Physical variation of water vapor, and the relation with carbon dioxide
Analysis of the long term NOAA carbon dioxide flask sample records to examine the exchange among the continental Antarctic air mass and other air masses shows a meteorological variation of carbon dioxide concentration. There is an inverse relation between the seasonal variation of carbon dioxide con...
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Veröffentlicht in: | Geophysical research letters 1991-12, Vol.18 (12), p.2245-2248 |
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creator | Egan, W. G. Hogan, A. W. Zhu, H. |
description | Analysis of the long term NOAA carbon dioxide flask sample records to examine the exchange among the continental Antarctic air mass and other air masses shows a meteorological variation of carbon dioxide concentration. There is an inverse relation between the seasonal variation of carbon dioxide concentration and water vapor at all stations examined. Well established diffusion coefficients indicate an interaction of water and carbon dioxide vapor on the molecular scale. Laboratory experiments using a Fourier transform spectrometer show carbon dioxide to be removed from an airstream in proportion to water vapor precipitated. We propose that interaction of carbon dioxide and water vapor in the atmosphere provides temporary sinks that can influence the balance of the carbon dioxide budget. |
doi_str_mv | 10.1029/91GL02770 |
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G. ; Hogan, A. W. ; Zhu, H.</creator><creatorcontrib>Egan, W. G. ; Hogan, A. W. ; Zhu, H.</creatorcontrib><description>Analysis of the long term NOAA carbon dioxide flask sample records to examine the exchange among the continental Antarctic air mass and other air masses shows a meteorological variation of carbon dioxide concentration. There is an inverse relation between the seasonal variation of carbon dioxide concentration and water vapor at all stations examined. Well established diffusion coefficients indicate an interaction of water and carbon dioxide vapor on the molecular scale. Laboratory experiments using a Fourier transform spectrometer show carbon dioxide to be removed from an airstream in proportion to water vapor precipitated. We propose that interaction of carbon dioxide and water vapor in the atmosphere provides temporary sinks that can influence the balance of the carbon dioxide budget.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/91GL02770</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Air masses ; Carbon dioxide ; Carbon dioxide concentration ; Chemical composition and interactions. 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G.</creatorcontrib><creatorcontrib>Hogan, A. W.</creatorcontrib><creatorcontrib>Zhu, H.</creatorcontrib><title>Physical variation of water vapor, and the relation with carbon dioxide</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>Analysis of the long term NOAA carbon dioxide flask sample records to examine the exchange among the continental Antarctic air mass and other air masses shows a meteorological variation of carbon dioxide concentration. There is an inverse relation between the seasonal variation of carbon dioxide concentration and water vapor at all stations examined. Well established diffusion coefficients indicate an interaction of water and carbon dioxide vapor on the molecular scale. Laboratory experiments using a Fourier transform spectrometer show carbon dioxide to be removed from an airstream in proportion to water vapor precipitated. We propose that interaction of carbon dioxide and water vapor in the atmosphere provides temporary sinks that can influence the balance of the carbon dioxide budget.</description><subject>Air masses</subject><subject>Carbon dioxide</subject><subject>Carbon dioxide concentration</subject><subject>Chemical composition and interactions. Ionic interactions and processes</subject><subject>Diffusion coefficient</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Inverse</subject><subject>Meteorology</subject><subject>Seasonal variations</subject><subject>Stations</subject><subject>Water vapor</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1991</creationdate><recordtype>article</recordtype><recordid>eNqNkU1v1DAQhi0EEkvpgX-QA0IgNe3Yjr-OtKIpYlsqBIKbNUkmWkO6WeyU7f57XKXaGx-akWY0et73MC9jLzgccxDuxPF6CcIYeMQW3FVVaQHMY7YAcHkXRj9lz1L6DgASJF-w-nq1S6HFofiFMeAUxnUx9sUWJ4r5tBnjUYHrrphWVEQaZmAbplXRYmzy3oXxLnT0nD3pcUh0-DAP2Jfzd5_PLsrlx_r92dtl2Vaai1J3Td_1yBvZGTKtxt5RBSqXUVIgz22cMQKtcVYQ6cZa0pIaEFor7OQBezX7buL485bS5G9CamkYcE3jbfJCSaW5Ev8EuRVSCZAZfP13UFdC5M-J_0CVcE5yqSCjb2a0jWNKkXq_ieEG485z8PdJ-X1SmX35YIspJ9FHXLch7QWK28pWPGPHM7YNA-3-7OfrT0tl-f0LylkQ0kR3ewHGH14baZT_elX76kJ9O_3AL_2V_A3_VqzW</recordid><startdate>199112</startdate><enddate>199112</enddate><creator>Egan, W. G.</creator><creator>Hogan, A. W.</creator><creator>Zhu, H.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>199112</creationdate><title>Physical variation of water vapor, and the relation with carbon dioxide</title><author>Egan, W. G. ; Hogan, A. W. ; Zhu, H.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4612-6dbfdfa1b3d7e7c6af9e4050507532a12a179772a87982ee6b88e63eb02665ad3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1991</creationdate><topic>Air masses</topic><topic>Carbon dioxide</topic><topic>Carbon dioxide concentration</topic><topic>Chemical composition and interactions. Ionic interactions and processes</topic><topic>Diffusion coefficient</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Inverse</topic><topic>Meteorology</topic><topic>Seasonal variations</topic><topic>Stations</topic><topic>Water vapor</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Egan, W. G.</creatorcontrib><creatorcontrib>Hogan, A. W.</creatorcontrib><creatorcontrib>Zhu, H.</creatorcontrib><collection>Istex</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>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Egan, W. G.</au><au>Hogan, A. W.</au><au>Zhu, H.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Physical variation of water vapor, and the relation with carbon dioxide</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>1991-12</date><risdate>1991</risdate><volume>18</volume><issue>12</issue><spage>2245</spage><epage>2248</epage><pages>2245-2248</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>Analysis of the long term NOAA carbon dioxide flask sample records to examine the exchange among the continental Antarctic air mass and other air masses shows a meteorological variation of carbon dioxide concentration. There is an inverse relation between the seasonal variation of carbon dioxide concentration and water vapor at all stations examined. Well established diffusion coefficients indicate an interaction of water and carbon dioxide vapor on the molecular scale. Laboratory experiments using a Fourier transform spectrometer show carbon dioxide to be removed from an airstream in proportion to water vapor precipitated. We propose that interaction of carbon dioxide and water vapor in the atmosphere provides temporary sinks that can influence the balance of the carbon dioxide budget.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/91GL02770</doi><tpages>4</tpages></addata></record> |
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issn | 0094-8276 1944-8007 |
language | eng |
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subjects | Air masses Carbon dioxide Carbon dioxide concentration Chemical composition and interactions. Ionic interactions and processes Diffusion coefficient Earth, ocean, space Exact sciences and technology External geophysics Inverse Meteorology Seasonal variations Stations Water vapor |
title | Physical variation of water vapor, and the relation with carbon dioxide |
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