Effect of recent sea surface temperature trends on the Arctic stratospheric vortex
Comprehensive chemistry‐climate model experiments and observational data are used to show that up to half of the satellite era early springtime cooling trend in the Arctic lower stratosphere was caused by changing sea surface temperatures (SSTs). An ensemble of experiments forced only by changing SS...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Garfinkel, C. I [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: Journal of geophysical research / D - Washington, DC : Union, 1984, 120(2015), 11, Seite 5404-5416 |
|---|---|
| Übergeordnetes Werk: |
volume:120 ; year:2015 ; number:11 ; pages:5404-5416 |
| Links: |
|---|
| DOI / URN: |
10.1002/2015JD023284 |
|---|
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| 520 | |a Comprehensive chemistry‐climate model experiments and observational data are used to show that up to half of the satellite era early springtime cooling trend in the Arctic lower stratosphere was caused by changing sea surface temperatures (SSTs). An ensemble of experiments forced only by changing SSTs is compared to an ensemble of experiments in which both the observed SSTs and chemically and radiatively active trace species are changing. By comparing the two ensembles, it is shown that warming of Indian Ocean, North Pacific, and North Atlantic SSTs and cooling of the tropical Pacific have strongly contributed to recent polar stratospheric cooling in late winter and early spring. When concentrations of ozone‐depleting substances and greenhouse gases are fixed, polar ozone concentrations show a small but robust decline due to changing SSTs. Ozone loss is larger in the presence of changing concentrations of ozone‐depleting substances and greenhouse gases. The stratospheric changes can be understood by examining the tropospheric height and heat flux anomalies generated by the anomalous SSTs. Finally, recent SST changes have contributed to a decrease in the frequency of late winter stratospheric sudden warmings. SSTs have driven ∼1/2 of observed spring cooling trend in Arctic stratosphere Recent SST trends have driven polar ozone depletion SST anomalies generate anomalous wave driving of the vortex | ||
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| 650 | 4 | |a ozone trends | |
| 650 | 4 | |a SST trends | |
| 650 | 4 | |a ozone loss | |
| 650 | 4 | |a Arctic stratosphere | |
| 650 | 4 | |a Temperature | |
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10.1002/2015JD023284 doi PQ20160617 (DE-627)OLC1957058048 (DE-599)GBVOLC1957058048 (PRQ)p2137-7a4c36c5911ad384978035dd142d3d80349d2deef4fc0439b89c95f7152fbe6a0 (KEY)0137985220150000120001105404effectofrecentseasurfacetemperaturetrendsonthearct DE-627 ger DE-627 rakwb eng 550 DNB Garfinkel, C. I verfasserin aut Effect of recent sea surface temperature trends on the Arctic stratospheric vortex 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Comprehensive chemistry‐climate model experiments and observational data are used to show that up to half of the satellite era early springtime cooling trend in the Arctic lower stratosphere was caused by changing sea surface temperatures (SSTs). An ensemble of experiments forced only by changing SSTs is compared to an ensemble of experiments in which both the observed SSTs and chemically and radiatively active trace species are changing. By comparing the two ensembles, it is shown that warming of Indian Ocean, North Pacific, and North Atlantic SSTs and cooling of the tropical Pacific have strongly contributed to recent polar stratospheric cooling in late winter and early spring. When concentrations of ozone‐depleting substances and greenhouse gases are fixed, polar ozone concentrations show a small but robust decline due to changing SSTs. Ozone loss is larger in the presence of changing concentrations of ozone‐depleting substances and greenhouse gases. The stratospheric changes can be understood by examining the tropospheric height and heat flux anomalies generated by the anomalous SSTs. Finally, recent SST changes have contributed to a decrease in the frequency of late winter stratospheric sudden warmings. SSTs have driven ∼1/2 of observed spring cooling trend in Arctic stratosphere Recent SST trends have driven polar ozone depletion SST anomalies generate anomalous wave driving of the vortex Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. ozone trends SST trends ozone loss Arctic stratosphere Temperature Meteorology Trends Stratosphere Ozone Hurwitz, M. M oth Oman, L. D oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 120(2015), 11, Seite 5404-5416 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:120 year:2015 number:11 pages:5404-5416 http://dx.doi.org/10.1002/2015JD023284 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015JD023284/abstract http://search.proquest.com/docview/1691232864 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 120 2015 11 5404-5416 |
