Interhemispheric Differences in Dentifrication and Related Processes Affecting Polar Ozone
The severe depletion of stratospheric ozone over Antarctica in late winter and early spring is caused by enhanced CLO abundances arising from heterogeneous reactions on polar stratospheric clouds (PSCs). CLO abundances comparable to those over Antarctica have also been observed throughout the Arctic...
| Main Authors: | , , , , , , , , |
|---|---|
| Language: | English |
| Published: |
2004
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/2014/33820 |
| _version_ | 1821549035880710144 |
|---|---|
| author | Santee, M. L. Read, W. G. Waters, J. W. Froidevaux, L. Manney, G. L. Flower, D. A. Jarnot, R. F. Harwood, R. S. Peckham, G. E. |
| author_facet | Santee, M. L. Read, W. G. Waters, J. W. Froidevaux, L. Manney, G. L. Flower, D. A. Jarnot, R. F. Harwood, R. S. Peckham, G. E. |
| author_sort | Santee, M. L. |
| collection | JPL Technical Report Server |
| description | The severe depletion of stratospheric ozone over Antarctica in late winter and early spring is caused by enhanced CLO abundances arising from heterogeneous reactions on polar stratospheric clouds (PSCs). CLO abundances comparable to those over Antarctica have also been observed throughout the Arctic Vortex, but the accompanying loss of Arctic ozone has been much less severe. |
| genre | Antarc* Antarctica Arctic |
| genre_facet | Antarc* Antarctica Arctic |
| geographic | Arctic |
| geographic_facet | Arctic |
| id | ftnasajpl:oai:trs.jpl.nasa.gov:2014/33820 |
| institution | Open Polar |
| language | English |
| op_collection_id | ftnasajpl |
| op_relation | 94-0551 http://hdl.handle.net/2014/33820 |
| publishDate | 2004 |
| record_format | openpolar |
| spelling | ftnasajpl:oai:trs.jpl.nasa.gov:2014/33820 2025-01-16T19:04:26+00:00 Interhemispheric Differences in Dentifrication and Related Processes Affecting Polar Ozone Santee, M. L. Read, W. G. Waters, J. W. Froidevaux, L. Manney, G. L. Flower, D. A. Jarnot, R. F. Harwood, R. S. Peckham, G. E. 2004-10-05T21:47:32Z 1019349 bytes application/pdf http://hdl.handle.net/2014/33820 en_US eng 94-0551 http://hdl.handle.net/2014/33820 ozone depletion 2004 ftnasajpl 2021-12-23T13:19:34Z The severe depletion of stratospheric ozone over Antarctica in late winter and early spring is caused by enhanced CLO abundances arising from heterogeneous reactions on polar stratospheric clouds (PSCs). CLO abundances comparable to those over Antarctica have also been observed throughout the Arctic Vortex, but the accompanying loss of Arctic ozone has been much less severe. Other/Unknown Material Antarc* Antarctica Arctic JPL Technical Report Server Arctic |
| spellingShingle | ozone depletion Santee, M. L. Read, W. G. Waters, J. W. Froidevaux, L. Manney, G. L. Flower, D. A. Jarnot, R. F. Harwood, R. S. Peckham, G. E. Interhemispheric Differences in Dentifrication and Related Processes Affecting Polar Ozone |
| title | Interhemispheric Differences in Dentifrication and Related Processes Affecting Polar Ozone |
| title_full | Interhemispheric Differences in Dentifrication and Related Processes Affecting Polar Ozone |
| title_fullStr | Interhemispheric Differences in Dentifrication and Related Processes Affecting Polar Ozone |
| title_full_unstemmed | Interhemispheric Differences in Dentifrication and Related Processes Affecting Polar Ozone |
| title_short | Interhemispheric Differences in Dentifrication and Related Processes Affecting Polar Ozone |
| title_sort | interhemispheric differences in dentifrication and related processes affecting polar ozone |
| topic | ozone depletion |
| topic_facet | ozone depletion |
| url | http://hdl.handle.net/2014/33820 |