Satellite constraint on the tropospheric ozone radiative effect
Tropospheric ozone directly affects the radiative balance of the Earth through interaction with shortwave and longwave radiation. Here we use measurements of tropospheric ozone from the Tropospheric Emission Spectrometer satellite instrument, together with chemical transport and radiative transfer m...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Rap, A [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Rechteinformationen: |
Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Geophysical research letters - Washington, DC : Union, 1974, 42(2015), 12, Seite 5074-5081 |
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| Übergeordnetes Werk: |
volume:42 ; year:2015 ; number:12 ; pages:5074-5081 |
| Links: |
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| DOI / URN: |
10.1002/2015GL064037 |
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OLC1964150183 |
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| 520 | |a Tropospheric ozone directly affects the radiative balance of the Earth through interaction with shortwave and longwave radiation. Here we use measurements of tropospheric ozone from the Tropospheric Emission Spectrometer satellite instrument, together with chemical transport and radiative transfer models, to produce a first estimate of the stratospherically adjusted annual radiative effect (RE) of tropospheric ozone. We show that differences between modeled and observed ozone concentrations have little impact on the RE, indicating that our present‐day tropospheric ozone RE estimate of 1.17 ± 0.03 W m −2 is robust. The RE normalized by column ozone decreased between the preindustrial and the present‐day. Using a simulation with historical biomass burning and no anthropogenic emissions, we calculate a radiative forcing of 0.32 W m −2 for tropospheric ozone, within the current best estimate range. We propose a radiative kernel approach as an efficient and accurate tool for calculating ozone REs in simulations with similar ozone abundances. First robust estimate of annual mean tropospheric ozone radiative effect (RE) The normalized RE decreased between the preindustrial and present‐day Radiative kernel approach is an efficient and accurate tool for RE calculations | ||
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| 650 | 4 | |a tropospheric ozone | |
| 650 | 4 | |a radiative forcing | |
| 650 | 4 | |a radiative kernel | |
| 650 | 4 | |a radiative effect | |
| 650 | 4 | |a Troposphere | |
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| 700 | 1 | |a Richards, N. A. D |4 oth | |
| 700 | 1 | |a Forster, P. M |4 oth | |
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| 700 | 1 | |a Arnold, S. R |4 oth | |
| 700 | 1 | |a Chipperfield, M. P |4 oth | |
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10.1002/2015GL064037 doi PQ20160617 (DE-627)OLC1964150183 (DE-599)GBVOLC1964150183 (PRQ)c2498-45a691d1beec4251b6fe4f48bc936c4a40638c35b2e6beca2d0868b1e9a36ba80 (KEY)0026932820150000042001205074satelliteconstraintonthetroposphericozoneradiative DE-627 ger DE-627 rakwb eng 550 DNB 38.70 bkl Rap, A verfasserin aut Satellite constraint on the tropospheric ozone radiative effect 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Tropospheric ozone directly affects the radiative balance of the Earth through interaction with shortwave and longwave radiation. Here we use measurements of tropospheric ozone from the Tropospheric Emission Spectrometer satellite instrument, together with chemical transport and radiative transfer models, to produce a first estimate of the stratospherically adjusted annual radiative effect (RE) of tropospheric ozone. We show that differences between modeled and observed ozone concentrations have little impact on the RE, indicating that our present‐day tropospheric ozone RE estimate of 1.17 ± 0.03 W m −2 is robust. The RE normalized by column ozone decreased between the preindustrial and the present‐day. Using a simulation with historical biomass burning and no anthropogenic emissions, we calculate a radiative forcing of 0.32 W m −2 for tropospheric ozone, within the current best estimate range. We propose a radiative kernel approach as an efficient and accurate tool for calculating ozone REs in simulations with similar ozone abundances. First robust estimate of annual mean tropospheric ozone radiative effect (RE) The normalized RE decreased between the preindustrial and present‐day Radiative kernel approach is an efficient and accurate tool for RE calculations Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. tropospheric ozone radiative forcing radiative kernel radiative effect Troposphere Ozone Richards, N. A. D oth Forster, P. M oth Monks, S. A oth Arnold, S. R oth Chipperfield, M. P oth Enthalten in Geophysical research letters Washington, DC : Union, 1974 42(2015), 12, Seite 5074-5081 (DE-627)129095109 (DE-600)7403-2 (DE-576)01443122X 0094-8276 nnns volume:42 year:2015 number:12 pages:5074-5081 http://dx.doi.org/10.1002/2015GL064037 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015GL064037/abstract http://search.proquest.com/docview/1696184378 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_47 GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2279 38.70 AVZ AR 42 2015 12 5074-5081 |