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10.1002/2015JD023284 doi PQ20160617 (DE-627)OLC1957058048 (DE-599)GBVOLC1957058048 (PRQ)p2137-7a4c36c5911ad384978035dd142d3d80349d2deef4fc0439b89c95f7152fbe6a0 (KEY)0137985220150000120001105404effectofrecentseasurfacetemperaturetrendsonthearct DE-627 ger DE-627 rakwb eng 550 DNB Garfinkel, C. I verfasserin aut Effect of recent sea surface temperature trends on the Arctic stratospheric vortex 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Comprehensive chemistry‐climate model experiments and observational data are used to show that up to half of the satellite era early springtime cooling trend in the Arctic lower stratosphere was caused by changing sea surface temperatures (SSTs). An ensemble of experiments forced only by changing SSTs is compared to an ensemble of experiments in which both the observed SSTs and chemically and radiatively active trace species are changing. By comparing the two ensembles, it is shown that warming of Indian Ocean, North Pacific, and North Atlantic SSTs and cooling of the tropical Pacific have strongly contributed to recent polar stratospheric cooling in late winter and early spring. When concentrations of ozone‐depleting substances and greenhouse gases are fixed, polar ozone concentrations show a small but robust decline due to changing SSTs. Ozone loss is larger in the presence of changing concentrations of ozone‐depleting substances and greenhouse gases. The stratospheric changes can be understood by examining the tropospheric height and heat flux anomalies generated by the anomalous SSTs. Finally, recent SST changes have contributed to a decrease in the frequency of late winter stratospheric sudden warmings. SSTs have driven ∼1/2 of observed spring cooling trend in Arctic stratosphere Recent SST trends have driven polar ozone depletion SST anomalies generate anomalous wave driving of the vortex Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. ozone trends SST trends ozone loss Arctic stratosphere Temperature Meteorology Trends Stratosphere Ozone Hurwitz, M. M oth Oman, L. D oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 120(2015), 11, Seite 5404-5416 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:120 year:2015 number:11 pages:5404-5416 http://dx.doi.org/10.1002/2015JD023284 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015JD023284/abstract http://search.proquest.com/docview/1691232864 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 120 2015 11 5404-5416 |
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10.1002/2015JD023284 doi PQ20160617 (DE-627)OLC1957058048 (DE-599)GBVOLC1957058048 (PRQ)p2137-7a4c36c5911ad384978035dd142d3d80349d2deef4fc0439b89c95f7152fbe6a0 (KEY)0137985220150000120001105404effectofrecentseasurfacetemperaturetrendsonthearct DE-627 ger DE-627 rakwb eng 550 DNB Garfinkel, C. I verfasserin aut Effect of recent sea surface temperature trends on the Arctic stratospheric vortex 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Comprehensive chemistry‐climate model experiments and observational data are used to show that up to half of the satellite era early springtime cooling trend in the Arctic lower stratosphere was caused by changing sea surface temperatures (SSTs). An ensemble of experiments forced only by changing SSTs is compared to an ensemble of experiments in which both the observed SSTs and chemically and radiatively active trace species are changing. By comparing the two ensembles, it is shown that warming of Indian Ocean, North Pacific, and North Atlantic SSTs and cooling of the tropical Pacific have strongly contributed to recent polar stratospheric cooling in late winter and early spring. When concentrations of ozone‐depleting substances and greenhouse gases are fixed, polar ozone concentrations show a small but robust decline due to changing SSTs. Ozone loss is larger in the presence of changing concentrations of ozone‐depleting substances and greenhouse gases. The stratospheric changes can be understood by examining the tropospheric height and heat flux anomalies generated by the anomalous SSTs. Finally, recent SST changes have contributed to a decrease in the frequency of late winter stratospheric sudden warmings. SSTs have driven ∼1/2 of observed spring cooling trend in Arctic stratosphere Recent SST trends have driven polar ozone depletion SST anomalies generate anomalous wave driving of the vortex Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. ozone trends SST trends ozone loss Arctic stratosphere Temperature Meteorology Trends Stratosphere Ozone Hurwitz, M. M oth Oman, L. D oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 120(2015), 11, Seite 5404-5416 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:120 year:2015 number:11 pages:5404-5416 http://dx.doi.org/10.1002/2015JD023284 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015JD023284/abstract http://search.proquest.com/docview/1691232864 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 120 2015 11 5404-5416 |
