Tropospheric Ozone Assessment Report: Present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation
'The Tropospheric Ozone Assessment Report' (TOAR) is an activity of the International Global Atmospheric Chemistry Project. This paper is a component of the report, focusing on the present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistr...
Ausführliche Beschreibung
Autor*in: |
A. Gaudel [verfasserIn] O. R. Cooper [verfasserIn] G. Ancellet [verfasserIn] B. Barret [verfasserIn] A. Boynard [verfasserIn] J. P. Burrows [verfasserIn] C. Clerbaux [verfasserIn] P. -F. Coheur [verfasserIn] J. Cuesta [verfasserIn] E. Cuevas [verfasserIn] S. Doniki [verfasserIn] G. Dufour [verfasserIn] F. Ebojie [verfasserIn] G. Foret [verfasserIn] O. Garcia [verfasserIn] M. J. Granados Muños [verfasserIn] J. W. Hannigan [verfasserIn] F. Hase [verfasserIn] G. Huang [verfasserIn] B. Hassler [verfasserIn] D. Hurtmans [verfasserIn] D. Jaffe [verfasserIn] N. Jones [verfasserIn] P. Kalabokas [verfasserIn] B. Kerridge [verfasserIn] S. S. Kulawik [verfasserIn] B. Latter [verfasserIn] T. Leblanc [verfasserIn] E. Le Flochmoën [verfasserIn] W. Lin [verfasserIn] J. Liu [verfasserIn] X. Liu [verfasserIn] E. Mahieu [verfasserIn] A. McClure-Begley [verfasserIn] J. L. Neu [verfasserIn] M. Osman [verfasserIn] M. Palm [verfasserIn] H. Petetin [verfasserIn] I. Petropavlovskikh [verfasserIn] R. Querel [verfasserIn] N. Rahpoe [verfasserIn] A. Rozanov [verfasserIn] M. G. Schultz [verfasserIn] J. Schwab [verfasserIn] R. Siddans [verfasserIn] D. Smale [verfasserIn] M. Steinbacher [verfasserIn] H. Tanimoto [verfasserIn] D. W. Tarasick [verfasserIn] V. Thouret [verfasserIn] A. M. Thompson [verfasserIn] T. Trickl [verfasserIn] E. Weatherhead [verfasserIn] C. Wespes [verfasserIn] H. M. Worden [verfasserIn] C. Vigouroux [verfasserIn] X. Xu [verfasserIn] G. Zeng [verfasserIn] J. Ziemke [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2018 |
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Schlagwörter: |
Tropospheric composition and chemistry |
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Übergeordnetes Werk: |
In: Elementa: Science of the Anthropocene - BioOne, 2014, 6(2018), 1 |
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Übergeordnetes Werk: |
volume:6 ; year:2018 ; number:1 |
Links: |
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DOI / URN: |
10.1525/elementa.291 |
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Katalog-ID: |
DOAJ001616234 |
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520 | |a 'The Tropospheric Ozone Assessment Report' (TOAR) is an activity of the International Global Atmospheric Chemistry Project. This paper is a component of the report, focusing on the present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation. Utilizing the TOAR surface ozone database, several figures present the global distribution and trends of daytime average ozone at 2702 non-urban monitoring sites, highlighting the regions and seasons of the world with the greatest ozone levels. Similarly, ozonesonde and commercial aircraft observations reveal ozone’s distribution throughout the depth of the free troposphere. Long-term surface observations are limited in their global spatial coverage, but data from remote locations indicate that ozone in the 21st century is greater than during the 1970s and 1980s. While some remote sites and many sites in the heavily polluted regions of East Asia show ozone increases since 2000, many others show decreases and there is no clear global pattern for surface ozone changes since 2000. Two new satellite products provide detailed views of ozone in the lower troposphere across East Asia and Europe, revealing the full spatial extent of the spring and summer ozone enhancements across eastern China that cannot be assessed from limited surface observations. Sufficient data are now available (ozonesondes, satellite, aircraft) across the tropics from South America eastwards to the western Pacific Ocean, to indicate a likely tropospheric column ozone increase since the 1990s. The 2014–2016 mean tropospheric ozone burden (TOB) between 60°N–60°S from five satellite products is 300 Tg ± 4%. While this agreement is excellent, the products differ in their quantification of TOB trends and further work is required to reconcile the differences. Satellites can now estimate ozone’s global long-wave radiative effect, but evaluation is difficult due to limited in situ observations where the radiative effect is greatest. | ||
650 | 4 | |a tropospheric ozone | |
650 | 4 | |a ground-level ozone | |
650 | 4 | |a Tropospheric composition and chemistry | |
650 | 4 | |a Global tropospheric ozone burden | |
650 | 4 | |a Ozone trends | |
653 | 0 | |a Environmental sciences | |
700 | 0 | |a O. R. Cooper |e verfasserin |4 aut | |
700 | 0 | |a G. Ancellet |e verfasserin |4 aut | |
700 | 0 | |a B. Barret |e verfasserin |4 aut | |
