Application of general circulation models to the study of stratospheric ozone
Summary Observations of the ozone distribution indicate that modifications are required to the photochemical theory. These modifications involve ozone destruction by hydrogen and nitrogen products and ozone transport (both vertical and horizontal) due to atmospheric motions in the stratosphere. If t...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
London, Julius [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1973 |
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| Schlagwörter: |
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| Anmerkung: |
© Birkhäuser Verlag 1973 |
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| Übergeordnetes Werk: |
Enthalten in: Pure and applied geophysics - Birkhäuser-Verlag, 1964, 106-108(1973), 1 vom: 01. Dez., Seite 1611-1617 |
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| Übergeordnetes Werk: |
volume:106-108 ; year:1973 ; number:1 ; day:01 ; month:12 ; pages:1611-1617 |
| Links: |
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| DOI / URN: |
10.1007/BF00881110 |
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| Katalog-ID: |
OLC2069454681 |
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| 520 | |a Summary Observations of the ozone distribution indicate that modifications are required to the photochemical theory. These modifications involve ozone destruction by hydrogen and nitrogen products and ozone transport (both vertical and horizontal) due to atmospheric motions in the stratosphere. If the photochemical terms in the ozone continuity equation are omitted, changes due to atmospheric transport alone can be evaluated. Numerical computations were made of the three-dimensional wind structure as derived from the 12-layer (0–36 km) General Circulation Model developed by NCAR. The results showed that ozone is transported from the equatorial stratosphere poleward and downward in both hemispheres. The horizontal transport is primarily by the Hadley Cell in the tropics and by large-scale eddies in mid and high latitudes. The dominant mechanism for ozone transport are found to be similar to those derived for the horizontal heat and momentum transport found in other general circulation studies. | ||
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| 650 | 4 | |a General Circulation Model | |
| 650 | 4 | |a Stratospheric Ozone | |
| 650 | 4 | |a Hadley Cell | |
| 650 | 4 | |a Eddy Flux | |
| 700 | 1 | |a Park, Jae |4 aut | |
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10.1007/BF00881110 doi (DE-627)OLC2069454681 (DE-He213)BF00881110-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn London, Julius verfasserin aut Application of general circulation models to the study of stratospheric ozone 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser Verlag 1973 Summary Observations of the ozone distribution indicate that modifications are required to the photochemical theory. These modifications involve ozone destruction by hydrogen and nitrogen products and ozone transport (both vertical and horizontal) due to atmospheric motions in the stratosphere. If the photochemical terms in the ozone continuity equation are omitted, changes due to atmospheric transport alone can be evaluated. Numerical computations were made of the three-dimensional wind structure as derived from the 12-layer (0–36 km) General Circulation Model developed by NCAR. The results showed that ozone is transported from the equatorial stratosphere poleward and downward in both hemispheres. The horizontal transport is primarily by the Hadley Cell in the tropics and by large-scale eddies in mid and high latitudes. The dominant mechanism for ozone transport are found to be similar to those derived for the horizontal heat and momentum transport found in other general circulation studies. Ozone General Circulation Model Stratospheric Ozone Hadley Cell Eddy Flux Park, Jae aut Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 106-108(1973), 1 vom: 01. Dez., Seite 1611-1617 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:106-108 year:1973 number:1 day:01 month:12 pages:1611-1617 https://doi.org/10.1007/BF00881110 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 106-108 1973 1 01 12 1611-1617 |
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10.1007/BF00881110 doi (DE-627)OLC2069454681 (DE-He213)BF00881110-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn London, Julius verfasserin aut Application of general circulation models to the study of stratospheric ozone 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser Verlag 1973 Summary Observations of the ozone distribution indicate that modifications are required to the photochemical theory. These modifications involve ozone destruction by hydrogen and nitrogen products and ozone transport (both vertical and horizontal) due to atmospheric motions in the stratosphere. If the photochemical terms in the ozone continuity equation are omitted, changes due to atmospheric transport alone can be evaluated. Numerical computations were made