First detection of a brief mesoscale elevated stratopause in very early winter
Elevated stratopauses are typically associated with prolonged disturbed conditions in the Northern Hemisphere polar winter. The Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) and the Microwave Limb Sounder (MLS) observed a short-lived and highly zonally asymmetric stratopause at m...
Published in: | Geophysical Research Letters |
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American Geophysical Union
2020
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Online Access: | http://hdl.handle.net/10261/205312 https://doi.org/10.1029/2019GL086751 https://doi.org/10.13039/501100000780 |
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ftcsic:oai:digital.csic.es:10261/205312 2024-02-11T10:01:34+01:00 First detection of a brief mesoscale elevated stratopause in very early winter García Comas, Maia Funke, Bernd López-Puertas, Manuel González-Galindo, F. Hoepfner, M. Ministerio de Ciencia, Innovación y Universidades (España) European Commission 2020 http://hdl.handle.net/10261/205312 https://doi.org/10.1029/2019GL086751 https://doi.org/10.13039/501100000780 unknown American Geophysical Union #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/SEV-2017-0709 info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/ESP2017-87143-R Publisher's version http://dx.doi.org/10.1029/2019GL086751 Sí doi:10.1029/2019GL086751 issn: 1944-8007 Geophysical Research Letters 47(4): Ae2019GL086 (2020) http://hdl.handle.net/10261/205312 http://dx.doi.org/10.13039/501100000780 open artículo http://purl.org/coar/resource_type/c_6501 2020 ftcsic https://doi.org/10.1029/2019GL08675110.13039/501100000780 2024-01-16T10:50:49Z Elevated stratopauses are typically associated with prolonged disturbed conditions in the Northern Hemisphere polar winter. The Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) and the Microwave Limb Sounder (MLS) observed a short-lived and highly zonally asymmetric stratopause at mesospheric altitudes in November 2009, the earliest in the season reported so far. The Arctic climatological winter stratopause vanished, and MIPAS and MLS measured temperatures of 260 K at 82 km and 250 K at 75 km, respectively, in a region smaller than in typical midwinter elevated stratopause events. Planetary wave activity was initially high. Zonal mean zonal winds and the poleward temperature gradient northward of 70°N stayed reversed during 7 days, but the mesosphere did not cool. Wave activity dropped until the eastward stratospheric winds resumed and a strong vortex restored in the mesosphere. The stratopause emerged at high altitudes, staying there for 2–5 days. It was accompanied by enhanced downward transport. It took the stratopause 9 days to move down to its typical winter altitudes. ©2020. American Geophysical Union. All Rights Reserved. The IAA team acknowledges financial support from the State Agency for Research of the Spanish MCIU through Project ESP2017?87143-R, the ?Center of Excellence Severo Ochoa? award to the IAA-CSIC (SEV-2017-0709), and EC FEDER funds. MIPAS data sets can be accessed upon request online (https://www.imk-asf.kit.edu/english/308.php). We thank the Global Modeling and Assimilation Office for providing MERRA-2 data and the MLS science and data processing teams for providing MLS data publicly through the NASA Goddard Space Flight Center Earth Sciences (GES) Data and Information Services Center. Article in Journal/Newspaper Arctic Digital.CSIC (Spanish National Research Council) Arctic Merra ENVELOPE(12.615,12.615,65.816,65.816) Midwinter ENVELOPE(139.931,139.931,-66.690,-66.690) Geophysical Research Letters 47 4 |
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Open Polar |
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Digital.CSIC (Spanish National Research Council) |
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ftcsic |
language |
unknown |
description |
Elevated stratopauses are typically associated with prolonged disturbed conditions in the Northern Hemisphere polar winter. The Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) and the Microwave Limb Sounder (MLS) observed a short-lived and highly zonally asymmetric stratopause at mesospheric altitudes in November 2009, the earliest in the season reported so far. The Arctic climatological winter stratopause vanished, and MIPAS and MLS measured temperatures of 260 K at 82 km and 250 K at 75 km, respectively, in a region smaller than in typical midwinter elevated stratopause events. Planetary wave activity was initially high. Zonal mean zonal winds and the poleward temperature gradient northward of 70°N stayed reversed during 7 days, but the mesosphere did not cool. Wave activity dropped until the eastward stratospheric winds resumed and a strong vortex restored in the mesosphere. The stratopause emerged at high altitudes, staying there for 2–5 days. It was accompanied by enhanced downward transport. It took the stratopause 9 days to move down to its typical winter altitudes. ©2020. American Geophysical Union. All Rights Reserved. The IAA team acknowledges financial support from the State Agency for Research of the Spanish MCIU through Project ESP2017?87143-R, the ?Center of Excellence Severo Ochoa? award to the IAA-CSIC (SEV-2017-0709), and EC FEDER funds. MIPAS data sets can be accessed upon request online (https://www.imk-asf.kit.edu/english/308.php). We thank the Global Modeling and Assimilation Office for providing MERRA-2 data and the MLS science and data processing teams for providing MLS data publicly through the NASA Goddard Space Flight Center Earth Sciences (GES) Data and Information Services Center. |
author2 |
Ministerio de Ciencia, Innovación y Universidades (España) European Commission |
format |
Article in Journal/Newspaper |
author |
García Comas, Maia Funke, Bernd López-Puertas, Manuel González-Galindo, F. Hoepfner, M. |
spellingShingle |
García Comas, Maia Funke, Bernd López-Puertas, Manuel González-Galindo, F. Hoepfner, M. First detection of a brief mesoscale elevated stratopause in very early winter |
author_facet |
García Comas, Maia Funke, Bernd López-Puertas, Manuel González-Galindo, F. Hoepfner, M. |
author_sort |
García Comas, Maia |
title |
First detection of a brief mesoscale elevated stratopause in very early winter |
title_short |
First detection of a brief mesoscale elevated stratopause in very early winter |
title_full |
First detection of a brief mesoscale elevated stratopause in very early winter |
title_fullStr |
First detection of a brief mesoscale elevated stratopause in very early winter |
title_full_unstemmed |
First detection of a brief mesoscale elevated stratopause in very early winter |
title_sort |
first detection of a brief mesoscale elevated stratopause in very early winter |
publisher |
American Geophysical Union |
publishDate |
2020 |
url |
http://hdl.handle.net/10261/205312 https://doi.org/10.1029/2019GL086751 https://doi.org/10.13039/501100000780 |
long_lat |
ENVELOPE(12.615,12.615,65.816,65.816) ENVELOPE(139.931,139.931,-66.690,-66.690) |
geographic |
Arctic Merra Midwinter |
geographic_facet |
Arctic Merra Midwinter |
genre |
Arctic |
genre_facet |
Arctic |
op_relation |
#PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/SEV-2017-0709 info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/ESP2017-87143-R Publisher's version http://dx.doi.org/10.1029/2019GL086751 Sí doi:10.1029/2019GL086751 issn: 1944-8007 Geophysical Research Letters 47(4): Ae2019GL086 (2020) http://hdl.handle.net/10261/205312 http://dx.doi.org/10.13039/501100000780 |
op_rights |
open |
op_doi |
https://doi.org/10.1029/2019GL08675110.13039/501100000780 |
container_title |
Geophysical Research Letters |
container_volume |
47 |
container_issue |
4 |
_version_ |
1790597357744685056 |