700 | 0 | |a A. Boynard |e verfasserin |4 aut | |
700 | 0 | |a J. P. Burrows |e verfasserin |4 aut | |
700 | 0 | |a C. Clerbaux |e verfasserin |4 aut | |
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700 | 0 | |a J. Cuesta |e verfasserin |4 aut | |
700 | 0 | |a E. Cuevas |e verfasserin |4 aut | |
700 | 0 | |a S. Doniki |e verfasserin |4 aut | |
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700 | 0 | |a J. W. Hannigan |e verfasserin |4 aut | |
700 | 0 | |a F. Hase |e verfasserin |4 aut | |
700 | 0 | |a G. Huang |e verfasserin |4 aut | |
700 | 0 | |a B. Hassler |e verfasserin |4 aut | |
700 | 0 | |a D. Hurtmans |e verfasserin |4 aut | |
700 | 0 | |a D. Jaffe |e verfasserin |4 aut | |
700 | 0 | |a N. Jones |e verfasserin |4 aut | |
700 | 0 | |a P. Kalabokas |e verfasserin |4 aut | |
700 | 0 | |a B. Kerridge |e verfasserin |4 aut | |
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700 | 0 | |a J. Liu |e verfasserin |4 aut | |
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700 | 0 | |a J. L. Neu |e verfasserin |4 aut | |
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700 | 0 | |a R. Siddans |e verfasserin |4 aut | |
700 | 0 | |a D. Smale |e verfasserin |4 aut | |
700 | 0 | |a M. Steinbacher |e verfasserin |4 aut | |
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700 | 0 | |a D. W. Tarasick |e verfasserin |4 aut | |
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700 | 0 | |a A. M. Thompson |e verfasserin |4 aut | |
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700 | 0 | |a C. Vigouroux |e verfasserin |4 aut | |
700 | 0 | |a X. Xu |e verfasserin |4 aut | |
700 | 0 | |a G. Zeng |e verfasserin |4 aut | |
700 | 0 | |a J. Ziemke |e verfasserin |4 aut | |
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10.1525/elementa.291 doi (DE-627)DOAJ001616234 (DE-599)DOAJa63a6859f5004f68938f10bc029be03f DE-627 ger DE-627 rakwb eng GE1-350 A. Gaudel verfasserin aut Tropospheric Ozone Assessment Report: Present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier 'The Tropospheric Ozone Assessment Report' (TOAR) is an activity of the International Global Atmospheric Chemistry Project. This paper is a component of the report, focusing on the present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation. Utilizing the TOAR surface ozone database, several figures present the global distribution and trends of daytime average ozone at 2702 non-urban monitoring sites, highlighting the regions and seasons of the world with the greatest ozone levels. Similarly, ozonesonde and commercial aircraft observations reveal ozone’s distribution throughout the depth of the free troposphere. Long-term surface observations are limited in their global spatial coverage, but data from remote locations indicate that ozone in the 21st century is greater than during the 1970s and 1980s. While some remote sites and many sites in the heavily polluted regions of East Asia show ozone increases since 2000, many others show decreases and there is no clear global pattern for surface ozone changes since 2000. Two new satellite products provide detailed views of ozone in the lower troposphere across East Asia and Europe, revealing the full spatial extent of the spring and summer ozone enhancements across eastern China that cannot be assessed from limited surface observations. Sufficient data are now available (ozonesondes, satellite, aircraft) across the tropics from South America eastwards to the western Pacific Ocean, to indicate a likely tropospheric column ozone increase since the 1990s. The 2014–2016 mean tropospheric ozone burden (TOB) between 60°N–60°S from five satellite products is 300 Tg ± 4%. While this agreement is excellent, the products differ in their quantification of TOB trends and further work is required to reconcile the differences. Satellites can now estimate ozone’s global long-wave radiative effect, but evaluation is difficult due to limited in situ observations where the radiative effect is greatest. tropospheric ozone ground-level ozone Tropospheric composition and chemistry Global tropospheric ozone burden Ozone trends Environmental sciences O. R. Cooper verfasserin aut G. Ancellet verfasserin aut B. Barret verfasserin aut A. Boynard verfasserin aut J. P. Burrows verfasserin aut C. Clerbaux verfasserin aut P. -F. Coheur verfasserin aut J. Cuesta verfasserin aut E. Cuevas verfasserin aut S. Doniki verfasserin aut G. Dufour verfasserin aut F. Ebojie verfasserin aut G. Foret verfasserin aut O. Garcia verfasserin aut M. J. Granados Muños verfasserin aut J. W. Hannigan verfasserin aut F. Hase verfasserin aut G. Huang verfasserin aut B. Hassler verfasserin aut D. Hurtmans verfasserin aut D. Jaffe verfasserin aut N. Jones verfasserin aut P. Kalabokas verfasserin aut B. Kerridge verfasserin aut S. S. Kulawik verfasserin aut B. Latter verfasserin aut T. Leblanc verfasserin aut E. Le Flochmoën verfasserin