The day-to-day effects of strong geomagnetic disturbances on the North Atlantic Oscillation in the winter periods of years 1951-2003

The day-to-day effects of the strong geomagnetic disturbances on geopotential heights (GPH) in the winter lower atmosphere were described in many papers in the beginning of 1970s. These works focused on the North-East Pacific, while the North Atlantic was until now omitted. Our aim is therefore to i...

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Published in:Studia Geophysica et Geodaetica
Main Authors: Bochníček, Josef, Šimkanin, Ján, Hejda, Pavel, Huth, Radan
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:https://kramerius.lib.cas.cz/view/uuid:5ffa3e1c-1f3f-4c92-bdd6-040f15fbe39c
https://doi.org/10.1007/s11200-018-0488-5
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author Bochníček, Josef
Šimkanin, Ján
Hejda, Pavel
Huth, Radan
author_facet Bochníček, Josef
Šimkanin, Ján
Hejda, Pavel
Huth, Radan
author_sort Bochníček, Josef
collection Czech Academy of Sciences: dKNAV
container_issue 3
container_start_page 455
container_title Studia Geophysica et Geodaetica
container_volume 63
description The day-to-day effects of the strong geomagnetic disturbances on geopotential heights (GPH) in the winter lower atmosphere were described in many papers in the beginning of 1970s. These works focused on the North-East Pacific, while the North Atlantic was until now omitted. Our aim is therefore to investigate the possible effect of strong geomagnetic disturbances on the lower atmosphere GPH changes over the winter North Atlantic on the day-to-day time scale, represented by the daily index of the North Atlantic Oscillation (NAO). The investigated intervals are winter periods (December-March) of 1951–2003. The daily NAO average values in 3-day intervals before and after the disturbance onsets are compared. The graphs of NAO differences are complemented by the maps of GPH differences. The NAO response to geomagnetic disturbance, as registered on the day-to-day time scale, also shows a change in its behaviour around the year 1970. This response reaches its highest values in the years 1951–1969, usually 2–5 days following the onset of geomagnetic disturbances. Intensity of the response depends on the disturbance intensity (the largest differences were associated with extremely strong disturbances).
format Article in Journal/Newspaper
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
geographic Pacific
geographic_facet Pacific
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spelling ftczechacademysc:oai:kramerius.lib.cas.cz:uuid:5ffa3e1c-1f3f-4c92-bdd6-040f15fbe39c 2025-01-16T23:30:55+00:00 The day-to-day effects of strong geomagnetic disturbances on the North Atlantic Oscillation in the winter periods of years 1951-2003 Bochníček, Josef Šimkanin, Ján Hejda, Pavel Huth, Radan 455-464 média svazek https://kramerius.lib.cas.cz/view/uuid:5ffa3e1c-1f3f-4c92-bdd6-040f15fbe39c https://doi.org/10.1007/s11200-018-0488-5 unknown https://kramerius.lib.cas.cz/view/uuid:5ffa3e1c-1f3f-4c92-bdd6-040f15fbe39c doi:10.1007/s11200-018-0488-5 policy:private geomagnetic disturbances North Atlantic Oscillation lower stratosphere-troposphere global atmospheric electrical circuit model:article ftczechacademysc https://doi.org/10.1007/s11200-018-0488-5 2024-02-19T22:57:32Z The day-to-day effects of the strong geomagnetic disturbances on geopotential heights (GPH) in the winter lower atmosphere were described in many papers in the beginning of 1970s. These works focused on the North-East Pacific, while the North Atlantic was until now omitted. Our aim is therefore to investigate the possible effect of strong geomagnetic disturbances on the lower atmosphere GPH changes over the winter North Atlantic on the day-to-day time scale, represented by the daily index of the North Atlantic Oscillation (NAO). The investigated intervals are winter periods (December-March) of 1951–2003. The daily NAO average values in 3-day intervals before and after the disturbance onsets are compared. The graphs of NAO differences are complemented by the maps of GPH differences. The NAO response to geomagnetic disturbance, as registered on the day-to-day time scale, also shows a change in its behaviour around the year 1970. This response reaches its highest values in the years 1951–1969, usually 2–5 days following the onset of geomagnetic disturbances. Intensity of the response depends on the disturbance intensity (the largest differences were associated with extremely strong disturbances). Article in Journal/Newspaper North Atlantic North Atlantic oscillation Czech Academy of Sciences: dKNAV Pacific Studia Geophysica et Geodaetica 63 3 455 464
spellingShingle geomagnetic disturbances
North Atlantic Oscillation
lower stratosphere-troposphere
global atmospheric electrical circuit
Bochníček, Josef
Šimkanin, Ján
Hejda, Pavel
Huth, Radan
The day-to-day effects of strong geomagnetic disturbances on the North Atlantic Oscillation in the winter periods of years 1951-2003
title The day-to-day effects of strong geomagnetic disturbances on the North Atlantic Oscillation in the winter periods of years 1951-2003
title_full The day-to-day effects of strong geomagnetic disturbances on the North Atlantic Oscillation in the winter periods of years 1951-2003
title_fullStr The day-to-day effects of strong geomagnetic disturbances on the North Atlantic Oscillation in the winter periods of years 1951-2003
title_full_unstemmed The day-to-day effects of strong geomagnetic disturbances on the North Atlantic Oscillation in the winter periods of years 1951-2003
title_short The day-to-day effects of strong geomagnetic disturbances on the North Atlantic Oscillation in the winter periods of years 1951-2003
title_sort day-to-day effects of strong geomagnetic disturbances on the north atlantic oscillation in the winter periods of years 1951-2003
topic geomagnetic disturbances
North Atlantic Oscillation
lower stratosphere-troposphere
global atmospheric electrical circuit
topic_facet geomagnetic disturbances
North Atlantic Oscillation
lower stratosphere-troposphere
global atmospheric electrical circuit
url https://kramerius.lib.cas.cz/view/uuid:5ffa3e1c-1f3f-4c92-bdd6-040f15fbe39c
https://doi.org/10.1007/s11200-018-0488-5