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)...
Main Authors: | , , , , , |
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Format: | Conference Object |
Language: | English |
Published: |
2022
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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>. |
op_rights | cc_by |
publishDate | 2022 |
record_format | openpolar |
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/ |