Atmospheric blocking signatures in total ozone and ozone miniholes

© 2010 American Meteorological Society. This work has been partially supported by the MICINN (Spanish government) under Projects CGL2007-65891-C05-05/CLI (DB and JAG) and CGL2008-05939-C03-02/CLI (M. Anton). ERA-40 reanalysis data were provided by the ECMWF from their data server Web site (http://ww...

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Main Authors: Barriopedro Cepero, David, Antón Martínez, Manuel, García García, José Agustín
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2010
Subjects:
52
Northern-Hemisphere Blocking
Polar Stratospheric Cloud
Long-Term Changes
Mini-Hole Events
Potential Vorticity
Column Ozone
Interannual Variations
Atlantic Oscillation
Era-40 Reanalysis
Middle Latitudes
Astrofísica
Astronomía (Física)
Física atmosférica
2501 Ciencias de la Atmósfera
Arctic
Alaska
Online Access:https://hdl.handle.net/20.500.14352/44116
https://doi.org/10.1175/2010JCLI3508.1
id ftunivcmadrid:oai:docta.ucm.es:20.500.14352/44116
record_format openpolar
institution Open Polar
collection Docta Complutense (Universidad Complutense de Madrid - UCM)
op_collection_id ftunivcmadrid
language English
topic 52
Northern-Hemisphere Blocking
Polar Stratospheric Cloud
Long-Term Changes
Mini-Hole Events
Potential Vorticity
Column Ozone
Interannual Variations
Atlantic Oscillation
Era-40 Reanalysis
Middle Latitudes
Astrofísica
Astronomía (Física)
Física atmosférica
2501 Ciencias de la Atmósfera
spellingShingle 52
Northern-Hemisphere Blocking
Polar Stratospheric Cloud
Long-Term Changes
Mini-Hole Events
Potential Vorticity
Column Ozone
Interannual Variations
Atlantic Oscillation
Era-40 Reanalysis
Middle Latitudes
Astrofísica
Astronomía (Física)
Física atmosférica
2501 Ciencias de la Atmósfera
Barriopedro Cepero, David
Antón Martínez, Manuel
García García, José Agustín
Atmospheric blocking signatures in total ozone and ozone miniholes
topic_facet 52
Northern-Hemisphere Blocking
Polar Stratospheric Cloud
Long-Term Changes
Mini-Hole Events
Potential Vorticity
Column Ozone
Interannual Variations
Atlantic Oscillation
Era-40 Reanalysis
Middle Latitudes
Astrofísica
Astronomía (Física)
Física atmosférica
2501 Ciencias de la Atmósfera
description © 2010 American Meteorological Society. This work has been partially supported by the MICINN (Spanish government) under Projects CGL2007-65891-C05-05/CLI (DB and JAG) and CGL2008-05939-C03-02/CLI (M. Anton). ERA-40 reanalysis data were provided by the ECMWF from their data server Web site (http://www.ecmwf.int/). MA thanks Junta de Extremadura-Consejeria de Infraestructuras y Desarrollo Tecnologico-and Fondo Social Europeo for concession of a postdoctoral grant. R. R. Garcia provided helpful comments on this manuscript. Two anonymous reviewers contributed to improving the final version of this paper. This paper analyzes the statistical relationship between the total ozone column (TOC) and atmospheric blocking using 40-yr European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-40) data for the 1978-98 period, with special emphasis on winter and the European and eastern Pacific sectors. Regional blocking occurrence is accompanied by a decrease of TOC within the anticyclonic circulation region and a distinctive ozone increase upstream and downstream (upstream and south) in the Pacific (European) sector. Blocking significantly enhances the likelihood of low TOC extremes, especially over the Scandinavian and the Alaska Peninsulas, where more than 50% of winter blocks lead to TOC values in the lowest tail of the distribution. The relationship between ozone miniholes and blocking is confined to the high latitudes of both basins and is strong in Europe, where about half of the ozone miniholes occur simultaneously with blocking. Blocking-related ozone miniholes (blocking ozone miniholes) are also among the most intense and persistent. Although blocking activity does not drive the interannual variability of regional ozone miniholes, blocking ozone miniholes account for up to two-thirds of the total observed trend of ozone miniholes in Europe. The polar vortex is proposed as a feasible candidate for explaining the enhanced coupling of blocking and ozone miniholes in Europe and its long-term ...
