Persistence of ozone anomalies in the Arctic stratospheric vortex in autumn
Dynamical processes during the formation phase of the Arctic stratospheric vortex in autumn (from September to December) can introduce considerable interannual variability in the amount of ozone that is incorporated into the vortex. Chemistry in autumn tends to remove part of this variability becaus...
| Main Authors: | , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2012-06-01
|
| Series: | Atmospheric Chemistry and Physics |
| Online Access: | http://www.atmos-chem-phys.net/12/4817/2012/acp-12-4817-2012.pdf |
| _version_ | 1811236419098640384 |
|---|---|
| author | D. Blessmann I. Wohltmann R. Lehmann M. Rex |
| author_facet | D. Blessmann I. Wohltmann R. Lehmann M. Rex |
| author_sort | D. Blessmann |
| collection | DOAJ |
| description | Dynamical processes during the formation phase of the Arctic stratospheric vortex in autumn (from September to December) can introduce considerable interannual variability in the amount of ozone that is incorporated into the vortex. Chemistry in autumn tends to remove part of this variability because ozone relaxes towards equilibrium. As a quantitative measure of how important dynamical variability during vortex formation is for the winter ozone abundances above the Arctic we analyze which fraction of an ozone anomaly induced during vortex formation persists until early winter (3 January). The work is based on the Lagrangian Chemistry Transport Model ATLAS. In a case study, model runs for the winter 1999–2000 are used to assess the fate of an ozone anomaly artificially introduced during the vortex formation phase on 16 September. In addition, runs with reduced resolution explore the sensitivity of the results to interannual changes in transport, mixing, temperatures and NO<sub>x</sub>. The runs provide information about the persistence of the induced ozone anomaly as a function of time, potential temperature and latitude. The induced ozone anomaly survives longer inside the polar vortex than outside the vortex. Half of the initial perturbation survives until 3 January at 550 K inside the polar vortex, with a rapid fall off towards higher levels, mainly due to NO<sub>x</sub> induced chemistry. Above 750 K the signal falls to values below 0.5%. Hence, dynamically induced ozone variability from the early vortex formation phase cannot significantly contribute to early winter variability above 750 K. At lower levels increasingly larger fractions of the initial perturbation survive, reaching 90% at 450 K. In this vertical range dynamical processes during the vortex formation phase are crucial for the ozone abundance in early winter. |
| first_indexed | 2024-04-12T12:09:36Z |
| format | Article |
| id | doaj.art-dc5525b559bd480bb35ce40956970ff5 |
| institution | Directory Open Access Journal |
| issn | 1680-7316 1680-7324 |
| language | English |
| last_indexed | 2024-04-12T12:09:36Z |
| publishDate | 2012-06-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Atmospheric Chemistry and Physics |
| spelling | doaj.art-dc5525b559bd480bb35ce40956970ff52022-12-22T03:33:38ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242012-06-0112114817482310.5194/acp-12-4817-2012Persistence of ozone anomalies in the Arctic stratospheric vortex in autumnD. BlessmannI. WohltmannR. LehmannM. RexDynamical processes during the formation phase of the Arctic stratospheric vortex in autumn (from September to December) can introduce considerable interannual variability in the amount of ozone that is incorporated into the vortex. Chemistry in autumn tends to remove part of this variability because ozone relaxes towards equilibrium. As a quantitative measure of how important dynamical variability during vortex formation is for the winter ozone abundances above the Arctic we analyze which fraction of an ozone anomaly induced during vortex formation persists until early winter (3 January). The work is based on the Lagrangian Chemistry Transport Model ATLAS. In a case study, model runs for the winter 1999–2000 are used to assess the fate of an ozone anomaly artificially introduced during the vortex formation phase on 16 September. In addition, runs with reduced resolution explore the sensitivity of the results to interannual changes in transport, mixing, temperatures and NO<sub>x</sub>. The runs provide information about the persistence of the induced ozone anomaly as a function of time, potential temperature and latitude. The induced ozone anomaly survives longer inside the polar vortex than outside the vortex. Half of the initial perturbation survives until 3 January at 550 K inside the polar vortex, with a rapid fall off towards higher levels, mainly due to NO<sub>x</sub> induced chemistry. Above 750 K the signal falls to values below 0.5%. Hence, dynamically induced ozone variability from the early vortex formation phase cannot significantly contribute to early winter variability above 750 K. At lower levels increasingly larger fractions of the initial perturbation survive, reaching 90% at 450 K. In this vertical range dynamical processes during the vortex formation phase are crucial for the ozone abundance in early winter.http://www.atmos-chem-phys.net/12/4817/2012/acp-12-4817-2012.pdf |
| spellingShingle | D. Blessmann I. Wohltmann R. Lehmann M. Rex Persistence of ozone anomalies in the Arctic stratospheric vortex in autumn Atmospheric Chemistry and Physics |
| title | Persistence of ozone anomalies in the Arctic stratospheric vortex in autumn |
| title_full | Persistence of ozone anomalies in the Arctic stratospheric vortex in autumn |
| title_fullStr | Persistence of ozone anomalies in the Arctic stratospheric vortex in autumn |
| title_full_unstemmed | Persistence of ozone anomalies in the Arctic stratospheric vortex in autumn |
| title_short | Persistence of ozone anomalies in the Arctic stratospheric vortex in autumn |
| title_sort | persistence of ozone anomalies in the arctic stratospheric vortex in autumn |
| url | http://www.atmos-chem-phys.net/12/4817/2012/acp-12-4817-2012.pdf |
| work_keys_str_mv | AT dblessmann persistenceofozoneanomaliesinthearcticstratosphericvortexinautumn AT iwohltmann persistenceofozoneanomaliesinthearcticstratosphericvortexinautumn AT rlehmann persistenceofozoneanomaliesinthearcticstratosphericvortexinautumn AT mrex persistenceofozoneanomaliesinthearcticstratosphericvortexinautumn |