Multi‐Instrument Observations of Ion‐Neutral Coupling in the Dayside Cusp
Using data from the Scanning Doppler Imager, the Super Dual Auroral Radar Network, the EISCAT Svalbard Radar, and an auroral all‐sky imager, we examine an instance of urn:x-wiley:grl:media:grl60177:grl60177-math-0001 region neutral winds which have been influenced by the presence of poleward moving...
Main Authors: | , , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union (AGU)
2020
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Subjects: | |
Online Access: | https://discovery.ucl.ac.uk/id/eprint/10092567/8/Aruliah_2019GL085590_1.pdf https://discovery.ucl.ac.uk/id/eprint/10092567/ |
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author | Billett, DD Hosokawa, K Grocott, A Wild, JA Aruliah, AL Ogawa, Y Taguchi, S Lester, M |
author_facet | Billett, DD Hosokawa, K Grocott, A Wild, JA Aruliah, AL Ogawa, Y Taguchi, S Lester, M |
author_sort | Billett, DD |
collection | University College London: UCL Discovery |
description | Using data from the Scanning Doppler Imager, the Super Dual Auroral Radar Network, the EISCAT Svalbard Radar, and an auroral all‐sky imager, we examine an instance of urn:x-wiley:grl:media:grl60177:grl60177-math-0001 region neutral winds which have been influenced by the presence of poleward moving auroral forms near the dayside cusp region. We observe a reduction in the time taken for the ion drag force to reorientate the neutrals into the direction of the convective plasma (on the order of minutes), compared to before the auroral activity began. Additionally, because the ionosphere near the cusp is influenced much more readily by changes in the solar wind via dayside reconnection, we observe the neutrals responding to an interplanetary magnetic field change within minutes of it occurring. This has implications on the rate that energy is deposited into the ionosphere via Joule heating, which we show to become dampened by the neutral winds. |
format | Article in Journal/Newspaper |
genre | EISCAT Svalbard |
genre_facet | EISCAT Svalbard |
geographic | Svalbard |
geographic_facet | Svalbard |
id | ftucl:oai:eprints.ucl.ac.uk.OAI2:10092567 |
institution | Open Polar |
language | English |
op_collection_id | ftucl |
op_relation | https://discovery.ucl.ac.uk/id/eprint/10092567/8/Aruliah_2019GL085590_1.pdf https://discovery.ucl.ac.uk/id/eprint/10092567/ |
op_rights | open |
op_source | Geophysical Research Letters , 47 (4) (2020) |
publishDate | 2020 |
publisher | American Geophysical Union (AGU) |
record_format | openpolar |
spelling | ftucl:oai:eprints.ucl.ac.uk.OAI2:10092567 2025-01-16T21:42:13+00:00 Multi‐Instrument Observations of Ion‐Neutral Coupling in the Dayside Cusp Billett, DD Hosokawa, K Grocott, A Wild, JA Aruliah, AL Ogawa, Y Taguchi, S Lester, M 2020-02-28 text https://discovery.ucl.ac.uk/id/eprint/10092567/8/Aruliah_2019GL085590_1.pdf https://discovery.ucl.ac.uk/id/eprint/10092567/ eng eng American Geophysical Union (AGU) https://discovery.ucl.ac.uk/id/eprint/10092567/8/Aruliah_2019GL085590_1.pdf https://discovery.ucl.ac.uk/id/eprint/10092567/ open Geophysical Research Letters , 47 (4) (2020) ionosphere neutral wind ion‐neutral coupling ion drag SuperDARN FPI Article 2020 ftucl 2023-11-27T13:07:34Z Using data from the Scanning Doppler Imager, the Super Dual Auroral Radar Network, the EISCAT Svalbard Radar, and an auroral all‐sky imager, we examine an instance of urn:x-wiley:grl:media:grl60177:grl60177-math-0001 region neutral winds which have been influenced by the presence of poleward moving auroral forms near the dayside cusp region. We observe a reduction in the time taken for the ion drag force to reorientate the neutrals into the direction of the convective plasma (on the order of minutes), compared to before the auroral activity began. Additionally, because the ionosphere near the cusp is influenced much more readily by changes in the solar wind via dayside reconnection, we observe the neutrals responding to an interplanetary magnetic field change within minutes of it occurring. This has implications on the rate that energy is deposited into the ionosphere via Joule heating, which we show to become dampened by the neutral winds. Article in Journal/Newspaper EISCAT Svalbard University College London: UCL Discovery Svalbard |
spellingShingle | ionosphere neutral wind ion‐neutral coupling ion drag SuperDARN FPI Billett, DD Hosokawa, K Grocott, A Wild, JA Aruliah, AL Ogawa, Y Taguchi, S Lester, M Multi‐Instrument Observations of Ion‐Neutral Coupling in the Dayside Cusp |
title | Multi‐Instrument Observations of Ion‐Neutral Coupling in the Dayside Cusp |
title_full | Multi‐Instrument Observations of Ion‐Neutral Coupling in the Dayside Cusp |
title_fullStr | Multi‐Instrument Observations of Ion‐Neutral Coupling in the Dayside Cusp |
title_full_unstemmed | Multi‐Instrument Observations of Ion‐Neutral Coupling in the Dayside Cusp |
title_short | Multi‐Instrument Observations of Ion‐Neutral Coupling in the Dayside Cusp |
title_sort | multi‐instrument observations of ion‐neutral coupling in the dayside cusp |
topic | ionosphere neutral wind ion‐neutral coupling ion drag SuperDARN FPI |
topic_facet | ionosphere neutral wind ion‐neutral coupling ion drag SuperDARN FPI |
url | https://discovery.ucl.ac.uk/id/eprint/10092567/8/Aruliah_2019GL085590_1.pdf https://discovery.ucl.ac.uk/id/eprint/10092567/ |