The Tropospheric Chemistry of Ozone in the Polar Regions:
The Arctic troposphere (0 to ca. 8 km) plays an important role in environmental concerns for global change. It is a unique chemical reactor influenced by human activity and the Arctic ocean. It is surrounded by industrialized continents that in winter contribute gaseous and particulate pollution (Ar...
Gespeichert in:
| Weitere Verfasser: | , |
|---|---|
| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Berlin, Heidelberg
Springer Berlin Heidelberg
1993
|
| Schriftenreihe: | NATO ASI Series, Series I: Global Environmental Change
7 |
| Schlagworte: | |
| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | The Arctic troposphere (0 to ca. 8 km) plays an important role in environmental concerns for global change. It is a unique chemical reactor influenced by human activity and the Arctic ocean. It is surrounded by industrialized continents that in winter contribute gaseous and particulate pollution (Arctic haze). It is underlain by the flat Arctic ocean from which it is separated by a crack-ridden ice membrane 3 to 4 m thick. Ocean to atmosphere exchange of heat, water vapor and marine biogenic gases influence the composition of the reactor. From September 21 to December 21 to March 21, the region north of the Arctic circle goes from a completely sunlit situation to a completely dark one and then back to light. At the same time the lower troposphere is stably stratified. This hinders vertical mixing. During this light period, surface temperature reaches as low as -40C. In this environment, chemical reactions involving sunlight are generally much slower than further south. Thus, the abundance of photochemically reactive compounds in the atmosphere can be high prior to polar sunrise. Between complete dark in February and complete light in April, a number of chemical changes in the lower troposphere take place |
| Beschreibung: | 1 Online-Ressource (VII, 425 p) |
| ISBN: | 9783642782114 |
| DOI: | 10.1007/978-3-642-78211-4 |
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| 245 | 1 | 0 | |a The Tropospheric Chemistry of Ozone in the Polar Regions |c edited by H. Niki, K. H. Becker |
| 246 | 1 | 3 | |a Proceedings of the NATO Advanced Research Workshop on The Tropospheric Chemistry of Ozone in the Polar Regions held at Wolfville, Nova Scotia, Canada, August 23-28, 1992 |
| 264 | 1 | |a Berlin, Heidelberg |b Springer Berlin Heidelberg |c 1993 | |
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| 490 | 0 | |a NATO ASI Series, Series I: Global Environmental Change |v 7 | |
| 520 | |a The Arctic troposphere (0 to ca. 8 km) plays an important role in environmental concerns for global change. It is a unique chemical reactor influenced by human activity and the Arctic ocean. It is surrounded by industrialized continents that in winter contribute gaseous and particulate pollution (Arctic haze). It is underlain by the flat Arctic ocean from which it is separated by a crack-ridden ice membrane 3 to 4 m thick. Ocean to atmosphere exchange of heat, water vapor and marine biogenic gases influence the composition of the reactor. From September 21 to December 21 to March 21, the region north of the Arctic circle goes from a completely sunlit situation to a completely dark one and then back to light. At the same time the lower troposphere is stably stratified. This hinders vertical mixing. During this light period, surface temperature reaches as low as -40C. In this environment, chemical reactions involving sunlight are generally much slower than further south. Thus, the abundance of photochemically reactive compounds in the atmosphere can be high prior to polar sunrise. Between complete dark in February and complete light in April, a number of chemical changes in the lower troposphere take place | ||
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Datensatz im Suchindex
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| author2 | Niki, H. Becker, K. H. |
| author2_role | edt edt |
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| author_facet | Niki, H. Becker, K. H. |
| building | Verbundindex |
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| collection | ZDB-2-EES |
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| dewey-full | 363.7392 |
| dewey-hundreds | 300 - Social sciences |
| dewey-ones | 363 - Other social problems and services |
| dewey-raw | 363.7392 |
| dewey-search | 363.7392 |
| dewey-sort | 3363.7392 |
| dewey-tens | 360 - Social problems and services; associations |
| discipline | Soziologie |
