Tropopause height at 78°N 16°E: average seasonal variation 2007-2010

We present a seasonal climatology of tropopause altitude for 78° N 16° E derived from observations 2007–2010 by the SOUSY VHF radar on Svalbard. The spring minimum occurs one month later than that of surface air temperature and instead coincides with the maximum in ozone column density. This confirm...

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Main Authors: Hall, Chris, Hansen, Georg, Sigernes, Fred, Kuyeng, Karim
Format: Article in Journal/Newspaper
Language:English
Published: European Geophysical Society 2011
Subjects:
Online Access:https://hdl.handle.net/10037/3938
https://doi.org/10.5194/acpd-11-39-2011
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author Hall, Chris
Hansen, Georg
Sigernes, Fred
Kuyeng, Karim
author_facet Hall, Chris
Hansen, Georg
Sigernes, Fred
Kuyeng, Karim
author_sort Hall, Chris
collection University of Tromsø: Munin Open Research Archive
description We present a seasonal climatology of tropopause altitude for 78° N 16° E derived from observations 2007–2010 by the SOUSY VHF radar on Svalbard. The spring minimum occurs one month later than that of surface air temperature and instead coincides with the maximum in ozone column density. This confirms similar studies based on radiosonde measurements in the arctic and demonstrates downward control by the stratosphere. If one is to exploit the potential of tropopause height as a metric for climate change at high latitude and elsewhere, it is imperative to observe and understand the processes which establish the tropopause – an understanding to which this study contributes.
format Article in Journal/Newspaper
genre Arctic
Climate change
Svalbard
genre_facet Arctic
Climate change
Svalbard
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
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language English
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op_doi https://doi.org/10.5194/acpd-11-39-2011
op_relation FRIDAID 521617
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op_rights openAccess
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publisher European Geophysical Society
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spelling ftunivtroemsoe:oai:munin.uit.no:10037/3938 2025-04-13T14:14:20+00:00 Tropopause height at 78°N 16°E: average seasonal variation 2007-2010 Hall, Chris Hansen, Georg Sigernes, Fred Kuyeng, Karim 2011 https://hdl.handle.net/10037/3938 https://doi.org/10.5194/acpd-11-39-2011 eng eng European Geophysical Society FRIDAID 521617 https://hdl.handle.net/10037/3938 openAccess VDP::Mathematics and natural science: 400::Geosciences: 450::Meteorology: 453 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Meteorologi: 453 Journal article Tidsskriftartikkel Peer reviewed 2011 ftunivtroemsoe https://doi.org/10.5194/acpd-11-39-2011 2025-03-14T05:17:55Z We present a seasonal climatology of tropopause altitude for 78° N 16° E derived from observations 2007–2010 by the SOUSY VHF radar on Svalbard. The spring minimum occurs one month later than that of surface air temperature and instead coincides with the maximum in ozone column density. This confirms similar studies based on radiosonde measurements in the arctic and demonstrates downward control by the stratosphere. If one is to exploit the potential of tropopause height as a metric for climate change at high latitude and elsewhere, it is imperative to observe and understand the processes which establish the tropopause – an understanding to which this study contributes. Article in Journal/Newspaper Arctic Climate change Svalbard University of Tromsø: Munin Open Research Archive Arctic Svalbard
spellingShingle VDP::Mathematics and natural science: 400::Geosciences: 450::Meteorology: 453
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Meteorologi: 453
Hall, Chris
Hansen, Georg
Sigernes, Fred
Kuyeng, Karim
Tropopause height at 78°N 16°E: average seasonal variation 2007-2010
title Tropopause height at 78°N 16°E: average seasonal variation 2007-2010
title_full Tropopause height at 78°N 16°E: average seasonal variation 2007-2010
title_fullStr Tropopause height at 78°N 16°E: average seasonal variation 2007-2010
title_full_unstemmed Tropopause height at 78°N 16°E: average seasonal variation 2007-2010
title_short Tropopause height at 78°N 16°E: average seasonal variation 2007-2010
title_sort tropopause height at 78°n 16°e: average seasonal variation 2007-2010
topic VDP::Mathematics and natural science: 400::Geosciences: 450::Meteorology: 453
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Meteorologi: 453
topic_facet VDP::Mathematics and natural science: 400::Geosciences: 450::Meteorology: 453
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Meteorologi: 453
url https://hdl.handle.net/10037/3938
https://doi.org/10.5194/acpd-11-39-2011