aut W. Lin verfasserin aut J. Liu verfasserin aut X. Liu verfasserin aut E. Mahieu verfasserin aut A. McClure-Begley verfasserin aut J. L. Neu verfasserin aut M. Osman verfasserin aut M. Palm verfasserin aut H. Petetin verfasserin aut I. Petropavlovskikh verfasserin aut R. Querel verfasserin aut N. Rahpoe verfasserin aut A. Rozanov verfasserin aut M. G. Schultz verfasserin aut J. Schwab verfasserin aut R. Siddans verfasserin aut D. Smale verfasserin aut M. Steinbacher verfasserin aut H. Tanimoto verfasserin aut D. W. Tarasick verfasserin aut V. Thouret verfasserin aut A. M. Thompson verfasserin aut T. Trickl verfasserin aut E. Weatherhead verfasserin aut C. Wespes verfasserin aut H. M. Worden verfasserin aut C. Vigouroux verfasserin aut X. Xu verfasserin aut G. Zeng verfasserin aut J. Ziemke verfasserin aut In Elementa: Science of the Anthropocene BioOne, 2014 6(2018), 1 (DE-627)774106972 (DE-600)2745461-7 23251026 nnns volume:6 year:2018 number:1 https://doi.org/10.1525/elementa.291 kostenfrei https://doaj.org/article/a63a6859f5004f68938f10bc029be03f kostenfrei https://www.elementascience.org/articles/291 kostenfrei https://doaj.org/toc/2325-1026 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 6 2018 1 |
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10.1525/elementa.291 doi (DE-627)DOAJ001616234 (DE-599)DOAJa63a6859f5004f68938f10bc029be03f DE-627 ger DE-627 rakwb eng GE1-350 A. Gaudel verfasserin aut Tropospheric Ozone Assessment Report: Present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier 'The Tropospheric Ozone Assessment Report' (TOAR) is an activity of the International Global Atmospheric Chemistry Project. This paper is a component of the report, focusing on the present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation. Utilizing the TOAR surface ozone database, several figures present the global distribution and trends of daytime average ozone at 2702 non-urban monitoring sites, highlighting the regions and seasons of the world with the greatest ozone levels. Similarly, ozonesonde and commercial aircraft observations reveal ozone’s distribution throughout the depth of the free troposphere. Long-term surface observations are limited in their global spatial coverage, but data from remote locations indicate that ozone in the 21st century is greater than during the 1970s and 1980s. While some remote sites and many sites in the heavily polluted regions of East Asia show ozone increases since 2000, many others show decreases and there is no clear global pattern for surface ozone changes since 2000. Two new satellite products provide detailed views of ozone in the lower troposphere across East Asia and Europe, revealing the full spatial extent of the spring and summer ozone enhancements across eastern China that cannot be assessed from limited surface observations. Sufficient data are now available (ozonesondes, satellite, aircraft) across the tropics from South America eastwards to the western Pacific Ocean, to indicate a likely tropospheric column ozone increase since the 1990s. The 2014–2016 mean tropospheric ozone burden (TOB) between 60°N–60°S from five satellite products is 300 Tg ± 4%. While this agreement is excellent, the products differ in their quantification of TOB trends and further work is required to reconcile the differences. Satellites can now estimate ozone’s global long-wave radiative effect, but evaluation is difficult due to limited in situ observations where the radiative effect is greatest. tropospheric ozone ground-level ozone Tropospheric composition and chemistry Global tropospheric ozone burden Ozone trends Environmental sciences O. R. Cooper verfasserin aut G. Ancellet verfasserin aut B. Barret verfasserin aut A. Boynard verfasserin aut J. P. Burrows verfasserin aut C. Clerbaux verfasserin aut P. -F. Coheur verfasserin aut J. Cuesta verfasserin aut E. Cuevas verfasserin aut S. Doniki verfasserin aut G. Dufour verfasserin aut F. Ebojie verfasserin aut G. Foret verfasserin aut O. Garcia verfasserin aut M. J. Granados Muños verfasserin aut J. W. Hannigan verfasserin aut F. Hase verfasserin aut G. Huang verfasserin aut B. Hassler verfasserin aut D. Hurtmans verfasserin aut D. Jaffe verfasserin aut N. Jones verfasserin aut P. Kalabokas verfasserin aut B. Kerridge verfasserin aut S. S. Kulawik verfasserin aut B. Latter verfasserin aut T. Leblanc verfasserin aut E. Le Flochmoën verfasserin aut W. Lin verfasserin aut J. Liu verfasserin aut X. Liu verfasserin aut E. Mahieu verfasserin aut A. McClure-Begley verfasserin aut J. L. Neu verfasserin aut M. Osman verfasserin aut M. Palm verfasserin aut H. Petetin verfasserin aut I. Petropavlovskikh verfasserin aut R. Querel verfasserin aut N. Rahpoe verfasserin aut A. Rozanov verfasserin aut M. G. Schultz verfasserin aut J. Schwab verfasserin aut R. Siddans verfasserin aut D. Smale verfasserin aut M. Steinbacher verfasserin aut H. Tanimoto verfasserin aut D. W. Tarasick verfasserin aut V. Thouret verfasserin aut A. M. Thompson verfasserin aut T. Trickl verfasserin aut E. Weatherhead verfasserin aut C. Wespes verfasserin aut H. M. Worden verfasserin aut C. Vigouroux verfasserin aut X. Xu verfasserin aut G. Zeng verfasserin aut J. Ziemke verfasserin aut In Elementa: Science of the Anthropocene BioOne, 2014 6(2018), 1 (DE-627)774106972 (DE-600)2745461-7 23251026 nnns volume:6 year:2018 number:1 https://doi.org/10.1525/elementa.291 kostenfrei https://doaj.org/article/a63a6859f5004f68938f10bc029be03f kostenfrei https://www.elementascience.org/articles/291 kostenfrei https://doaj.org/toc/2325-1026 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 6 2018 1 |