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10.1002/2015GL064037 doi PQ20160617 (DE-627)OLC1964150183 (DE-599)GBVOLC1964150183 (PRQ)c2498-45a691d1beec4251b6fe4f48bc936c4a40638c35b2e6beca2d0868b1e9a36ba80 (KEY)0026932820150000042001205074satelliteconstraintonthetroposphericozoneradiative DE-627 ger DE-627 rakwb eng 550 DNB 38.70 bkl Rap, A verfasserin aut Satellite constraint on the tropospheric ozone radiative effect 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Tropospheric ozone directly affects the radiative balance of the Earth through interaction with shortwave and longwave radiation. Here we use measurements of tropospheric ozone from the Tropospheric Emission Spectrometer satellite instrument, together with chemical transport and radiative transfer models, to produce a first estimate of the stratospherically adjusted annual radiative effect (RE) of tropospheric ozone. We show that differences between modeled and observed ozone concentrations have little impact on the RE, indicating that our present‐day tropospheric ozone RE estimate of 1.17 ± 0.03 W m −2 is robust. The RE normalized by column ozone decreased between the preindustrial and the present‐day. Using a simulation with historical biomass burning and no anthropogenic emissions, we calculate a radiative forcing of 0.32 W m −2 for tropospheric ozone, within the current best estimate range. We propose a radiative kernel approach as an efficient and accurate tool for calculating ozone REs in simulations with similar ozone abundances. First robust estimate of annual mean tropospheric ozone radiative effect (RE) The normalized RE decreased between the preindustrial and present‐day Radiative kernel approach is an efficient and accurate tool for RE calculations Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. tropospheric ozone radiative forcing radiative kernel radiative effect Troposphere Ozone Richards, N. A. D oth Forster, P. M oth Monks, S. A oth Arnold, S. R oth Chipperfield, M. P oth Enthalten in Geophysical research letters Washington, DC : Union, 1974 42(2015), 12, Seite 5074-5081 (DE-627)129095109 (DE-600)7403-2 (DE-576)01443122X 0094-8276 nnns volume:42 year:2015 number:12 pages:5074-5081 http://dx.doi.org/10.1002/2015GL064037 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015GL064037/abstract http://search.proquest.com/docview/1696184378 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_47 GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2279 38.70 AVZ AR 42 2015 12 5074-5081 |
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10.1002/2015GL064037 doi PQ20160617 (DE-627)OLC1964150183 (DE-599)GBVOLC1964150183 (PRQ)c2498-45a691d1beec4251b6fe4f48bc936c4a40638c35b2e6beca2d0868b1e9a36ba80 (KEY)0026932820150000042001205074satelliteconstraintonthetroposphericozoneradiative DE-627 ger DE-627 rakwb eng 550 DNB 38.70 bkl Rap, A verfasserin aut Satellite constraint on the tropospheric ozone radiative effect 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Tropospheric ozone directly affects the radiative balance of the Earth through interaction with shortwave and longwave radiation. Here we use measurements of tropospheric ozone from the Tropospheric Emission Spectrometer satellite instrument, together with chemical transport and radiative transfer models, to produce a first estimate of the stratospherically adjusted annual radiative effect (RE) of tropospheric ozone. We show that differences between modeled and observed ozone concentrations have little impact on the RE, indicating that our present‐day tropospheric ozone RE estimate of 1.17 ± 0.03 W m −2 is robust. The RE normalized by column ozone decreased between the preindustrial and the present‐day. Using a simulation with historical biomass burning and no anthropogenic emissions, we calculate a radiative forcing of 0.32 W m −2 for tropospheric ozone, within the current best estimate range. We propose a radiative kernel approach as an efficient and accurate tool for calculating ozone REs in simulations with similar ozone abundances. First robust estimate of annual mean tropospheric ozone radiative effect (RE) The normalized RE decreased between the preindustrial and present‐day Radiative kernel approach is an efficient and accurate tool for RE calculations Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. tropospheric ozone radiative forcing radiative kernel radiative effect Troposphere Ozone Richards, N. A. D oth Forster, P. M oth Monks, S. A oth Arnold, S. R oth Chipperfield, M. P oth Enthalten in Geophysical research letters Washington, DC : Union, 1974 42(2015), 12, Seite 5074-5081 (DE-627)129095109 (DE-600)7403-2 (DE-576)01443122X 0094-8276 nnns volume:42 year:2015 number:12 pages:5074-5081 http://dx.doi.org/10.1002/2015GL064037 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015GL064037/abstract http://search.proquest.com/docview/1696184378 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_47 GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2279 38.70 AVZ AR 42 2015 12 5074-5081 |
