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also be used in the validation of NO2 profile measurements made by satellite instruments. about 10 K warmer than those over Antarctica, pre-venting the formation of polar stratospheric clouds (PSCs), which are required for the catalytic cycles that destroy O3. In addition, the northern polar vortex...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.564.5966 2023-05-15T13:52:14+02:00 rie 1 The Pennsylvania State University CiteSeerX Archives 1999 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.5966 http://www.atmosp.physics.utoronto.ca/people/strong/papers/R23_2004_Melo_ASR.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.5966 http://www.atmosp.physics.utoronto.ca/people/strong/papers/R23_2004_Melo_ASR.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.atmosp.physics.utoronto.ca/people/strong/papers/R23_2004_Melo_ASR.pdf NO2 vertical profiles Stratospheric composition Canadian Arctic Arctic polar vertex text 1999 ftciteseerx 2016-06-19T00:01:16Z also be used in the validation of NO2 profile measurements made by satellite instruments. about 10 K warmer than those over Antarctica, pre-venting the formation of polar stratospheric clouds (PSCs), which are required for the catalytic cycles that destroy O3. In addition, the northern polar vortex is served over the Arctic. Springtime polar O3 loss is well accepted as resulting from chlorine activation on PSCs and subsequent catalytic photochemical reactions. Al-though atmospheric chlorine loading is believed to have reached its maximum or to be already declining, the cause of the recent observed decrease in stratospheric temperatures in the Arctic is still not clear. One theory is Text Antarc* Antarctica Arctic Unknown Arctic |
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English |
topic |
NO2 vertical profiles Stratospheric composition Canadian Arctic Arctic polar vertex |
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NO2 vertical profiles Stratospheric composition Canadian Arctic Arctic polar vertex rie 1 |
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NO2 vertical profiles Stratospheric composition Canadian Arctic Arctic polar vertex |
description |
also be used in the validation of NO2 profile measurements made by satellite instruments. about 10 K warmer than those over Antarctica, pre-venting the formation of polar stratospheric clouds (PSCs), which are required for the catalytic cycles that destroy O3. In addition, the northern polar vortex is served over the Arctic. Springtime polar O3 loss is well accepted as resulting from chlorine activation on PSCs and subsequent catalytic photochemical reactions. Al-though atmospheric chlorine loading is believed to have reached its maximum or to be already declining, the cause of the recent observed decrease in stratospheric temperatures in the Arctic is still not clear. One theory is |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
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title |
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title_full |
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title_fullStr |
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title_full_unstemmed |
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publishDate |
1999 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.5966 http://www.atmosp.physics.utoronto.ca/people/strong/papers/R23_2004_Melo_ASR.pdf |
geographic |
Arctic |
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Arctic |
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Antarc* Antarctica Arctic |
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Antarc* Antarctica Arctic |
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http://www.atmosp.physics.utoronto.ca/people/strong/papers/R23_2004_Melo_ASR.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.5966 http://www.atmosp.physics.utoronto.ca/people/strong/papers/R23_2004_Melo_ASR.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766256502856744960 |