Changing features of the Northern Hemisphere 500-hPa circumpolar vortex

The tropospheric circumpolar vortex (CPV), an important signature of processes steering the general atmospheric circulation, surrounds each pole and is linked to the surface weather conditions. The CPV can be characterized by its area and circularity ratio (R(c)), which both vary temporally. This re...

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Published in:Frontiers in Big Data
Main Authors: Bushra, Nazla, Rohli, Robert V., Li, Chunyan, Miller, Paul W., Mostafiz, Rubayet Bin
Format: Text
Language:English
Published: Frontiers Media S.A. 2023
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9869373/
http://www.ncbi.nlm.nih.gov/pubmed/36700138
https://doi.org/10.3389/fdata.2022.1009158
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spelling ftpubmed:oai:pubmedcentral.nih.gov:9869373 2023-05-15T15:04:15+02:00 Changing features of the Northern Hemisphere 500-hPa circumpolar vortex Bushra, Nazla Rohli, Robert V. Li, Chunyan Miller, Paul W. Mostafiz, Rubayet Bin 2023-01-09 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9869373/ http://www.ncbi.nlm.nih.gov/pubmed/36700138 https://doi.org/10.3389/fdata.2022.1009158 en eng Frontiers Media S.A. http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9869373/ http://www.ncbi.nlm.nih.gov/pubmed/36700138 http://dx.doi.org/10.3389/fdata.2022.1009158 Copyright © 2023 Bushra, Rohli, Li, Miller and Mostafiz. https://creativecommons.org/licenses/by/4.0/This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms. CC-BY Front Big Data Big Data Text 2023 ftpubmed https://doi.org/10.3389/fdata.2022.1009158 2023-01-29T02:11:06Z The tropospheric circumpolar vortex (CPV), an important signature of processes steering the general atmospheric circulation, surrounds each pole and is linked to the surface weather conditions. The CPV can be characterized by its area and circularity ratio (R(c)), which both vary temporally. This research advances previous work identifying the daily 500-hPa Northern Hemispheric CPV (NHCPV) area, R(c), and temporal trends in its centroid by examining linear trends and periodic cycles in NHCPV area and R(c) (1979–2017). Results suggest that NHCPV area has increased linearly over time. However, a more representative signal of the planetary warming may be the temporally weakening gradient which has blurred NHCPV distinctiveness—perhaps a new indicator of Arctic amplification. R(c) displays opposing trends in subperiods and an insignificant overall trend. Distinct annual and semiannual cycles exist for area and R(c) over all subperiods. These features of NHCPV change over time may impact surface weather/climate. Text Arctic PubMed Central (PMC) Arctic Frontiers in Big Data 5
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Big Data
spellingShingle Big Data
Bushra, Nazla
Rohli, Robert V.
Li, Chunyan
Miller, Paul W.
Mostafiz, Rubayet Bin
Changing features of the Northern Hemisphere 500-hPa circumpolar vortex
topic_facet Big Data
description The tropospheric circumpolar vortex (CPV), an important signature of processes steering the general atmospheric circulation, surrounds each pole and is linked to the surface weather conditions. The CPV can be characterized by its area and circularity ratio (R(c)), which both vary temporally. This research advances previous work identifying the daily 500-hPa Northern Hemispheric CPV (NHCPV) area, R(c), and temporal trends in its centroid by examining linear trends and periodic cycles in NHCPV area and R(c) (1979–2017). Results suggest that NHCPV area has increased linearly over time. However, a more representative signal of the planetary warming may be the temporally weakening gradient which has blurred NHCPV distinctiveness—perhaps a new indicator of Arctic amplification. R(c) displays opposing trends in subperiods and an insignificant overall trend. Distinct annual and semiannual cycles exist for area and R(c) over all subperiods. These features of NHCPV change over time may impact surface weather/climate.
format Text
author Bushra, Nazla
Rohli, Robert V.
Li, Chunyan
Miller, Paul W.
Mostafiz, Rubayet Bin
author_facet Bushra, Nazla
Rohli, Robert V.
Li, Chunyan
Miller, Paul W.
Mostafiz, Rubayet Bin
author_sort Bushra, Nazla
title Changing features of the Northern Hemisphere 500-hPa circumpolar vortex
title_short Changing features of the Northern Hemisphere 500-hPa circumpolar vortex
title_full Changing features of the Northern Hemisphere 500-hPa circumpolar vortex
title_fullStr Changing features of the Northern Hemisphere 500-hPa circumpolar vortex
title_full_unstemmed Changing features of the Northern Hemisphere 500-hPa circumpolar vortex
title_sort changing features of the northern hemisphere 500-hpa circumpolar vortex
publisher Frontiers Media S.A.
publishDate 2023
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9869373/
http://www.ncbi.nlm.nih.gov/pubmed/36700138
https://doi.org/10.3389/fdata.2022.1009158
geographic Arctic
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genre Arctic
genre_facet Arctic
op_source Front Big Data
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9869373/
http://www.ncbi.nlm.nih.gov/pubmed/36700138
http://dx.doi.org/10.3389/fdata.2022.1009158
op_rights Copyright © 2023 Bushra, Rohli, Li, Miller and Mostafiz.
https://creativecommons.org/licenses/by/4.0/This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
op_rightsnorm CC-BY
op_doi https://doi.org/10.3389/fdata.2022.1009158
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