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10.1525/elementa.291 doi (DE-627)DOAJ001616234 (DE-599)DOAJa63a6859f5004f68938f10bc029be03f DE-627 ger DE-627 rakwb eng GE1-350 A. Gaudel verfasserin aut Tropospheric Ozone Assessment Report: Present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier 'The Tropospheric Ozone Assessment Report' (TOAR) is an activity of the International Global Atmospheric Chemistry Project. This paper is a component of the report, focusing on the present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation. Utilizing the TOAR surface ozone database, several figures present the global distribution and trends of daytime average ozone at 2702 non-urban monitoring sites, highlighting the regions and seasons of the world with the greatest ozone levels. Similarly, ozonesonde and commercial aircraft observations reveal ozone’s distribution throughout the depth of the free troposphere. Long-term surface observations are limited in their global spatial coverage, but data from remote locations indicate that ozone in the 21st century is greater than during the 1970s and 1980s. While some remote sites and many sites in the heavily polluted regions of East Asia show ozone increases since 2000, many others show decreases and there is no clear global pattern for surface ozone changes since 2000. Two new satellite products provide detailed views of ozone in the lower troposphere across East Asia and Europe, revealing the full spatial extent of the spring and summer ozone enhancements across eastern China that cannot be assessed from limited surface observations. Sufficient data are now available (ozonesondes, satellite, aircraft) across the tropics from South America eastwards to the western Pacific Ocean, to indicate a likely tropospheric column ozone increase since the 1990s. The 2014–2016 mean tropospheric ozone burden (TOB) between 60°N–60°S from five satellite products is 300 Tg ± 4%. While this agreement is excellent, the products differ in their quantification of TOB trends and further work is required to reconcile the differences. Satellites can now estimate ozone’s global long-wave radiative effect, but evaluation is difficult due to limited in situ observations where the radiative effect is greatest. tropospheric ozone ground-level ozone Tropospheric composition and chemistry Global tropospheric ozone burden Ozone trends Environmental sciences O. R. Cooper verfasserin aut G. Ancellet verfasserin aut B. Barret verfasserin aut A. Boynard verfasserin aut J. P. Burrows verfasserin aut C. Clerbaux verfasserin aut P. -F. Coheur verfasserin aut J. Cuesta verfasserin aut E. Cuevas verfasserin aut S. Doniki verfasserin aut G. Dufour verfasserin aut F. Ebojie verfasserin aut G. Foret verfasserin aut O. Garcia verfasserin aut M. J. Granados Muños verfasserin aut J. W. Hannigan verfasserin aut F. Hase verfasserin aut G. Huang verfasserin aut B. Hassler verfasserin aut D. Hurtmans verfasserin aut D. Jaffe verfasserin aut N. Jones verfasserin aut P. Kalabokas verfasserin aut B. Kerridge verfasserin aut S. S. Kulawik verfasserin aut B. Latter verfasserin aut T. Leblanc verfasserin aut E. Le Flochmoën verfasserin aut W. Lin verfasserin aut J. Liu verfasserin aut X. Liu verfasserin aut E. Mahieu verfasserin aut A. McClure-Begley verfasserin aut J. L. Neu verfasserin aut M. Osman verfasserin aut M. Palm verfasserin aut H. Petetin verfasserin aut I. Petropavlovskikh verfasserin aut R. Querel verfasserin aut N. Rahpoe verfasserin aut A. Rozanov verfasserin aut M. G. Schultz verfasserin aut J. 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Ziemke verfasserin aut In Elementa: Science of the Anthropocene BioOne, 2014 6(2018), 1 (DE-627)774106972 (DE-600)2745461-7 23251026 nnns volume:6 year:2018 number:1 https://doi.org/10.1525/elementa.291 kostenfrei https://doaj.org/article/a63a6859f5004f68938f10bc029be03f kostenfrei https://www.elementascience.org/articles/291 kostenfrei https://doaj.org/toc/2325-1026 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 6 2018 1 |