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Satellite constraint on the tropospheric ozone radiative effect |
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satellite constraint on the tropospheric ozone radiative effect |
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Satellite constraint on the tropospheric ozone radiative effect |
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Tropospheric ozone directly affects the radiative balance of the Earth through interaction with shortwave and longwave radiation. Here we use measurements of tropospheric ozone from the Tropospheric Emission Spectrometer satellite instrument, together with chemical transport and radiative transfer models, to produce a first estimate of the stratospherically adjusted annual radiative effect (RE) of tropospheric ozone. We show that differences between modeled and observed ozone concentrations have little impact on the RE, indicating that our present‐day tropospheric ozone RE estimate of 1.17 ± 0.03 W m −2 is robust. The RE normalized by column ozone decreased between the preindustrial and the present‐day. Using a simulation with historical biomass burning and no anthropogenic emissions, we calculate a radiative forcing of 0.32 W m −2 for tropospheric ozone, within the current best estimate range. We propose a radiative kernel approach as an efficient and accurate tool for calculating ozone REs in simulations with similar ozone abundances. First robust estimate of annual mean tropospheric ozone radiative effect (RE) The normalized RE decreased between the preindustrial and present‐day Radiative kernel approach is an efficient and accurate tool for RE calculations |
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Tropospheric ozone directly affects the radiative balance of the Earth through interaction with shortwave and longwave radiation. Here we use measurements of tropospheric ozone from the Tropospheric Emission Spectrometer satellite instrument, together with chemical transport and radiative transfer models, to produce a first estimate of the stratospherically adjusted annual radiative effect (RE) of tropospheric ozone. We show that differences between modeled and observed ozone concentrations have little impact on the RE, indicating that our present‐day tropospheric ozone RE estimate of 1.17 ± 0.03 W m −2 is robust. The RE normalized by column ozone decreased between the preindustrial and the present‐day. Using a simulation with historical biomass burning and no anthropogenic emissions, we calculate a radiative forcing of 0.32 W m −2 for tropospheric ozone, within the current best estimate range. We propose a radiative kernel approach as an efficient and accurate tool for calculating ozone REs in simulations with similar ozone abundances. First robust estimate of annual mean tropospheric ozone radiative effect (RE) The normalized RE decreased between the preindustrial and present‐day Radiative kernel approach is an efficient and accurate tool for RE calculations |
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Tropospheric ozone directly affects the radiative balance of the Earth through interaction with shortwave and longwave radiation. Here we use measurements of tropospheric ozone from the Tropospheric Emission Spectrometer satellite instrument, together with chemical transport and radiative transfer models, to produce a first estimate of the stratospherically adjusted annual radiative effect (RE) of tropospheric ozone. We show that differences between modeled and observed ozone concentrations have little impact on the RE, indicating that our present‐day tropospheric ozone RE estimate of 1.17 ± 0.03 W m −2 is robust. The RE normalized by column ozone decreased between the preindustrial and the present‐day. Using a simulation with historical biomass burning and no anthropogenic emissions, we calculate a radiative forcing of 0.32 W m −2 for tropospheric ozone, within the current best estimate range. We propose a radiative kernel approach as an efficient and accurate tool for calculating ozone REs in simulations with similar ozone abundances. First robust estimate of annual mean tropospheric ozone radiative effect (RE) The normalized RE decreased between the preindustrial and present‐day Radiative kernel approach is an efficient and accurate tool for RE calculations |
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Satellite constraint on the tropospheric ozone radiative effect |
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