Spectral observations of Polar Mesospheric Summer Echoes (PMSE)

We present spectral measurements of PMSE under the influence of HF heating cycles. The data has been obtained with EISCAT VHF radar, during the EISCAT campaign 2004 in Tromsø. Examples where the PMSE overshoot appears when the electrons are heated with a specific cycle are shown. A detailed analysis...

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Bibliographic Details
Main Author: López Muñoz, Aquilino
Format: Master Thesis
Language:English
Published: Universitetet i Tromsø 2007
Subjects:
Online Access:https://hdl.handle.net/10037/1201
id ftunivtroemsoe:oai:munin.uit.no:10037/1201
record_format openpolar
spelling ftunivtroemsoe:oai:munin.uit.no:10037/1201 2024-06-02T08:05:58+00:00 Spectral observations of Polar Mesospheric Summer Echoes (PMSE) López Muñoz, Aquilino 2007-06-15 6559958 bytes application/pdf https://hdl.handle.net/10037/1201 eng eng Universitetet i Tromsø University of Tromsø https://hdl.handle.net/10037/1201 URN:NBN:no-uit_munin_892 openAccess Copyright 2007 The Author(s) VDP::Mathematics and natural science: 400::Physics: 430 Frequency jumps gravity waves heating facility overshoot Polar Mesospheric Summer Echoes Master thesis Mastergradsoppgave 2007 ftunivtroemsoe 2024-05-07T08:40:37Z We present spectral measurements of PMSE under the influence of HF heating cycles. The data has been obtained with EISCAT VHF radar, during the EISCAT campaign 2004 in Tromsø. Examples where the PMSE overshoot appears when the electrons are heated with a specific cycle are shown. A detailed analysis of PMSE spectral width during the heating cycles concluded that there is no evidence of a possible correlation between them. In our measurements we found several frequency jumps. By analysing the abruptness one observed (with a discontinuity of the vertical velocity around 56 m/s in less than 10 seconds), we resolve for the first time how this “jump” takes place. During the transition from one Doppler velocity to the opposite, the gradual death of one Doppler velocity “layer” is observed while a new one appears increasing in amplitude until the frequency jump finishes, where the first Doppler has completely disappear and the new one has a value equivalent to the one before with opposite sign. Different models which may explain the source of the frequency jumps were tested, finding that wave steepening could explain some of the cases reported. Not many clear examples of possible signatures of gravity waves were found. In the analysis of the best candidates, we obtained values of vertical phase velocities around /s and vertical wave numbers around 15 m/s and vertical wave numbers around 6x10e-4(1/m)which are reasonable values for atmospherical gravity waves so, we think that PMSE could be modulated by gravity waves during the EISCAT campaign. Master Thesis EISCAT Tromsø University of Tromsø: Munin Open Research Archive Tromsø
institution Open Polar
collection University of Tromsø: Munin Open Research Archive
op_collection_id ftunivtroemsoe
language English
topic VDP::Mathematics and natural science: 400::Physics: 430
Frequency jumps
gravity waves
heating facility
overshoot
Polar Mesospheric Summer Echoes
spellingShingle VDP::Mathematics and natural science: 400::Physics: 430
Frequency jumps
gravity waves
heating facility
overshoot
Polar Mesospheric Summer Echoes
López Muñoz, Aquilino
Spectral observations of Polar Mesospheric Summer Echoes (PMSE)
topic_facet VDP::Mathematics and natural science: 400::Physics: 430
Frequency jumps
gravity waves
heating facility
overshoot
Polar Mesospheric Summer Echoes
description We present spectral measurements of PMSE under the influence of HF heating cycles. The data has been obtained with EISCAT VHF radar, during the EISCAT campaign 2004 in Tromsø. Examples where the PMSE overshoot appears when the electrons are heated with a specific cycle are shown. A detailed analysis of PMSE spectral width during the heating cycles concluded that there is no evidence of a possible correlation between them. In our measurements we found several frequency jumps. By analysing the abruptness one observed (with a discontinuity of the vertical velocity around 56 m/s in less than 10 seconds), we resolve for the first time how this “jump” takes place. During the transition from one Doppler velocity to the opposite, the gradual death of one Doppler velocity “layer” is observed while a new one appears increasing in amplitude until the frequency jump finishes, where the first Doppler has completely disappear and the new one has a value equivalent to the one before with opposite sign. Different models which may explain the source of the frequency jumps were tested, finding that wave steepening could explain some of the cases reported. Not many clear examples of possible signatures of gravity waves were found. In the analysis of the best candidates, we obtained values of vertical phase velocities around /s and vertical wave numbers around 15 m/s and vertical wave numbers around 6x10e-4(1/m)which are reasonable values for atmospherical gravity waves so, we think that PMSE could be modulated by gravity waves during the EISCAT campaign.
format Master Thesis
author López Muñoz, Aquilino
author_facet López Muñoz, Aquilino
author_sort López Muñoz, Aquilino
title Spectral observations of Polar Mesospheric Summer Echoes (PMSE)
title_short Spectral observations of Polar Mesospheric Summer Echoes (PMSE)
title_full Spectral observations of Polar Mesospheric Summer Echoes (PMSE)
title_fullStr Spectral observations of Polar Mesospheric Summer Echoes (PMSE)
title_full_unstemmed Spectral observations of Polar Mesospheric Summer Echoes (PMSE)
title_sort spectral observations of polar mesospheric summer echoes (pmse)
publisher Universitetet i Tromsø
publishDate 2007
url https://hdl.handle.net/10037/1201
geographic Tromsø
geographic_facet Tromsø
genre EISCAT
Tromsø
genre_facet EISCAT
Tromsø
op_relation https://hdl.handle.net/10037/1201
URN:NBN:no-uit_munin_892
op_rights openAccess
Copyright 2007 The Author(s)
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