Cold surge episodes over southeastern Brazil - a potential vorticity perspective

Most intense cold surges and associated frost events in southern and southeastern Brazil are characterized by a large amplitude trough over South America extending toward tropical latitudes and a ridge to the west of it over the Pacific Ocean. In this study, potential vorticity (PV) streamers serve...

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Main Authors: Arnold, Julian, Sprenger, Michael, Martius, Olivia
Format: Text
Language:English
Published: Wiley 2013
Subjects:
Online Access:https://dx.doi.org/10.7892/boris.39674
http://boris.unibe.ch/39674/
id ftdatacite:10.7892/boris.39674
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spelling ftdatacite:10.7892/boris.39674 2023-05-15T13:59:40+02:00 Cold surge episodes over southeastern Brazil - a potential vorticity perspective Arnold, Julian Sprenger, Michael Martius, Olivia 2013 application/pdf https://dx.doi.org/10.7892/boris.39674 http://boris.unibe.ch/39674/ en eng Wiley info:eu-repo/semantics/openAccess 550 Earth sciences & geology 910 Geography & travel Text article-journal ScholarlyArticle 2013 ftdatacite https://doi.org/10.7892/boris.39674 2021-11-05T12:55:41Z Most intense cold surges and associated frost events in southern and southeastern Brazil are characterized by a large amplitude trough over South America extending toward tropical latitudes and a ridge to the west of it over the Pacific Ocean. In this study, potential vorticity (PV) streamers serve to examine the flow condition leading to cold surges. Case studies suggest that several PV anomalies are related to cold surge episodes: (1) the potential vorticity unit (2-PVU) isoline upstream of South America becomes progressively more distorted prior and during the cold surge episode, indicating a flow situation which is conducive for Rossby wave breaking and hence a flow which strongly deviates from zonality; (2) the initial stage of a cold surge episode is characterized by a northward bulging of high-PV air to the east of the Andes, resulting in a PV streamer whose northern end reaches Uruguay and southeastern Brazil; the strong PV gradient on its western flank constitutes a flow configuration that induces and maintains the transport of sub-Antarctic air toward the subtropics; (3) a distinct negative PV anomaly, a blocking, originates over the eastern South Pacific, upstream of the South America sector. A composite analysis of 27 cold surges is performed for stratospheric PV streamer frequency on several isentropic surfaces. It reveals that equatorward wave breaking over South America and the western South Atlantic represents an important potential component of the dynamics of intense cold surges. The indications are most pronounced around the isentropic levels of 320 K and immediately before the day with largest temperature drops over subtropical Brazil. Text Antarc* Antarctic DataCite Metadata Store (German National Library of Science and Technology) Antarctic Pacific Uruguay
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic 550 Earth sciences & geology
910 Geography & travel
spellingShingle 550 Earth sciences & geology
910 Geography & travel
Arnold, Julian
Sprenger, Michael
Martius, Olivia
Cold surge episodes over southeastern Brazil - a potential vorticity perspective
topic_facet 550 Earth sciences & geology
910 Geography & travel
description Most intense cold surges and associated frost events in southern and southeastern Brazil are characterized by a large amplitude trough over South America extending toward tropical latitudes and a ridge to the west of it over the Pacific Ocean. In this study, potential vorticity (PV) streamers serve to examine the flow condition leading to cold surges. Case studies suggest that several PV anomalies are related to cold surge episodes: (1) the potential vorticity unit (2-PVU) isoline upstream of South America becomes progressively more distorted prior and during the cold surge episode, indicating a flow situation which is conducive for Rossby wave breaking and hence a flow which strongly deviates from zonality; (2) the initial stage of a cold surge episode is characterized by a northward bulging of high-PV air to the east of the Andes, resulting in a PV streamer whose northern end reaches Uruguay and southeastern Brazil; the strong PV gradient on its western flank constitutes a flow configuration that induces and maintains the transport of sub-Antarctic air toward the subtropics; (3) a distinct negative PV anomaly, a blocking, originates over the eastern South Pacific, upstream of the South America sector. A composite analysis of 27 cold surges is performed for stratospheric PV streamer frequency on several isentropic surfaces. It reveals that equatorward wave breaking over South America and the western South Atlantic represents an important potential component of the dynamics of intense cold surges. The indications are most pronounced around the isentropic levels of 320 K and immediately before the day with largest temperature drops over subtropical Brazil.
format Text
author Arnold, Julian
Sprenger, Michael
Martius, Olivia
author_facet Arnold, Julian
Sprenger, Michael
Martius, Olivia
author_sort Arnold, Julian
title Cold surge episodes over southeastern Brazil - a potential vorticity perspective
title_short Cold surge episodes over southeastern Brazil - a potential vorticity perspective
title_full Cold surge episodes over southeastern Brazil - a potential vorticity perspective
title_fullStr Cold surge episodes over southeastern Brazil - a potential vorticity perspective
title_full_unstemmed Cold surge episodes over southeastern Brazil - a potential vorticity perspective
title_sort cold surge episodes over southeastern brazil - a potential vorticity perspective
publisher Wiley
publishDate 2013
url https://dx.doi.org/10.7892/boris.39674
http://boris.unibe.ch/39674/
geographic Antarctic
Pacific
Uruguay
geographic_facet Antarctic
Pacific
Uruguay
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.7892/boris.39674
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