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10.1525/elementa.291 doi (DE-627)DOAJ001616234 (DE-599)DOAJa63a6859f5004f68938f10bc029be03f DE-627 ger DE-627 rakwb eng GE1-350 A. Gaudel verfasserin aut Tropospheric Ozone Assessment Report: Present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier 'The Tropospheric Ozone Assessment Report' (TOAR) is an activity of the International Global Atmospheric Chemistry Project. This paper is a component of the report, focusing on the present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation. Utilizing the TOAR surface ozone database, several figures present the global distribution and trends of daytime average ozone at 2702 non-urban monitoring sites, highlighting the regions and seasons of the world with the greatest ozone levels. Similarly, ozonesonde and commercial aircraft observations reveal ozone’s distribution throughout the depth of the free troposphere. Long-term surface observations are limited in their global spatial coverage, but data from remote locations indicate that ozone in the 21st century is greater than during the 1970s and 1980s. While some remote sites and many sites in the heavily polluted regions of East Asia show ozone increases since 2000, many others show decreases and there is no clear global pattern for surface ozone changes since 2000. Two new satellite products provide detailed views of ozone in the lower troposphere across East Asia and Europe, revealing the full spatial extent of the spring and summer ozone enhancements across eastern China that cannot be assessed from limited surface observations. Sufficient data are now available (ozonesondes, satellite, aircraft) across the tropics from South America eastwards to the western Pacific Ocean, to indicate a likely tropospheric column ozone increase since the 1990s. The 2014–2016 mean tropospheric ozone burden (TOB) between 60°N–60°S from five satellite products is 300 Tg ± 4%. While this agreement is excellent, the products differ in their quantification of TOB trends and further work is required to reconcile the differences. Satellites can now estimate ozone’s global long-wave radiative effect, but evaluation is difficult due to limited in situ observations where the radiative effect is greatest. tropospheric ozone ground-level ozone Tropospheric composition and chemistry Global tropospheric ozone burden Ozone trends Environmental sciences O. R. Cooper verfasserin aut G. Ancellet verfasserin aut B. Barret verfasserin aut A. Boynard verfasserin aut J. P. Burrows verfasserin aut C. Clerbaux verfasserin aut P. -F. Coheur verfasserin aut J. Cuesta verfasserin aut E. Cuevas verfasserin aut S. Doniki verfasserin aut G. Dufour verfasserin aut F. Ebojie verfasserin aut G. Foret verfasserin aut O. Garcia verfasserin aut M. J. Granados Muños verfasserin aut J. W. Hannigan verfasserin aut F. Hase verfasserin aut G. Huang verfasserin aut B. Hassler verfasserin aut D. Hurtmans verfasserin aut D. Jaffe verfasserin aut N. Jones verfasserin aut P. Kalabokas verfasserin aut B. Kerridge verfasserin aut S. S. Kulawik verfasserin aut B. Latter verfasserin aut T. Leblanc verfasserin aut E. Le Flochmoën verfasserin aut W. Lin verfasserin aut J. Liu verfasserin aut X. Liu verfasserin aut E. Mahieu verfasserin aut A. McClure-Begley verfasserin aut J. L. Neu verfasserin aut M. Osman verfasserin aut M. Palm verfasserin aut H. Petetin verfasserin aut I. Petropavlovskikh verfasserin aut R. Querel verfasserin aut N. Rahpoe verfasserin aut A. Rozanov verfasserin aut M. G. Schultz verfasserin aut J. Schwab verfasserin aut R. Siddans verfasserin aut D. Smale verfasserin aut M. Steinbacher verfasserin aut H. Tanimoto verfasserin aut D. W. Tarasick verfasserin aut V. Thouret verfasserin aut A. M. Thompson verfasserin aut T. Trickl verfasserin aut E. Weatherhead verfasserin aut C. Wespes verfasserin aut H. M. Worden verfasserin aut C. Vigouroux verfasserin aut X. Xu verfasserin aut G. Zeng verfasserin aut J. Ziemke verfasserin aut In Elementa: Science of the Anthropocene BioOne, 2014 6(2018), 1 (DE-627)774106972 (DE-600)2745461-7 23251026 nnns volume:6 year:2018 number:1 https://doi.org/10.1525/elementa.291 kostenfrei https://doaj.org/article/a63a6859f5004f68938f10bc029be03f kostenfrei https://www.elementascience.org/articles/291 kostenfrei https://doaj.org/toc/2325-1026 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 6 2018 1 |
