Potential temperature inversion: Complementary approaches

Given the distribution of one atmospheric variable, that of nearly all others can be derived in balanced flow. In particular, potential vorticity inversion (PVI) selects PV to derive pressure, winds and potential temperature θ. Potential temperature inversion (θI) starts from available θ-fields to d...

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Published in:Journal of the Atmospheric Sciences
Main Authors: Egger, Joseph, Hoinka, Klaus-Peter
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2010
Subjects:
Online Access:https://elib.dlr.de/65914/
https://elib.dlr.de/65914/1/2010JAS3532.pdf
http://journals.ametsoc.org/doi/abs/10.1175/2010JAS3532.1
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author Egger, Joseph
Hoinka, Klaus-Peter
author_facet Egger, Joseph
Hoinka, Klaus-Peter
author_sort Egger, Joseph
collection Unknown
container_issue 12
container_start_page 4001
container_title Journal of the Atmospheric Sciences
container_volume 67
description Given the distribution of one atmospheric variable, that of nearly all others can be derived in balanced flow. In particular, potential vorticity inversion (PVI) selects PV to derive pressure, winds and potential temperature θ. Potential temperature inversion (θI) starts from available θ-fields to derive pressure, winds and PV. While PVI has been applied extensively, θI has hardly been used as a research tool although the related technical steps are well known and simpler than those needed in PVI. Two idealized examples of θI and PVI are compared. ERA analyses are used to determine typical anomalies of PV and of θ in the North Atlantic stormtrack region. Statistical forms of PVI and θI are applied to these anomalies. The inversions are equivalent but the results of θI are generally easier to understand than those of PVI. The issues of attribution and piecewise inversion are discussed.
format Article in Journal/Newspaper
genre North Atlantic
genre_facet North Atlantic
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op_doi https://doi.org/10.1175/2010JAS3532.1
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Egger, Joseph und Hoinka, Klaus-Peter (2010) Potential temperature inversion: Complementary approaches. Journal of the Atmospheric Sciences, 67, Seiten 4001-4016. American Meteorological Society. doi:10.1175/2010JAS3532.1 <https://doi.org/10.1175/2010JAS3532.1>.
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spelling ftdlr:oai:elib.dlr.de:65914 2025-06-15T14:43:04+00:00 Potential temperature inversion: Complementary approaches Egger, Joseph Hoinka, Klaus-Peter 2010 application/pdf https://elib.dlr.de/65914/ https://elib.dlr.de/65914/1/2010JAS3532.pdf http://journals.ametsoc.org/doi/abs/10.1175/2010JAS3532.1 en eng American Meteorological Society https://elib.dlr.de/65914/1/2010JAS3532.pdf Egger, Joseph und Hoinka, Klaus-Peter (2010) Potential temperature inversion: Complementary approaches. Journal of the Atmospheric Sciences, 67, Seiten 4001-4016. American Meteorological Society. doi:10.1175/2010JAS3532.1 <https://doi.org/10.1175/2010JAS3532.1>. Wolkenphysik und Verkehrsmeteorologie Zeitschriftenbeitrag PeerReviewed 2010 ftdlr https://doi.org/10.1175/2010JAS3532.1 2025-06-04T04:58:08Z Given the distribution of one atmospheric variable, that of nearly all others can be derived in balanced flow. In particular, potential vorticity inversion (PVI) selects PV to derive pressure, winds and potential temperature θ. Potential temperature inversion (θI) starts from available θ-fields to derive pressure, winds and PV. While PVI has been applied extensively, θI has hardly been used as a research tool although the related technical steps are well known and simpler than those needed in PVI. Two idealized examples of θI and PVI are compared. ERA analyses are used to determine typical anomalies of PV and of θ in the North Atlantic stormtrack region. Statistical forms of PVI and θI are applied to these anomalies. The inversions are equivalent but the results of θI are generally easier to understand than those of PVI. The issues of attribution and piecewise inversion are discussed. Article in Journal/Newspaper North Atlantic Unknown Journal of the Atmospheric Sciences 67 12 4001 4016
spellingShingle Wolkenphysik und Verkehrsmeteorologie
Egger, Joseph
Hoinka, Klaus-Peter
Potential temperature inversion: Complementary approaches
title Potential temperature inversion: Complementary approaches
title_full Potential temperature inversion: Complementary approaches
title_fullStr Potential temperature inversion: Complementary approaches
title_full_unstemmed Potential temperature inversion: Complementary approaches
title_short Potential temperature inversion: Complementary approaches
title_sort potential temperature inversion: complementary approaches
topic Wolkenphysik und Verkehrsmeteorologie
topic_facet Wolkenphysik und Verkehrsmeteorologie
url https://elib.dlr.de/65914/
https://elib.dlr.de/65914/1/2010JAS3532.pdf
http://journals.ametsoc.org/doi/abs/10.1175/2010JAS3532.1