| doi_str_mv | 10.1007/978-3-642-78211-4 |
| format | Electronic eBook |
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| id | DE-604.BV045178931 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:50Z |
| institution | BVB |
| isbn | 9783642782114 |
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| publishDate | 1993 |
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| spelling | The Tropospheric Chemistry of Ozone in the Polar Regions edited by H. Niki, K. H. Becker Proceedings of the NATO Advanced Research Workshop on The Tropospheric Chemistry of Ozone in the Polar Regions held at Wolfville, Nova Scotia, Canada, August 23-28, 1992 Berlin, Heidelberg Springer Berlin Heidelberg 1993 1 Online-Ressource (VII, 425 p) txt rdacontent c rdamedia cr rdacarrier NATO ASI Series, Series I: Global Environmental Change 7 The Arctic troposphere (0 to ca. 8 km) plays an important role in environmental concerns for global change. It is a unique chemical reactor influenced by human activity and the Arctic ocean. It is surrounded by industrialized continents that in winter contribute gaseous and particulate pollution (Arctic haze). It is underlain by the flat Arctic ocean from which it is separated by a crack-ridden ice membrane 3 to 4 m thick. Ocean to atmosphere exchange of heat, water vapor and marine biogenic gases influence the composition of the reactor. From September 21 to December 21 to March 21, the region north of the Arctic circle goes from a completely sunlit situation to a completely dark one and then back to light. At the same time the lower troposphere is stably stratified. This hinders vertical mixing. During this light period, surface temperature reaches as low as -40C. In this environment, chemical reactions involving sunlight are generally much slower than further south. Thus, the abundance of photochemically reactive compounds in the atmosphere can be high prior to polar sunrise. Between complete dark in February and complete light in April, a number of chemical changes in the lower troposphere take place Environment Atmospheric Protection/Air Quality Control/Air Pollution Atmospheric Sciences Geography, general Ecology Atmospheric sciences Geography Air pollution Troposphäre (DE-588)4061018-4 gnd rswk-swf Ozon (DE-588)4173038-0 gnd rswk-swf Polargebiete (DE-588)4076200-2 gnd rswk-swf 1\p (DE-588)1071861417 Konferenzschrift 1992 Wolfville gnd-content Polargebiete (DE-588)4076200-2 g Troposphäre (DE-588)4061018-4 s Ozon (DE-588)4173038-0 s 2\p DE-604 Niki, H. edt Becker, K. H. edt Erscheint auch als Druck-Ausgabe 9783642782138 https://doi.org/10.1007/978-3-642-78211-4 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 2\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | The Tropospheric Chemistry of Ozone in the Polar Regions Environment Atmospheric Protection/Air Quality Control/Air Pollution Atmospheric Sciences Geography, general Ecology Atmospheric sciences Geography Air pollution Troposphäre (DE-588)4061018-4 gnd Ozon (DE-588)4173038-0 gnd |
| subject_GND | (DE-588)4061018-4 (DE-588)4173038-0 (DE-588)4076200-2 (DE-588)1071861417 |
| title | The Tropospheric Chemistry of Ozone in the Polar Regions |
| title_alt | Proceedings of the NATO Advanced Research Workshop on The Tropospheric Chemistry of Ozone in the Polar Regions held at Wolfville, Nova Scotia, Canada, August 23-28, 1992 |
| title_auth | The Tropospheric Chemistry of Ozone in the Polar Regions |
| title_exact_search | The Tropospheric Chemistry of Ozone in the Polar Regions |
| title_full | The Tropospheric Chemistry of Ozone in the Polar Regions edited by H. Niki, K. H. Becker |
| title_fullStr | The Tropospheric Chemistry of Ozone in the Polar Regions edited by H. Niki, K. H. Becker |
| title_full_unstemmed | The Tropospheric Chemistry of Ozone in the Polar Regions edited by H. Niki, K. H. Becker |
| title_short | The Tropospheric Chemistry of Ozone in the Polar Regions |
| title_sort | the tropospheric chemistry of ozone in the polar regions |
| topic | Environment Atmospheric Protection/Air Quality Control/Air Pollution Atmospheric Sciences Geography, general Ecology Atmospheric sciences Geography Air pollution Troposphäre (DE-588)4061018-4 gnd Ozon (DE-588)4173038-0 gnd |
| topic_facet | Environment Atmospheric Protection/Air Quality Control/Air Pollution Atmospheric Sciences Geography, general Ecology Atmospheric sciences Geography Air pollution Troposphäre Ozon Polargebiete Konferenzschrift 1992 Wolfville |
| url | https://doi.org/10.1007/978-3-642-78211-4 |
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