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10.1525/elementa.291 doi (DE-627)DOAJ001616234 (DE-599)DOAJa63a6859f5004f68938f10bc029be03f DE-627 ger DE-627 rakwb eng GE1-350 A. Gaudel verfasserin aut Tropospheric Ozone Assessment Report: Present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier 'The Tropospheric Ozone Assessment Report' (TOAR) is an activity of the International Global Atmospheric Chemistry Project. This paper is a component of the report, focusing on the present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation. Utilizing the TOAR surface ozone database, several figures present the global distribution and trends of daytime average ozone at 2702 non-urban monitoring sites, highlighting the regions and seasons of the world with the greatest ozone levels. Similarly, ozonesonde and commercial aircraft observations reveal ozone’s distribution throughout the depth of the free troposphere. Long-term surface observations are limited in their global spatial coverage, but data from remote locations indicate that ozone in the 21st century is greater than during the 1970s and 1980s. While some remote sites and many sites in the heavily polluted regions of East Asia show ozone increases since 2000, many others show decreases and there is no clear global pattern for surface ozone changes since 2000. Two new satellite products provide detailed views of ozone in the lower troposphere across East Asia and Europe, revealing the full spatial extent of the spring and summer ozone enhancements across eastern China that cannot be assessed from limited surface observations. Sufficient data are now available (ozonesondes, satellite, aircraft) across the tropics from South America eastwards to the western Pacific Ocean, to indicate a likely tropospheric column ozone increase since the 1990s. The 2014–2016 mean tropospheric ozone burden (TOB) between 60°N–60°S from five satellite products is 300 Tg ± 4%. While this agreement is excellent, the products differ in their quantification of TOB trends and further work is required to reconcile the differences. Satellites can now estimate ozone’s global long-wave radiative effect, but evaluation is difficult due to limited in situ observations where the radiative effect is greatest. tropospheric ozone ground-level ozone Tropospheric composition and chemistry Global tropospheric ozone burden Ozone trends Environmental sciences O. R. Cooper verfasserin aut G. Ancellet verfasserin aut B. Barret verfasserin aut A. Boynard verfasserin aut J. P. Burrows verfasserin aut C. Clerbaux verfasserin aut P. -F. Coheur verfasserin aut J. Cuesta verfasserin aut E. Cuevas verfasserin aut S. Doniki verfasserin aut G. Dufour verfasserin aut F. Ebojie verfasserin aut G. Foret verfasserin aut O. Garcia verfasserin aut M. J. Granados Muños verfasserin aut J. W. Hannigan verfasserin aut F. Hase verfasserin aut G. Huang verfasserin aut B. Hassler verfasserin aut D. Hurtmans verfasserin aut D. Jaffe verfasserin aut N. Jones verfasserin aut P. Kalabokas verfasserin aut B. Kerridge verfasserin aut S. S. Kulawik verfasserin aut B. Latter verfasserin aut T. Leblanc verfasserin aut E. Le Flochmoën verfasserin aut W. Lin verfasserin aut J. Liu verfasserin aut X. Liu verfasserin aut E. Mahieu verfasserin aut A. McClure-Begley verfasserin aut J. L. Neu verfasserin aut M. Osman verfasserin aut M. Palm verfasserin aut H. Petetin verfasserin aut I. Petropavlovskikh verfasserin aut R. Querel verfasserin aut N. Rahpoe verfasserin aut A. Rozanov verfasserin aut M. G. Schultz verfasserin aut J. Schwab verfasserin aut R. Siddans verfasserin aut D. Smale verfasserin aut M. Steinbacher verfasserin aut H. Tanimoto verfasserin aut D. W. Tarasick verfasserin aut V. Thouret verfasserin aut A. M. Thompson verfasserin aut T. Trickl verfasserin aut E. Weatherhead verfasserin aut C. Wespes verfasserin aut H. M. Worden verfasserin aut C. Vigouroux verfasserin aut X. Xu verfasserin aut G. Zeng verfasserin aut J. Ziemke verfasserin aut In Elementa: Science of the Anthropocene BioOne, 2014 6(2018), 1 (DE-627)774106972 (DE-600)2745461-7 23251026 nnns volume:6 year:2018 number:1 https://doi.org/10.1525/elementa.291 kostenfrei https://doaj.org/article/a63a6859f5004f68938f10bc029be03f kostenfrei https://www.elementascience.org/articles/291 kostenfrei https://doaj.org/toc/2325-1026 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 6 2018 1 |
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A. Gaudel @@aut@@ O. R. Cooper @@aut@@ G. Ancellet @@aut@@ B. Barret @@aut@@ A. Boynard @@aut@@ J. P. Burrows @@aut@@ C. Clerbaux @@aut@@ P. -F. Coheur @@aut@@ J. Cuesta @@aut@@ E. Cuevas @@aut@@ S. Doniki @@aut@@ G. Dufour @@aut@@ F. Ebojie @@aut@@ G. Foret @@aut@@ O. Garcia @@aut@@ M. J. Granados Muños @@aut@@ J. W. Hannigan @@aut@@ F. Hase @@aut@@ G. Huang @@aut@@ B. Hassler @@aut@@ D. Hurtmans @@aut@@ D. Jaffe @@aut@@ N. Jones @@aut@@ P. Kalabokas @@aut@@ B. Kerridge @@aut@@ S. S. Kulawik @@aut@@ B. Latter @@aut@@ T. Leblanc @@aut@@ E. Le Flochmoën @@aut@@ W. Lin @@aut@@ J. Liu @@aut@@ X. Liu @@aut@@ E. Mahieu @@aut@@ A. McClure-Begley @@aut@@ J. L. Neu @@aut@@ M. Osman @@aut@@ M. Palm @@aut@@ H. Petetin @@aut@@ I. Petropavlovskikh @@aut@@ R. Querel @@aut@@ N. Rahpoe @@aut@@ A. Rozanov @@aut@@ M. G. Schultz @@aut@@ J. Schwab @@aut@@ R. Siddans @@aut@@ D. Smale @@aut@@ M. Steinbacher @@aut@@ H. Tanimoto @@aut@@ D. W. Tarasick @@aut@@ V. Thouret @@aut@@ A. M. Thompson @@aut@@ T. Trickl @@aut@@ E. Weatherhead @@aut@@ C. Wespes @@aut@@ H. M. Worden @@aut@@ C. Vigouroux @@aut@@ X. Xu @@aut@@ G. Zeng @@aut@@ J. Ziemke @@aut@@ |
