb96dc241ea35c3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/0004698184903512$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>309,310,314,780,784,789,790,3480,4022,4048,4049,23929,23930,25139,27922,27923,27924,45992</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=8974912$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Bamber, D.J.</creatorcontrib><creatorcontrib>Healey, P.G.W.</creatorcontrib><creatorcontrib>Jones, B.M.R.</creatorcontrib><creatorcontrib>Penkett, S.A.</creatorcontrib><creatorcontrib>Tuck, A.F.</creatorcontrib><creatorcontrib>Vaughan, G.</creatorcontrib><title>Vertical profiles of tropospheric gases: Chemical consequences of stratospheric intrusions</title><title>Atmospheric environment</title><description>The M.R.F. Hercules aircraft was used to obtain two vertical profiles of minor atmospheric constituents in a stationary low pressure circulation over the N. Atlantic. Results for CFCl
3, CF
2Cl
2, N
2O, C
2H
2, C
2H
6, C
3H
8, C
4H
10 and O
3 are presented, and interpreted by means of air parcel back trajectories on isentropic surfaces. Substantial evidence was found for air of stratospheric origin in the upper troposphere on the second flight, and the data from both flights point to an enhancement in OH concentrations, and thus hydrocarbon depletion rates, following mixing between stratospheric and tropospheric air.</description><subject>Applied sciences</subject><subject>Atmospheric pollution</subject><subject>Exact sciences and technology</subject><subject>Pollutants physicochemistry study: properties, effects, reactions, transport and distribution</subject><subject>Pollution</subject><issn>0004-6981</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1984</creationdate><recordtype>article</recordtype><recordid>eNqFkMtKw0AUhrNQsFbfwEUWIrqIzjXJuBCkeIOCG3XhZphMztiRNIlzUsG3d9KWLnV14PD95_IlyQkll5TQ_IoQIrJclfS8FBeKcEkztpdMdu2D5BDxkxDGS6YmyfsbhMFb06R96JxvANPOpUPo-g77BQRv0w-DgNfpbAHLNWi7FuFrBa3dwDgEM-xo3w5hhT4yR8m-Mw3C8bZOk9f7u5fZYzZ_fnia3c4zy5UcMiZzUdWV4SZXYK2rOeOSSQFlZUG4uiiNkVY6EDUUhVQMXKXy2jJBwXBp-TQ528yNH8SzcNBLjxaaxrTQrVAzIRRVXP4L0pJHKZxEUGxAGzrEAE73wS9N-NGU6NGyHnXqUacuhV5b1izGTrfzDUZRLpjWetxlS1XEQ0bsZoNBlPLtIWi0frRZ-wB20HXn_97zC1BslTs</recordid><startdate>1984</startdate><enddate>1984</enddate><creator>Bamber, D.J.</creator><creator>Healey, P.G.W.</creator><creator>Jones, B.M.R.</creator><creator>Penkett, S.A.</creator><creator>Tuck, A.F.</creator><creator>Vaughan, G.</creator><general>Elsevier B.V</general><general>Pergamon Press</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>1984</creationdate><title>Vertical profiles of tropospheric gases: Chemical consequences of stratospheric intrusions</title><author>Bamber, D.J. ; Healey, P.G.W. ; Jones, B.M.R. ; Penkett, S.A. ; Tuck, A.F. ; Vaughan, G.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c395t-2564bdba3a69eccfd3235254e8bce4fd78aa5c5fe4de77592efb96dc241ea35c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1984</creationdate><topic>Applied sciences</topic><topic>Atmospheric pollution</topic><topic>Exact sciences and technology</topic><topic>Pollutants physicochemistry study: properties, effects, reactions, transport and distribution</topic><topic>Pollution</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bamber, D.J.</creatorcontrib><creatorcontrib>Healey, P.G.W.</creatorcontrib><creatorcontrib>Jones, B.M.R.</creatorcontrib><creatorcontrib>Penkett, S.A.</creatorcontrib><creatorcontrib>Tuck, A.F.</creatorcontrib><creatorcontrib>Vaughan, G.</creatorcontrib><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><jtitle>Atmospheric environment</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bamber, D.J.</au><au>Healey, P.G.W.</au><au>Jones, B.M.R.</au><au>Penkett, S.A.</au><au>Tuck, A.F.</au><au>Vaughan, G.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Vertical profiles of tropospheric gases: Chemical consequences of stratospheric intrusions</atitle><jtitle>Atmospheric environment</jtitle><date>1984</date><risdate>1984</risdate><volume>18</volume><issue>9</issue><spage>1759</spage><epage>1766</epage><pages>1759-1766</pages><issn>0004-6981</issn><coden>ATENBP</coden><abstract>The M.R.F. Hercules aircraft was used to obtain two vertical profiles of minor atmospheric constituents in a stationary low pressure circulation over the N. Atlantic. Results for CFCl
3, CF
2Cl
2, N
2O, C
2H
2, C
2H
6, C
3H
8, C
4H
10 and O
3 are presented, and interpreted by means of air parcel back trajectories on isentropic surfaces. Substantial evidence was found for air of stratospheric origin in the upper troposphere on the second flight, and the data from both flights point to an enhancement in OH concentrations, and thus hydrocarbon depletion rates, following mixing between stratospheric and tropospheric air.</abstract><cop>Oxford</cop><cop>New York, NY</cop><pub>Elsevier B.V</pub><doi>10.1016/0004-6981(84)90351-2</doi><tpages>8</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0004-6981 |
| ispartof | Atmospheric environment, 1984, Vol.18 (9), p.1759-1766 |
| issn | 0004-6981 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_24491935 |
| source | Backfile Package - Environmental Science (Legacy) [YES] |
| subjects | Applied sciences Atmospheric pollution Exact sciences and technology Pollutants physicochemistry study: properties, effects, reactions, transport and distribution Pollution |
| title | Vertical profiles of tropospheric gases: Chemical consequences of stratospheric intrusions |
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