Comparison of stratospheric warmings following Agung and Chichon
Temperatures at 50, 30, 20, and 10 mb in the western quadrant of the Northern Hemisphere are used to estimate the stratospheric warming resulting from the volcanic eruptions of Agung in 1963 and El Chichon in 1982. After allowing for quasi-biennial temperature variations, a warming of similar to 4 d...
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Veröffentlicht in: | Monthly weather review 1983-10, Vol.111 (10), p.2129-2135 |
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creator | ANGELL, J. K KORSHOVER, J |
description | Temperatures at 50, 30, 20, and 10 mb in the western quadrant of the Northern Hemisphere are used to estimate the stratospheric warming resulting from the volcanic eruptions of Agung in 1963 and El Chichon in 1982. After allowing for quasi-biennial temperature variations, a warming of similar to 4 degrees C is found at 50 mb in the equatorial zone after the eruption of Agung and at 30 mb in the northern subtropics after the eruption of Chichon. In both cases, the warming was at a maximum two seasons after the eruption. The Chichon-induced warming in the American sector of the northern subtropics is indicated to be slightly greater than in the Pacific sector. |
doi_str_mv | 10.1175/1520-0493(1983)111<2129:coswfa>2.0.co;2 |
format | Article |
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The Chichon-induced warming in the American sector of the northern subtropics is indicated to be slightly greater than in the Pacific sector.</description><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>General properties of the high atmosphere</subject><subject>Physics of the high neutral atmosphere</subject><issn>0027-0644</issn><issn>1520-0493</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1983</creationdate><recordtype>article</recordtype><recordid>eNqFkE1LAzEQhoMoWKv_YQ8ietg2k6_dqIhlsVUo9KDiMaRp0q5sNzXZUvz37tLSq5eZl-HhHXgQGgIeAGR8CJzgFDNJb0Hm9A4AHgkQeW983Dn9RAZ4YPwDOUG9I3mKehiTLMWCsXN0EeM3xlgIRnroufDrjQ5l9HXiXRKboBsfNysbSpPsdFiX9TImzleV37UxGS237dT1IilWpVn5-hKdOV1Fe3XYffQ5fvkoXtPpbPJWjKapYVQ2KZNzyjOtWS6zOdVcS06ctEYSbinFXOKcGcGEEdy6Re6IkKBhjjMr3cJlgvbRzb53E_zP1sZGrctobFXp2vptVIQC4Zxm_4KQUw6AeQtO9qAJPsZgndqEcq3DrwKsOtWqE6g6gapT3d5AdapVMXv_Go8UUbiN7ec-uj681NHoygVdmzIe6ySjlElB_wA_LoI3</recordid><startdate>19831001</startdate><enddate>19831001</enddate><creator>ANGELL, J. 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K ; KORSHOVER, J</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c439t-49b357aa4897b3a5a952f9ec925e33059084c646c65efd8f2691a1b07e9fdf763</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1983</creationdate><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>General properties of the high atmosphere</topic><topic>Physics of the high neutral atmosphere</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>ANGELL, J. K</creatorcontrib><creatorcontrib>KORSHOVER, J</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>Monthly weather review</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>ANGELL, J. K</au><au>KORSHOVER, J</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Comparison of stratospheric warmings following Agung and Chichon</atitle><jtitle>Monthly weather review</jtitle><date>1983-10-01</date><risdate>1983</risdate><volume>111</volume><issue>10</issue><spage>2129</spage><epage>2135</epage><pages>2129-2135</pages><issn>0027-0644</issn><eissn>1520-0493</eissn><coden>MWREAB</coden><abstract>Temperatures at 50, 30, 20, and 10 mb in the western quadrant of the Northern Hemisphere are used to estimate the stratospheric warming resulting from the volcanic eruptions of Agung in 1963 and El Chichon in 1982. After allowing for quasi-biennial temperature variations, a warming of similar to 4 degrees C is found at 50 mb in the equatorial zone after the eruption of Agung and at 30 mb in the northern subtropics after the eruption of Chichon. In both cases, the warming was at a maximum two seasons after the eruption. The Chichon-induced warming in the American sector of the northern subtropics is indicated to be slightly greater than in the Pacific sector.</abstract><cop>Boston, MA</cop><pub>American Meteorological Society</pub><doi>10.1175/1520-0493(1983)111<2129:coswfa>2.0.co;2</doi><tpages>7</tpages><oa>free_for_read</oa></addata></record> |
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source | American Meteorological Society; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Alma/SFX Local Collection |
subjects | Earth, ocean, space Exact sciences and technology External geophysics General properties of the high atmosphere Physics of the high neutral atmosphere |
title | Comparison of stratospheric warmings following Agung and Chichon |
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