format Article in Journal/Newspaper
author Barriopedro Cepero, David
Antón Martínez, Manuel
García García, José Agustín
author_facet Barriopedro Cepero, David
Antón Martínez, Manuel
García García, José Agustín
author_sort Barriopedro Cepero, David
title Atmospheric blocking signatures in total ozone and ozone miniholes
title_short Atmospheric blocking signatures in total ozone and ozone miniholes
title_full Atmospheric blocking signatures in total ozone and ozone miniholes
title_fullStr Atmospheric blocking signatures in total ozone and ozone miniholes
title_full_unstemmed Atmospheric blocking signatures in total ozone and ozone miniholes
title_sort atmospheric blocking signatures in total ozone and ozone miniholes
publisher American Meteorological Society
publishDate 2010
url https://hdl.handle.net/20.500.14352/44116
https://doi.org/10.1175/2010JCLI3508.1
genre Arctic
Alaska
genre_facet Arctic
Alaska
op_relation CGL2007-65891-C05-05/CLI
CGL2008-05939-C03-02/CLI
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https://hdl.handle.net/20.500.14352/44116
0894-8755
doi:10.1175/2010JCLI3508.1
op_rights open access
op_doi https://doi.org/20.500.14352/4411610.1175/2010JCLI3508.110.1029/2002GL014935
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spelling ftunivcmadrid:oai:docta.ucm.es:20.500.14352/44116 2024-09-15T17:52:04+00:00 Atmospheric blocking signatures in total ozone and ozone miniholes Barriopedro Cepero, David Antón Martínez, Manuel García García, José Agustín 2010-07-15 application/pdf https://hdl.handle.net/20.500.14352/44116 https://doi.org/10.1175/2010JCLI3508.1 eng eng American Meteorological Society CGL2007-65891-C05-05/CLI CGL2008-05939-C03-02/CLI Allen, D. R., and N. Nakamura, 2002: Dynamical reconstruction of the record low column ozone over Europe on 30 November 1999. Geophys. Res. Lett., 29, 1362, doi:10.1029/2002GL014935. Altenhoff, A. M., O. Martius, M. Croci-Maspoli, C. Schwierz, and H. C. Davies, 2008: Linkage of atmospheric blocks and synopticscale Rossby waves: A climatological analysis. Tellus, 60A, 1053–1063. Antón, M., M. L. Cancillo, A. Serrano, J. M. Vaquero, and J. A. García, 2007: Ozone minihole over southwestern Spain during January 2004: Influence over ultraviolet radiation. Geophys. Res. Lett., 34, L10808, doi:10.1029/2007GL029689. ——, A. Serrano, M. L. Cancillo, and J. A. García, 2008: Total ozone and solar erythemal irradiance in southwestern Spain: Day-to-day variability and extreme episodes. Geophys. Res. Lett., 35, L20804, doi:10.1029/2008GL035290. Appenzeller, C., A. K. Weiss, and J. Staehelin, 2000: North Atlantic Oscillation modulates total ozone winter trends. Geophys. Res. Lett., 27, 1131–1134. Barriopedro,D.,R.Garcia Herrera, A. R. Lupo, and E.Hernández, 2006: A climatology of Northern Hemisphere blocking. J. Climate, 19, 1042–1063. ——, R. García Herrera, and R. M. Trigo, 2010: Application of blocking diagnosis methods to general circulation models. Part I. A novel detection scheme. Climate Dyn., in press, doi:10.1007/s00382-010-0767-5. Bojkov, R. D., and D. S. Balis, 2001: Characteristics of episodes with extremely low ozone values in the northern middle latitudes 1957–2000. Ann. Geophys., 19, 797–897. Brönnimann, S., and L. L. Hood, 2003: Frequency of low-ozone events over northwestern Europe in 1952–1963 and 1990–2000. Geophys. Res. Lett., 30, 2118, doi:10.1029/2003GL018431. Canziani, P. O., R. H. Compagnucci, and A. Bischoff, 2002:A study of impacts of tropospheric synoptic processes on the genesis and evolution of extreme total ozone anomalies over southern South America. J. Geophys. Res., 107, 4741, doi:10.1029/2001JD000965. Carslaw, K. S., and Coauthors, 1998: Increased stratospheric ozone depletion due to mountain-induced atmospheric waves. Nature, 391, 675–678. Croci-Maspoli, M., C. Schwierz, and H. C. Davies, 2007: Atmospheric blocking: Space–time links to the NAO and PNA. Climate Dyn., 29, 713–725. Dethof, A., and E. V. Hólm, 2004: Ozone assimilation in the ERA-40 reanalysis project. Quart. J. Roy. Meteor. Soc., 130, 2851–2872, doi:10.1256/qj.03.196. Dobson, G. M. B., D. N. Harrison, and J. Lawrence, 1929: Measurements of the amount of ozone in the earth’s atmosphere and its relation to other geophysical conditions: Part III. Proc. Roy. Soc. London, 122A, 456–486. Engelen, R. J., 1996: The effect of planetary waves on the total ozone deviations in the presence of a persistent blocking anticyclone system. J. Geophys. Res., 101 (D22), 28 775–28 784. Farman, J. C., B. G. Gardiner, and J. D. Shanklin, 1985: Large losses of total ozone in Antarctica reveal seasonal ClOx 5 NOx interaction. Nature, 315, 207–210. ——, A. O’Neill, and R. Swinbank, 1994: The dynamics of the arctic polar vortex during the EASOE campaign. Geophys. Res. Lett., 21, 1195–1198. Fusco, A. C., and M. L. Salby, 1999: Interannual variations of total ozone and their relationships to variations of planetary wave