000 | 01579 a2200289 4500 | ||
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008 | 040419s xx 000 0 eng | ||
022 | _a1522-3264; | ||
050 | _aAC1.S5 | ||
082 | _a050 | ||
100 | _aAllen, Jeannie, | ||
245 | 0 |
_aWatching Our Ozone Weather. _cJeannie Allen. |
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260 |
_bEarth Observatory, _c2003. |
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440 |
_aSIRS Enduring Issues 2004. _nArticle 17, _pScience, _x1522-3264; |
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500 | _aArticles Contained in SIRS Enduring Issues 2004. | ||
500 | _aOriginally Published: Watching Our Ozone Weather, Aug. 22, 2003; pp. n.p.. | ||
520 | _a"Until about 30 years ago, atmospheric scientists believed that all of the ozone in the lower atmosphere (troposphere) intruded from the upper atmosphere (stratosphere), where it formed by the action of sunlight on oxygen molecules. The work of atmospheric chemists during the 1970s dramatically altered that view. Now we understand that more than half of the ozone in the troposphere comes from chemical interactions within the troposphere itself." (EARTH OBSERVATORY) This article discusses the formation of ozone and examines what needs to be done to lessen ozone pollution. | ||
599 | _aRecords created from non-MARC resource. | ||
650 | _aAir pollution | ||
650 |
_aAir quality _xStandards |
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650 | _aArtificial satellites in earth sciences | ||
650 | _aOzone | ||
650 |
_aOzone _xMeasurement |
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650 |
_aOzone _xPhysiological effect |
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650 | _aTroposphere | ||
710 |
_aProQuest Information and Learning Company _tSIRS Enduring Issues 2004, _pScience. _x1522-3264; |
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942 | _c UKN | ||
999 |
_c35866 _d35866 |