of the three-dimensional wind structure as derived from the 12-layer (0–36 km) General Circulation Model developed by NCAR. The results showed that ozone is transported from the equatorial stratosphere poleward and downward in both hemispheres. The horizontal transport is primarily by the Hadley Cell in the tropics and by large-scale eddies in mid and high latitudes. The dominant mechanism for ozone transport are found to be similar to those derived for the horizontal heat and momentum transport found in other general circulation studies. Ozone General Circulation Model Stratospheric Ozone Hadley Cell Eddy Flux Park, Jae aut Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 106-108(1973), 1 vom: 01. Dez., Seite 1611-1617 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:106-108 year:1973 number:1 day:01 month:12 pages:1611-1617 https://doi.org/10.1007/BF00881110 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 106-108 1973 1 01 12 1611-1617 |
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10.1007/BF00881110 doi (DE-627)OLC2069454681 (DE-He213)BF00881110-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn London, Julius verfasserin aut Application of general circulation models to the study of stratospheric ozone 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser Verlag 1973 Summary Observations of the ozone distribution indicate that modifications are required to the photochemical theory. These modifications involve ozone destruction by hydrogen and nitrogen products and ozone transport (both vertical and horizontal) due to atmospheric motions in the stratosphere. If the photochemical terms in the ozone continuity equation are omitted, changes due to atmospheric transport alone can be evaluated. Numerical computations were made of the three-dimensional wind structure as derived from the 12-layer (0–36 km) General Circulation Model developed by NCAR. The results showed that ozone is transported from the equatorial stratosphere poleward and downward in both hemispheres. The horizontal transport is primarily by the Hadley Cell in the tropics and by large-scale eddies in mid and high latitudes. The dominant mechanism for ozone transport are found to be similar to those derived for the horizontal heat and momentum transport found in other general circulation studies. Ozone General Circulation Model Stratospheric Ozone Hadley Cell Eddy Flux Park, Jae aut Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 106-108(1973), 1 vom: 01. Dez., Seite 1611-1617 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:106-108 year:1973 number:1 day:01 month:12 pages:1611-1617 https://doi.org/10.1007/BF00881110 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 106-108 1973 1 01 12 1611-1617 |
| allfieldsGer |
10.1007/BF00881110 doi (DE-627)OLC2069454681 (DE-He213)BF00881110-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn London, Julius verfasserin aut Application of general circulation models to the study of stratospheric ozone 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser Verlag 1973 Summary Observations of the ozone distribution indicate that modifications are required to the photochemical theory. These modifications involve ozone destruction by hydrogen and nitrogen products and ozone transport (both vertical and horizontal) due to atmospheric motions in the stratosphere. If the photochemical terms in the ozone continuity equation are omitted, changes due to atmospheric transport alone can be evaluated. Numerical computations were made of the three-dimensional wind structure as derived from the 12-layer (0–36 km) General Circulation Model developed by NCAR. The results showed that ozone is transported from the equatorial stratosphere poleward and downward in both hemispheres. The horizontal transport is primarily by the Hadley Cell in the tropics and by large-scale eddies in mid and high latitudes. The dominant mechanism for ozone transport are found to be similar to those derived for the horizontal heat and momentum transport found in other general circulation studies. Ozone General Circulation Model Stratospheric Ozone Hadley Cell Eddy Flux Park, Jae aut Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 106-108(1973), 1 vom: 01. Dez., Seite 1611-1617 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:106-108 year:1973 number:1 day:01 month:12 pages:1611-1617 https://doi.org/10.1007/BF00881110 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 106-108 1973 1 01 12 1611-1617 |
