Triskeles and Symmetries of Mean Global Sea-Level Pressure

The evolution of mean sea-level atmospheric pressure since 1850 is analyzed using iterative singular spectrum analysis. Maps of the main components (the trends) reveal striking symmetries of order 3 and 4. The Northern Hemisphere (NH) displays a set of three positive features, forming an almost perf...

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Published in:Atmosphere
Main Authors: Fernando Lopes, Vincent Courtillot, Jean-Louis Le Mouël
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/atmos13091354
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spelling ftmdpi:oai:mdpi.com:/2073-4433/13/9/1354/ 2023-08-20T04:02:23+02:00 Triskeles and Symmetries of Mean Global Sea-Level Pressure Fernando Lopes Vincent Courtillot Jean-Louis Le Mouël agris 2022-08-25 application/pdf https://doi.org/10.3390/atmos13091354 EN eng Multidisciplinary Digital Publishing Institute Biosphere/Hydrosphere/Land–Atmosphere Interactions https://dx.doi.org/10.3390/atmos13091354 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 13; Issue 9; Pages: 1354 global sea-level pressure Taylor–Couette flow triskeles pattern Text 2022 ftmdpi https://doi.org/10.3390/atmos13091354 2023-08-01T06:12:34Z The evolution of mean sea-level atmospheric pressure since 1850 is analyzed using iterative singular spectrum analysis. Maps of the main components (the trends) reveal striking symmetries of order 3 and 4. The Northern Hemisphere (NH) displays a set of three positive features, forming an almost perfect equilateral triangle. The Southern Hemisphere (SH) displays a set of three positive features arranged as an isosceles triangle, with a possible fourth (weaker) feature. This geometry can be modeled as the Taylor–Couette flow of mode 3 (NH) or 4 (SH). The remarkable regularity and three-order symmetry of the NH triskeles occurs despite the lack of cylindrical symmetry of the northern continents. The stronger intensity and larger size of features in the SH is linked to the presence of the annular Antarctic Oscillation (AAO), which monitors the periodic reinforcement and weakening of the circumpolar vortex; it is a stationary mode. These components represent 70% of the variance in total pressure since 1850 and are stable in both time and space. In the remaining 30% of the variance, we have extracted quasi-periodical components with periods larger than 1 year (2% of the variance) and a harmonic sequence of the 1-year period (20% of the variance). Text Antarc* Antarctic MDPI Open Access Publishing Antarctic Atmosphere 13 9 1354
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic global sea-level pressure
Taylor–Couette flow
triskeles pattern
spellingShingle global sea-level pressure
Taylor–Couette flow
triskeles pattern
Fernando Lopes
Vincent Courtillot
Jean-Louis Le Mouël
Triskeles and Symmetries of Mean Global Sea-Level Pressure
topic_facet global sea-level pressure
Taylor–Couette flow
triskeles pattern
description The evolution of mean sea-level atmospheric pressure since 1850 is analyzed using iterative singular spectrum analysis. Maps of the main components (the trends) reveal striking symmetries of order 3 and 4. The Northern Hemisphere (NH) displays a set of three positive features, forming an almost perfect equilateral triangle. The Southern Hemisphere (SH) displays a set of three positive features arranged as an isosceles triangle, with a possible fourth (weaker) feature. This geometry can be modeled as the Taylor–Couette flow of mode 3 (NH) or 4 (SH). The remarkable regularity and three-order symmetry of the NH triskeles occurs despite the lack of cylindrical symmetry of the northern continents. The stronger intensity and larger size of features in the SH is linked to the presence of the annular Antarctic Oscillation (AAO), which monitors the periodic reinforcement and weakening of the circumpolar vortex; it is a stationary mode. These components represent 70% of the variance in total pressure since 1850 and are stable in both time and space. In the remaining 30% of the variance, we have extracted quasi-periodical components with periods larger than 1 year (2% of the variance) and a harmonic sequence of the 1-year period (20% of the variance).
format Text
author Fernando Lopes
Vincent Courtillot
Jean-Louis Le Mouël
author_facet Fernando Lopes
Vincent Courtillot
Jean-Louis Le Mouël
author_sort Fernando Lopes
title Triskeles and Symmetries of Mean Global Sea-Level Pressure
title_short Triskeles and Symmetries of Mean Global Sea-Level Pressure
title_full Triskeles and Symmetries of Mean Global Sea-Level Pressure
title_fullStr Triskeles and Symmetries of Mean Global Sea-Level Pressure
title_full_unstemmed Triskeles and Symmetries of Mean Global Sea-Level Pressure
title_sort triskeles and symmetries of mean global sea-level pressure
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/atmos13091354
op_coverage agris
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source Atmosphere; Volume 13; Issue 9; Pages: 1354
op_relation Biosphere/Hydrosphere/Land–Atmosphere Interactions
https://dx.doi.org/10.3390/atmos13091354
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos13091354
container_title Atmosphere
container_volume 13
container_issue 9
container_start_page 1354
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