Vertical coupling and transport in high-latitude ionosphere
Various plasma anomalies appear at auroral latitudes, extending across the polar cap as a tongue of ionisation (TOI) and polar patches (PPs). Mechanisms responsible for horizontal and vertical plasma transport include the forcing from above (solar irradiance and geomagnetic activity) and from below...
Main Authors: | , , , , |
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Format: | Conference Object |
Language: | English |
Published: |
2022
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Online Access: | https://elib.dlr.de/188787/ https://elib.dlr.de/188787/1/image2022_Pokhotelov.pdf https://space.fmi.fi/image/www/image_meeting_2022/ |
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author | Pokhotelov, Dimitry Günzkofer, Florian Ludwig Stober, Gunter Fernandez Gomez, Isabel Borries, C. |
author_facet | Pokhotelov, Dimitry Günzkofer, Florian Ludwig Stober, Gunter Fernandez Gomez, Isabel Borries, C. |
author_sort | Pokhotelov, Dimitry |
collection | Unknown |
description | Various plasma anomalies appear at auroral latitudes, extending across the polar cap as a tongue of ionisation (TOI) and 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 lower thermosphere, forming the ionospheric transition region. At higher altitudes (the F layer), plasma irregularities can be transported for hours, while in the E layer and below 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 will show relative contributions of the forcing from above and below. Examples of plasma irregularities seen by GNSS receiver networks and SAR radars will be also shown. |
format | Conference Object |
genre | EISCAT |
genre_facet | EISCAT |
id | ftdlr:oai:elib.dlr.de:188787 |
institution | Open Polar |
language | English |
op_collection_id | ftdlr |
op_doi | https://doi.org/10.13140/RG.2.2.22851.89128 |
op_relation | https://elib.dlr.de/188787/1/image2022_Pokhotelov.pdf Pokhotelov, Dimitry und Günzkofer, Florian Ludwig und Stober, Gunter und Fernandez Gomez, Isabel und Borries, C. (2022) Vertical coupling and transport in high-latitude ionosphere. 16th IMAGE Meeting, Helsinki, Finland. doi:10.13140/RG.2.2.22851.89128 <https://doi.org/10.13140/RG.2.2.22851.89128>. |
op_rights | cc_by |
publishDate | 2022 |
record_format | openpolar |
spelling | ftdlr:oai:elib.dlr.de:188787 2025-06-15T14:26:15+00:00 Vertical coupling and transport in high-latitude ionosphere Pokhotelov, Dimitry Günzkofer, Florian Ludwig Stober, Gunter Fernandez Gomez, Isabel Borries, C. 2022-10-06 application/pdf https://elib.dlr.de/188787/ https://elib.dlr.de/188787/1/image2022_Pokhotelov.pdf https://space.fmi.fi/image/www/image_meeting_2022/ en eng https://elib.dlr.de/188787/1/image2022_Pokhotelov.pdf Pokhotelov, Dimitry und Günzkofer, Florian Ludwig und Stober, Gunter und Fernandez Gomez, Isabel und Borries, C. (2022) Vertical coupling and transport in high-latitude ionosphere. 16th IMAGE Meeting, Helsinki, Finland. doi:10.13140/RG.2.2.22851.89128 <https://doi.org/10.13140/RG.2.2.22851.89128>. cc_by Institut für Solar-Terrestrische Physik Konferenzbeitrag NonPeerReviewed 2022 ftdlr https://doi.org/10.13140/RG.2.2.22851.89128 2025-06-04T04:58:08Z Various plasma anomalies appear at auroral latitudes, extending across the polar cap as a tongue of ionisation (TOI) and 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 lower thermosphere, forming the ionospheric transition region. At higher altitudes (the F layer), plasma irregularities can be transported for hours, while in the E layer and below 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 will show relative contributions of the forcing from above and below. Examples of plasma irregularities seen by GNSS receiver networks and SAR radars will be also shown. Conference Object EISCAT Unknown |
spellingShingle | Institut für Solar-Terrestrische Physik Pokhotelov, Dimitry Günzkofer, Florian Ludwig Stober, Gunter Fernandez Gomez, Isabel Borries, C. 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/188787/ https://elib.dlr.de/188787/1/image2022_Pokhotelov.pdf https://space.fmi.fi/image/www/image_meeting_2022/ |