Vertical coupling and transport in high-latitude ionosphere

Various ionospheric plasma anomalies appear at auroral latitudes, extending across the polar cap as a tongue of ionisation (TOI) and/or polar patches (PPs). Mechanisms responsible for horizontal and vertical plasma transport include the forcing from above (solar irradiance and geomagnetic activity)...

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Main Authors: Pokhotelov, Dimitry, Günzkofer, Florian Ludwig, Fernandez Gomez, Isabel, Sato, Hiroatsu, Borries, C., Jakowski, Norbert
Format: Conference Object
Language:English
Published: 2022
Subjects:
Online Access:https://elib.dlr.de/188184/
https://www.gfz-potsdam.de/sektion/weltraumphysik-und-weltraumwetter/
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author Pokhotelov, Dimitry
Günzkofer, Florian Ludwig
Fernandez Gomez, Isabel
Sato, Hiroatsu
Borries, C.
Jakowski, Norbert
author_facet Pokhotelov, Dimitry
Günzkofer, Florian Ludwig
Fernandez Gomez, Isabel
Sato, Hiroatsu
Borries, C.
Jakowski, Norbert
author_sort Pokhotelov, Dimitry
collection Unknown
description Various ionospheric plasma anomalies appear at auroral latitudes, extending across the polar cap as a tongue of ionisation (TOI) and/or polar patches (PPs). Mechanisms responsible for horizontal and vertical plasma transport include the forcing from above (solar irradiance and geomagnetic activity) and from below (atmospheric waves and tides). The forcing mechanisms balance each other in mesosphere/lower thermosphere, forming the ionospheric transition region. At higher altitudes (in the F layer), plasma irregularities can be transported for hours, while below (in the E layer) the irregularities recombine within seconds. Incoherent (ISR) and coherent scatter radars can observe vertical coupling and dynamics at various horizontal scales, providing a tool for analysing the transition region. Modelling with GCMs provides a basis for mitigating/forecasting the space weather. Vertical coupling and transport will be addressed in connection to the drifting polar cap anomalies (TOI and PPs). Examples of the vertical coupling and transport with the EISCAT ISR, coherent scatter radars, and GNSS receiver networks will show relative contributions of the forcing from above and below.
format Conference Object
genre EISCAT
genre_facet EISCAT
id ftdlr:oai:elib.dlr.de:188184
institution Open Polar
language English
op_collection_id ftdlr
op_doi https://doi.org/10.13140/RG.2.2.26242.76485
op_relation https://elib.dlr.de/188184/1/GFZ_Seminar_06-09-2022.pdf
Pokhotelov, Dimitry und Günzkofer, Florian Ludwig und Fernandez Gomez, Isabel und Sato, Hiroatsu und Borries, C. und Jakowski, Norbert (2022) Vertical coupling and transport in high-latitude ionosphere. GFZ seminar, Potsdam. doi:10.13140/RG.2.2.26242.76485 <https://doi.org/10.13140/RG.2.2.26242.76485>.
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spelling ftdlr:oai:elib.dlr.de:188184 2025-06-15T14:26:15+00:00 Vertical coupling and transport in high-latitude ionosphere Pokhotelov, Dimitry Günzkofer, Florian Ludwig Fernandez Gomez, Isabel Sato, Hiroatsu Borries, C. Jakowski, Norbert 2022-09-06 application/pdf https://elib.dlr.de/188184/ https://www.gfz-potsdam.de/sektion/weltraumphysik-und-weltraumwetter/ en eng https://elib.dlr.de/188184/1/GFZ_Seminar_06-09-2022.pdf Pokhotelov, Dimitry und Günzkofer, Florian Ludwig und Fernandez Gomez, Isabel und Sato, Hiroatsu und Borries, C. und Jakowski, Norbert (2022) Vertical coupling and transport in high-latitude ionosphere. GFZ seminar, Potsdam. doi:10.13140/RG.2.2.26242.76485 <https://doi.org/10.13140/RG.2.2.26242.76485>. cc_by Institut für Solar-Terrestrische Physik Konferenzbeitrag NonPeerReviewed 2022 ftdlr https://doi.org/10.13140/RG.2.2.26242.76485 2025-06-04T04:58:04Z Various ionospheric plasma anomalies appear at auroral latitudes, extending across the polar cap as a tongue of ionisation (TOI) and/or polar patches (PPs). Mechanisms responsible for horizontal and vertical plasma transport include the forcing from above (solar irradiance and geomagnetic activity) and from below (atmospheric waves and tides). The forcing mechanisms balance each other in mesosphere/lower thermosphere, forming the ionospheric transition region. At higher altitudes (in the F layer), plasma irregularities can be transported for hours, while below (in the E layer) the irregularities recombine within seconds. Incoherent (ISR) and coherent scatter radars can observe vertical coupling and dynamics at various horizontal scales, providing a tool for analysing the transition region. Modelling with GCMs provides a basis for mitigating/forecasting the space weather. Vertical coupling and transport will be addressed in connection to the drifting polar cap anomalies (TOI and PPs). Examples of the vertical coupling and transport with the EISCAT ISR, coherent scatter radars, and GNSS receiver networks will show relative contributions of the forcing from above and below. Conference Object EISCAT Unknown
spellingShingle Institut für Solar-Terrestrische Physik
Pokhotelov, Dimitry
Günzkofer, Florian Ludwig
Fernandez Gomez, Isabel
Sato, Hiroatsu
Borries, C.
Jakowski, Norbert
Vertical coupling and transport in high-latitude ionosphere
title Vertical coupling and transport in high-latitude ionosphere
title_full Vertical coupling and transport in high-latitude ionosphere
title_fullStr Vertical coupling and transport in high-latitude ionosphere
title_full_unstemmed Vertical coupling and transport in high-latitude ionosphere
title_short Vertical coupling and transport in high-latitude ionosphere
title_sort vertical coupling and transport in high-latitude ionosphere
topic Institut für Solar-Terrestrische Physik
topic_facet Institut für Solar-Terrestrische Physik
url https://elib.dlr.de/188184/
https://www.gfz-potsdam.de/sektion/weltraumphysik-und-weltraumwetter/