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...
Published in: | Journal of the Atmospheric Sciences |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Meteorological Society
2010
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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 |
id | ftdlr:oai:elib.dlr.de:65914 |
institution | Open Polar |
language | English |
op_collection_id | ftdlr |
op_container_end_page | 4016 |
op_doi | https://doi.org/10.1175/2010JAS3532.1 |
op_relation | 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>. |
publishDate | 2010 |
publisher | American Meteorological Society |
record_format | openpolar |
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 |