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After Nuclear War: Perturbations in Atmospheric Chemistry
Long-term atmospheric effects of nuclear war could be more devastating than nuclear explosions themselves. Assuming the detonation of 25,000 warheads, 330-825 teragrams of dust and debris would be lofted into the troposphere and stratosphere. Smoke from the thousands of fires started by nuclear fire...
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Published in: | Bioscience 1985-10, Vol.35 (9), p.557-562 |
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container_end_page | 562 |
container_issue | 9 |
container_start_page | 557 |
container_title | Bioscience |
container_volume | 35 |
creator | Stephens, Sherry L. Birks, John W. |
description | Long-term atmospheric effects of nuclear war could be more devastating than nuclear explosions themselves. Assuming the detonation of 25,000 warheads, 330-825 teragrams of dust and debris would be lofted into the troposphere and stratosphere. Smoke from the thousands of fires started by nuclear fireballs would absorb sunlight and reduce atmospheric temperatures more than lofted particles would. Gaseous and particulate emissions from blasts and fires would upset the stability of the atmosphere. In the stratosphere, the protective ozone layer could be severely damaged by nitrogen oxides. |
doi_str_mv | 10.2307/1309963 |
format | article |
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Assuming the detonation of 25,000 warheads, 330-825 teragrams of dust and debris would be lofted into the troposphere and stratosphere. Smoke from the thousands of fires started by nuclear fireballs would absorb sunlight and reduce atmospheric temperatures more than lofted particles would. Gaseous and particulate emissions from blasts and fires would upset the stability of the atmosphere. In the stratosphere, the protective ozone layer could be severely damaged by nitrogen oxides.</description><subject>Asbestos</subject><subject>Blasts</subject><subject>Fireballs</subject><subject>Gases</subject><subject>Nitrogen oxides</subject><subject>Nuclear warfare</subject><subject>Ozone</subject><subject>Smoke</subject><subject>Stratosphere</subject><subject>Troposphere</subject><issn>0006-3568</issn><issn>1525-3244</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1985</creationdate><recordtype>article</recordtype><recordid>eNp10EtLxDAUBeAgCtZR_AtdiK6quUmaNO7KMD5gUBeKy5K2CdOhL2_Sxfx7K52tq8OBj3vhEHIN9J5xqh6AU60lPyERpCxNOBPilESUUpnwVGbn5ML7_VxBcB0RnbtgMX6bqtYajL8NPsYfFsOEpQnN0Pu46eM8dIMfdxabKl7vbNf4gIdLcuZM6-3VMVfk62nzuX5Jtu_Pr-t8m1RMsJA4l4qU10xSUGmZacVUKWqhhCkrYJBlDijUWmoOSirjmJRS1KDKmqsyk5KvyO1yd8ThZ7I-FPP_yrat6e0w-QIEoyAZm-HdAiscvEfrihGbzuChAFr8TVMcp5nlzSL3Pgz4L_sFODlejg</recordid><startdate>19851001</startdate><enddate>19851001</enddate><creator>Stephens, Sherry L.</creator><creator>Birks, John W.</creator><general>American Institute of Biological Sciences</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>C1K</scope><scope>SOI</scope></search><sort><creationdate>19851001</creationdate><title>After Nuclear War: Perturbations in Atmospheric Chemistry</title><author>Stephens, Sherry L. ; Birks, John W.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c242t-ff5453d260175b89727b4d474abc12188f101d96931767af26664d17bd37b8663</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1985</creationdate><topic>Asbestos</topic><topic>Blasts</topic><topic>Fireballs</topic><topic>Gases</topic><topic>Nitrogen oxides</topic><topic>Nuclear warfare</topic><topic>Ozone</topic><topic>Smoke</topic><topic>Stratosphere</topic><topic>Troposphere</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Stephens, Sherry L.</creatorcontrib><creatorcontrib>Birks, John W.</creatorcontrib><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Environment Abstracts</collection><jtitle>Bioscience</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Stephens, Sherry L.</au><au>Birks, John W.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>After Nuclear War: Perturbations in Atmospheric Chemistry</atitle><jtitle>Bioscience</jtitle><date>1985-10-01</date><risdate>1985</risdate><volume>35</volume><issue>9</issue><spage>557</spage><epage>562</epage><pages>557-562</pages><issn>0006-3568</issn><eissn>1525-3244</eissn><abstract>Long-term atmospheric effects of nuclear war could be more devastating than nuclear explosions themselves. Assuming the detonation of 25,000 warheads, 330-825 teragrams of dust and debris would be lofted into the troposphere and stratosphere. Smoke from the thousands of fires started by nuclear fireballs would absorb sunlight and reduce atmospheric temperatures more than lofted particles would. Gaseous and particulate emissions from blasts and fires would upset the stability of the atmosphere. In the stratosphere, the protective ozone layer could be severely damaged by nitrogen oxides.</abstract><pub>American Institute of Biological Sciences</pub><doi>10.2307/1309963</doi><tpages>6</tpages></addata></record> |
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identifier | ISSN: 0006-3568 |
ispartof | Bioscience, 1985-10, Vol.35 (9), p.557-562 |
issn | 0006-3568 1525-3244 |
language | eng |
recordid | cdi_proquest_miscellaneous_14201622 |
source | JSTOR Archival Journals and Primary Sources Collection |
subjects | Asbestos Blasts Fireballs Gases Nitrogen oxides Nuclear warfare Ozone Smoke Stratosphere Troposphere |
title | After Nuclear War: Perturbations in Atmospheric Chemistry |
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