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10.1002/2015JD023284 doi PQ20160617 (DE-627)OLC1957058048 (DE-599)GBVOLC1957058048 (PRQ)p2137-7a4c36c5911ad384978035dd142d3d80349d2deef4fc0439b89c95f7152fbe6a0 (KEY)0137985220150000120001105404effectofrecentseasurfacetemperaturetrendsonthearct DE-627 ger DE-627 rakwb eng 550 DNB Garfinkel, C. I verfasserin aut Effect of recent sea surface temperature trends on the Arctic stratospheric vortex 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Comprehensive chemistry‐climate model experiments and observational data are used to show that up to half of the satellite era early springtime cooling trend in the Arctic lower stratosphere was caused by changing sea surface temperatures (SSTs). An ensemble of experiments forced only by changing SSTs is compared to an ensemble of experiments in which both the observed SSTs and chemically and radiatively active trace species are changing. By comparing the two ensembles, it is shown that warming of Indian Ocean, North Pacific, and North Atlantic SSTs and cooling of the tropical Pacific have strongly contributed to recent polar stratospheric cooling in late winter and early spring. When concentrations of ozone‐depleting substances and greenhouse gases are fixed, polar ozone concentrations show a small but robust decline due to changing SSTs. Ozone loss is larger in the presence of changing concentrations of ozone‐depleting substances and greenhouse gases. The stratospheric changes can be understood by examining the tropospheric height and heat flux anomalies generated by the anomalous SSTs. Finally, recent SST changes have contributed to a decrease in the frequency of late winter stratospheric sudden warmings. SSTs have driven ∼1/2 of observed spring cooling trend in Arctic stratosphere Recent SST trends have driven polar ozone depletion SST anomalies generate anomalous wave driving of the vortex Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. ozone trends SST trends ozone loss Arctic stratosphere Temperature Meteorology Trends Stratosphere Ozone Hurwitz, M. M oth Oman, L. D oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 120(2015), 11, Seite 5404-5416 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:120 year:2015 number:11 pages:5404-5416 http://dx.doi.org/10.1002/2015JD023284 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015JD023284/abstract http://search.proquest.com/docview/1691232864 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 120 2015 11 5404-5416 |
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10.1002/2015JD023284 doi PQ20160617 (DE-627)OLC1957058048 (DE-599)GBVOLC1957058048 (PRQ)p2137-7a4c36c5911ad384978035dd142d3d80349d2deef4fc0439b89c95f7152fbe6a0 (KEY)0137985220150000120001105404effectofrecentseasurfacetemperaturetrendsonthearct DE-627 ger DE-627 rakwb eng 550 DNB Garfinkel, C. I verfasserin aut Effect of recent sea surface temperature trends on the Arctic stratospheric vortex 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Comprehensive chemistry‐climate model experiments and observational data are used to show that up to half of the satellite era early springtime cooling trend in the Arctic lower stratosphere was caused by changing sea surface temperatures (SSTs). An ensemble of experiments forced only by changing SSTs is compared to an ensemble of experiments in which both the observed SSTs and chemically and radiatively active trace species are changing. By comparing the two ensembles, it is shown that warming of Indian Ocean, North Pacific, and North Atlantic SSTs and cooling of the tropical Pacific have strongly contributed to recent polar stratospheric cooling in late winter and early spring. When concentrations of ozone‐depleting substances and greenhouse gases are fixed, polar ozone concentrations show a small but robust decline due to changing SSTs. Ozone loss is larger in the presence of changing concentrations of ozone‐depleting substances and greenhouse gases. The stratospheric changes can be understood by examining the tropospheric height and heat flux anomalies generated by the anomalous SSTs. Finally, recent SST changes have contributed to a decrease in the frequency of late winter stratospheric sudden warmings. SSTs have driven ∼1/2 of observed spring cooling trend in Arctic stratosphere Recent SST trends have driven polar ozone depletion SST anomalies generate anomalous wave driving of the vortex Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. ozone trends SST trends ozone loss Arctic stratosphere Temperature Meteorology Trends Stratosphere Ozone Hurwitz, M. M oth Oman, L. D oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 120(2015), 11, Seite 5404-5416 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:120 year:2015 number:11 pages:5404-5416 http://dx.doi.org/10.1002/2015JD023284 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015JD023284/abstract http://search.proquest.com/docview/1691232864 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 120 2015 11 5404-5416 |
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Garfinkel, C. I |
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550 DNB Effect of recent sea surface temperature trends on the Arctic stratospheric vortex ozone trends SST trends ozone loss Arctic stratosphere Temperature Meteorology Trends Stratosphere Ozone |
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Effect of recent sea surface temperature trends on the Arctic stratospheric vortex |