activity. J. Climate, 12, 1619–1629. Grewe, V., and M. Dameris, 1997: Heterogeneous PSC ozone loss during an ozone minihole. Geophys. Res. Lett., 24, 2503–2506. ——, ——, and R. Sausen, 1998: Impact of stratospheric dynamics and chemistry on Northern Hemisphere midlatitude ozone loss. J. Geophys. Res., 103, 25 417–25 433. Hadjinicolaou, P., and J. A. Pyle, 2004: The impact of Arctic ozone depletion on northern middle latitudes: Interannual variability and dynamical control. J. Atmos. Chem., 47, 25–43. Harris, N. R. P., and Coauthors, 2008: Ozone trends at northern mid- and high latitudes—A European perspective. Ann. Geophys., 26, 1207–1220. Hood, L.L., andB.E. Soukharev, 2005: Interannual variations of total ozone at northern midlatitudes correlated with stratospheric EP flux and potential vorticity. J. Atmos. Sci., 62, 3724–3740. ——, J. P. McCormack, and K. Labitzke, 1997: An investigation of dynamical contributions to midlatitude ozone trends in winter. J. Geophys. Res., 102, 13 079–13 093. ——, S. Rossi, and M. Beulen, 1999: Trends in lower stratospheric zonal winds, Rossby wave breaking behavior and column ozone at northern midlatitudes. J. Geophys. Res., 104, 24 321–24 339. ——, B. E. Soukharev, M. Fromm, and J. P. McCormack, 2001: Origin of extreme ozone minima at middle to high northern latitudes. J. Geophys. Res., 106, 20 925–20 940. Hudson, R. D., M. F. Andrade, M. B. Follette, and A. D. Frolov, 2006: The total ozone field separated into meteorological regimes—Part II: Northern Hemisphere mid-latitude total ozone trends. Atmos. Chem. Phys., 6, 5183–5191. Iwao, K., and T. Hirooka, 2006: Dynamical quantifications of ozone minihole formation in both hemispheres. J. Geophys. Res., 111, D02104, doi:10.1029/2005JD006333. James, P. M., 1998: A climatology of ozone miniholes over the Northern Hemisphere. Int. J. Climatol., 18, 1287–1303. ——, and D. Peters, 2002: The Lagrangian structure of ozone miniholes and potential vorticity anomalies in the Northern Hemisphere. Ann. Geophys., 20, 835–846. ——, ——, and D. W. Waugh, 2000: Very low ozone episodes due to polar vortex displacement. Tellus, 52B, 1123–1137. Keil, M., D. R. 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Res., 115, D06108, doi:10.1029/2009JD012742. https://hdl.handle.net/20.500.14352/44116 0894-8755 doi:10.1175/2010JCLI3508.1 open access 52 Northern-Hemisphere Blocking Polar Stratospheric Cloud Long-Term Changes Mini-Hole Events Potential Vorticity Column Ozone Interannual Variations Atlantic Oscillation Era-40 Reanalysis Middle Latitudes Astrofísica Astronomía (Física) Física atmosférica 2501 Ciencias de la Atmósfera journal article 2010 ftunivcmadrid https://doi.org/20.500.14352/4411610.1175/2010JCLI3508.110.1029/2002GL014935 2024-08-02T03:34:54Z © 2010 American Meteorological Society. This work has been partially supported by the MICINN (Spanish government) under Projects CGL2007-65891-C05-05/CLI (DB and JAG) and CGL2008-05939-C03-02/CLI (M. Anton). ERA-40 reanalysis data were provided by the ECMWF from their data server Web site (http://www.ecmwf.int/). MA thanks Junta de Extremadura-Consejeria de Infraestructuras y Desarrollo Tecnologico-and Fondo Social Europeo for concession of a postdoctoral grant. R. R. Garcia provided helpful comments on this manuscript. Two anonymous reviewers contributed to improving the final version of this paper. This paper analyzes the statistical relationship between the total ozone column (TOC) and atmospheric blocking using 40-yr European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-40) data for the 1978-98 period, with special emphasis on winter and the European and eastern Pacific sectors. Regional blocking occurrence is accompanied by a decrease of TOC within the anticyclonic circulation region and a distinctive ozone increase upstream and downstream (upstream and south) in the Pacific (European) sector. Blocking significantly enhances the likelihood of low TOC extremes, especially over the Scandinavian and the Alaska Peninsulas, where more than 50% of winter blocks lead to TOC values in the lowest tail of the distribution. The relationship between ozone miniholes and blocking is confined to the high latitudes of both basins and is strong in Europe, where about half of the ozone miniholes occur simultaneously with blocking. Blocking-related ozone miniholes (blocking ozone miniholes) are also among the most intense and persistent. Although blocking activity does not drive the interannual variability of regional ozone miniholes, blocking ozone miniholes account for up to two-thirds of the total observed trend of ozone miniholes in Europe. The polar vortex is proposed as a feasible candidate for explaining the enhanced coupling of blocking and ozone miniholes in Europe and its long-term ... Article in Journal/Newspaper Arctic Alaska Docta Complutense (Universidad Complutense de Madrid - UCM)

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