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GE1-350 Tropospheric Ozone Assessment Report: Present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation tropospheric ozone ground-level ozone Tropospheric composition and chemistry Global tropospheric ozone burden Ozone trends |
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Tropospheric Ozone Assessment Report: Present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation |
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A. Gaudel O. R. Cooper G. Ancellet B. Barret A. Boynard J. P. Burrows C. Clerbaux P. -F. Coheur J. Cuesta E. Cuevas S. Doniki G. Dufour F. Ebojie G. Foret O. Garcia M. J. Granados Muños J. W. Hannigan F. Hase G. Huang B. Hassler D. Hurtmans D. Jaffe N. Jones P. Kalabokas B. Kerridge S. S. Kulawik B. Latter T. Leblanc E. Le Flochmoën W. Lin J. Liu X. Liu E. Mahieu A. McClure-Begley J. L. Neu M. Osman M. Palm H. Petetin I. Petropavlovskikh R. Querel N. Rahpoe A. Rozanov M. G. Schultz J. Schwab R. Siddans D. Smale M. Steinbacher H. Tanimoto D. W. Tarasick V. Thouret A. M. Thompson T. Trickl E. Weatherhead C. Wespes H. M. Worden C. Vigouroux X. Xu G. Zeng J. Ziemke |
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10.1525/elementa.291 |
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tropospheric ozone assessment report: present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation |
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GE1-350 |
title_auth |
Tropospheric Ozone Assessment Report: Present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation |
abstract |
'The Tropospheric Ozone Assessment Report' (TOAR) is an activity of the International Global Atmospheric Chemistry Project. This paper is a component of the report, focusing on the present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation. Utilizing the TOAR surface ozone database, several figures present the global distribution and trends of daytime average ozone at 2702 non-urban monitoring sites, highlighting the regions and seasons of the world with the greatest ozone levels. Similarly, ozonesonde and commercial aircraft observations reveal ozone’s distribution throughout the depth of the free troposphere. Long-term surface observations are limited in their global spatial coverage, but data from remote locations indicate that ozone in the 21st century is greater than during the 1970s and 1980s. While some remote sites and many sites in the heavily polluted regions of East Asia show ozone increases since 2000, many others show decreases and there is no clear global pattern for surface ozone changes since 2000. Two new satellite products provide detailed views of ozone in the lower troposphere across East Asia and Europe, revealing the full spatial extent of the spring and summer ozone enhancements across eastern China that cannot be assessed from limited surface observations. Sufficient data are now available (ozonesondes, satellite, aircraft) across the tropics from South America eastwards to the western Pacific Ocean, to indicate a likely tropospheric column ozone increase since the 1990s. The 2014–2016 mean tropospheric ozone burden (TOB) between 60°N–60°S from five satellite products is 300 Tg ± 4%. While this agreement is excellent, the products differ in their quantification of TOB trends and further work is required to reconcile the differences. Satellites can now estimate ozone’s global long-wave radiative effect, but evaluation is difficult due to limited in situ observations where the radiative effect is greatest. |
abstractGer |
'The Tropospheric Ozone Assessment Report' (TOAR) is an activity of the International Global Atmospheric Chemistry Project. This paper is a component of the report, focusing on the present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation. Utilizing the TOAR surface ozone database, several figures present the global distribution and trends of daytime average ozone at 2702 non-urban monitoring sites, highlighting the regions and seasons of the world with the greatest ozone levels. Similarly, ozonesonde and commercial aircraft observations reveal ozone’s distribution throughout the depth of the free troposphere. Long-term surface observations are limited in their global spatial coverage, but data from remote locations indicate that ozone in the 21st century is greater than during the 1970s and 1980s. While some remote sites and many sites in the heavily polluted regions of East Asia show ozone increases since 2000, many others show decreases and there is no clear global pattern for surface ozone changes since 2000. Two new satellite products provide detailed views of ozone in the lower troposphere across East Asia and Europe, revealing the full spatial extent of the spring and summer ozone enhancements across eastern China that cannot be assessed from limited surface observations. Sufficient data are now available (ozonesondes, satellite, aircraft) across the tropics from South America eastwards to the western Pacific Ocean, to indicate a likely tropospheric column ozone increase since the 1990s. The 2014–2016 mean tropospheric ozone burden (TOB) between 60°N–60°S from five satellite products is 300 Tg ± 4%. While this agreement is excellent, the products differ in their quantification of TOB trends and further work is required to reconcile the differences. Satellites can now estimate ozone’s global long-wave radiative effect, but evaluation is difficult due to limited in situ observations where the radiative effect is greatest. |