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Effect of recent sea surface temperature trends on the Arctic stratospheric vortex |
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effect of recent sea surface temperature trends on the arctic stratospheric vortex |
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Effect of recent sea surface temperature trends on the Arctic stratospheric vortex |
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Comprehensive chemistry‐climate model experiments and observational data are used to show that up to half of the satellite era early springtime cooling trend in the Arctic lower stratosphere was caused by changing sea surface temperatures (SSTs). An ensemble of experiments forced only by changing SSTs is compared to an ensemble of experiments in which both the observed SSTs and chemically and radiatively active trace species are changing. By comparing the two ensembles, it is shown that warming of Indian Ocean, North Pacific, and North Atlantic SSTs and cooling of the tropical Pacific have strongly contributed to recent polar stratospheric cooling in late winter and early spring. When concentrations of ozone‐depleting substances and greenhouse gases are fixed, polar ozone concentrations show a small but robust decline due to changing SSTs. Ozone loss is larger in the presence of changing concentrations of ozone‐depleting substances and greenhouse gases. The stratospheric changes can be understood by examining the tropospheric height and heat flux anomalies generated by the anomalous SSTs. Finally, recent SST changes have contributed to a decrease in the frequency of late winter stratospheric sudden warmings. SSTs have driven ∼1/2 of observed spring cooling trend in Arctic stratosphere Recent SST trends have driven polar ozone depletion SST anomalies generate anomalous wave driving of the vortex |
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Comprehensive chemistry‐climate model experiments and observational data are used to show that up to half of the satellite era early springtime cooling trend in the Arctic lower stratosphere was caused by changing sea surface temperatures (SSTs). An ensemble of experiments forced only by changing SSTs is compared to an ensemble of experiments in which both the observed SSTs and chemically and radiatively active trace species are changing. By comparing the two ensembles, it is shown that warming of Indian Ocean, North Pacific, and North Atlantic SSTs and cooling of the tropical Pacific have strongly contributed to recent polar stratospheric cooling in late winter and early spring. When concentrations of ozone‐depleting substances and greenhouse gases are fixed, polar ozone concentrations show a small but robust decline due to changing SSTs. Ozone loss is larger in the presence of changing concentrations of ozone‐depleting substances and greenhouse gases. The stratospheric changes can be understood by examining the tropospheric height and heat flux anomalies generated by the anomalous SSTs. Finally, recent SST changes have contributed to a decrease in the frequency of late winter stratospheric sudden warmings. SSTs have driven ∼1/2 of observed spring cooling trend in Arctic stratosphere Recent SST trends have driven polar ozone depletion SST anomalies generate anomalous wave driving of the vortex |
| abstract_unstemmed |
Comprehensive chemistry‐climate model experiments and observational data are used to show that up to half of the satellite era early springtime cooling trend in the Arctic lower stratosphere was caused by changing sea surface temperatures (SSTs). An ensemble of experiments forced only by changing SSTs is compared to an ensemble of experiments in which both the observed SSTs and chemically and radiatively active trace species are changing. By comparing the two ensembles, it is shown that warming of Indian Ocean, North Pacific, and North Atlantic SSTs and cooling of the tropical Pacific have strongly contributed to recent polar stratospheric cooling in late winter and early spring. When concentrations of ozone‐depleting substances and greenhouse gases are fixed, polar ozone concentrations show a small but robust decline due to changing SSTs. Ozone loss is larger in the presence of changing concentrations of ozone‐depleting substances and greenhouse gases. The stratospheric changes can be understood by examining the tropospheric height and heat flux anomalies generated by the anomalous SSTs. Finally, recent SST changes have contributed to a decrease in the frequency of late winter stratospheric sudden warmings. SSTs have driven ∼1/2 of observed spring cooling trend in Arctic stratosphere Recent SST trends have driven polar ozone depletion SST anomalies generate anomalous wave driving of the vortex |
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Effect of recent sea surface temperature trends on the Arctic stratospheric vortex |
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http://dx.doi.org/10.1002/2015JD023284 http://onlinelibrary.wiley.com/doi/10.1002/2015JD023284/abstract http://search.proquest.com/docview/1691232864 |
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