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10.1007/BF00881110 doi (DE-627)OLC2069454681 (DE-He213)BF00881110-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn London, Julius verfasserin aut Application of general circulation models to the study of stratospheric ozone 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser Verlag 1973 Summary Observations of the ozone distribution indicate that modifications are required to the photochemical theory. These modifications involve ozone destruction by hydrogen and nitrogen products and ozone transport (both vertical and horizontal) due to atmospheric motions in the stratosphere. If the photochemical terms in the ozone continuity equation are omitted, changes due to atmospheric transport alone can be evaluated. Numerical computations were made of the three-dimensional wind structure as derived from the 12-layer (0–36 km) General Circulation Model developed by NCAR. The results showed that ozone is transported from the equatorial stratosphere poleward and downward in both hemispheres. The horizontal transport is primarily by the Hadley Cell in the tropics and by large-scale eddies in mid and high latitudes. The dominant mechanism for ozone transport are found to be similar to those derived for the horizontal heat and momentum transport found in other general circulation studies. Ozone General Circulation Model Stratospheric Ozone Hadley Cell Eddy Flux Park, Jae aut Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 106-108(1973), 1 vom: 01. Dez., Seite 1611-1617 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:106-108 year:1973 number:1 day:01 month:12 pages:1611-1617 https://doi.org/10.1007/BF00881110 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 106-108 1973 1 01 12 1611-1617 |
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Enthalten in Pure and applied geophysics 106-108(1973), 1 vom: 01. Dez., Seite 1611-1617 volume:106-108 year:1973 number:1 day:01 month:12 pages:1611-1617 |
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Enthalten in Pure and applied geophysics 106-108(1973), 1 vom: 01. Dez., Seite 1611-1617 volume:106-108 year:1973 number:1 day:01 month:12 pages:1611-1617 |
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application of general circulation models to the study of stratospheric ozone |
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Application of general circulation models to the study of stratospheric ozone |
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Summary Observations of the ozone distribution indicate that modifications are required to the photochemical theory. These modifications involve ozone destruction by hydrogen and nitrogen products and ozone transport (both vertical and horizontal) due to atmospheric motions in the stratosphere. If the photochemical terms in the ozone continuity equation are omitted, changes due to atmospheric transport alone can be evaluated. Numerical computations were made of the three-dimensional wind structure as derived from the 12-layer (0–36 km) General Circulation Model developed by NCAR. The results showed that ozone is transported from the equatorial stratosphere poleward and downward in both hemispheres. The horizontal transport is primarily by the Hadley Cell in the tropics and by large-scale eddies in mid and high latitudes. The dominant mechanism for ozone transport are found to be similar to those derived for the horizontal heat and momentum transport found in other general circulation studies. © Birkhäuser Verlag 1973 |
| abstractGer |
Summary Observations of the ozone distribution indicate that modifications are required to the photochemical theory. These modifications involve ozone destruction by hydrogen and nitrogen products and ozone transport (both vertical and horizontal) due to atmospheric motions in the stratosphere. If the photochemical terms in the ozone continuity equation are omitted, changes due to atmospheric transport alone can be evaluated. Numerical computations were made of the three-dimensional wind structure as derived from the 12-layer (0–36 km) General Circulation Model developed by NCAR. The results showed that ozone is transported from the equatorial stratosphere poleward and downward in both hemispheres. The horizontal transport is primarily by the Hadley Cell in the tropics and by large-scale eddies in mid and high latitudes. The dominant mechanism for ozone transport are found to be similar to those derived for the horizontal heat and momentum transport found in other general circulation studies. © Birkhäuser Verlag 1973 |
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Summary Observations of the ozone distribution indicate that modifications are required to the photochemical theory. These modifications involve ozone destruction by hydrogen and nitrogen products and ozone transport (both vertical and horizontal) due to atmospheric motions in the stratosphere. If the photochemical terms in the ozone continuity equation are omitted, changes due to atmospheric transport alone can be evaluated. Numerical computations were made of the three-dimensional wind structure as derived from the 12-layer (0–36 km) General Circulation Model developed by NCAR. The results showed that ozone is transported from the equatorial stratosphere poleward and downward in both hemispheres. The horizontal transport is primarily by the Hadley Cell in the tropics and by large-scale eddies in mid and high latitudes. The dominant mechanism for ozone transport are found to be similar to those derived for the horizontal heat and momentum transport found in other general circulation studies. © Birkhäuser Verlag 1973 |
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