abstract_unstemmed |
'The Tropospheric Ozone Assessment Report' (TOAR) is an activity of the International Global Atmospheric Chemistry Project. This paper is a component of the report, focusing on the present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation. Utilizing the TOAR surface ozone database, several figures present the global distribution and trends of daytime average ozone at 2702 non-urban monitoring sites, highlighting the regions and seasons of the world with the greatest ozone levels. Similarly, ozonesonde and commercial aircraft observations reveal ozone’s distribution throughout the depth of the free troposphere. Long-term surface observations are limited in their global spatial coverage, but data from remote locations indicate that ozone in the 21st century is greater than during the 1970s and 1980s. While some remote sites and many sites in the heavily polluted regions of East Asia show ozone increases since 2000, many others show decreases and there is no clear global pattern for surface ozone changes since 2000. Two new satellite products provide detailed views of ozone in the lower troposphere across East Asia and Europe, revealing the full spatial extent of the spring and summer ozone enhancements across eastern China that cannot be assessed from limited surface observations. Sufficient data are now available (ozonesondes, satellite, aircraft) across the tropics from South America eastwards to the western Pacific Ocean, to indicate a likely tropospheric column ozone increase since the 1990s. The 2014–2016 mean tropospheric ozone burden (TOB) between 60°N–60°S from five satellite products is 300 Tg ± 4%. While this agreement is excellent, the products differ in their quantification of TOB trends and further work is required to reconcile the differences. Satellites can now estimate ozone’s global long-wave radiative effect, but evaluation is difficult due to limited in situ observations where the radiative effect is greatest. |
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Tropospheric Ozone Assessment Report: Present-day distribution and trends of tropospheric ozone relevant to climate and global atmospheric chemistry model evaluation |
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https://doi.org/10.1525/elementa.291 https://doaj.org/article/a63a6859f5004f68938f10bc029be03f https://www.elementascience.org/articles/291 https://doaj.org/toc/2325-1026 |
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O. R. Cooper G. Ancellet B. Barret A. Boynard J. P. Burrows C. Clerbaux P. -F. Coheur J. Cuesta E. Cuevas S. Doniki G. Dufour F. Ebojie G. Foret O. Garcia M. J. Granados Muños J. W. Hannigan F. Hase G. Huang B. Hassler D. Hurtmans D. Jaffe N. Jones P. Kalabokas B. Kerridge S. S. Kulawik B. Latter T. Leblanc E. Le Flochmoën W. Lin J. Liu X. Liu E. Mahieu A. McClure-Begley J. L. Neu M. Osman M. Palm H. Petetin I. Petropavlovskikh R. Querel N. Rahpoe A. Rozanov M. G. Schultz J. Schwab R. Siddans D. Smale M. Steinbacher H. Tanimoto D. W. Tarasick V. Thouret A. M. Thompson T. Trickl E. Weatherhead C. Wespes H. M. Worden C. Vigouroux X. Xu G. Zeng J. Ziemke |
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O. R. Cooper G. Ancellet B. Barret A. Boynard J. P. Burrows C. Clerbaux P. -F. Coheur J. Cuesta E. Cuevas S. Doniki G. Dufour F. Ebojie G. Foret O. Garcia M. J. Granados Muños J. W. Hannigan F. Hase G. Huang B. Hassler D. Hurtmans D. Jaffe N. Jones P. Kalabokas B. Kerridge S. S. Kulawik B. Latter T. Leblanc E. Le Flochmoën W. Lin J. Liu X. Liu E. Mahieu A. McClure-Begley J. L. Neu M. Osman M. Palm H. Petetin I. Petropavlovskikh R. Querel N. Rahpoe A. Rozanov M. G. Schultz J. Schwab R. Siddans D. Smale M. Steinbacher H. Tanimoto D. W. Tarasick V. Thouret A. M. Thompson T. Trickl E. Weatherhead C. Wespes H. M. Worden C. Vigouroux X. Xu G. Zeng J. Ziemke |
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GE - Environmental Sciences |
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10.1525/elementa.291 |
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2024-07-03T21:28:52.997Z |
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|
score |
7.400899 |