Estimation of ionospheric reflection height using long wave propagation

<p>Phase height measurements of low frequency radio waves are used to study the long-term variability of the mesosphere over Europe. Phase height measurements use a characteristic pattern in field strength registration of radio waves interpreted as phase relations between sky wave and surface...

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Main Author: D. Keuer
Format: Article
Language:deu
Published: Copernicus Publications 2019-09-01
Series:Advances in Radio Science
Online Access:https://www.adv-radio-sci.net/17/205/2019/ars-17-205-2019.pdf
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author D. Keuer
author_facet D. Keuer
author_sort D. Keuer
collection DOAJ
description <p>Phase height measurements of low frequency radio waves are used to study the long-term variability of the mesosphere over Europe. Phase height measurements use a characteristic pattern in field strength registration of radio waves interpreted as phase relations between sky wave and surface wave to obtain the apparent height of the reflection point, the Standard Phase Height (SPH). Based on this SPH-method a homogenized daily series was generated since 1959 at Kühlungsborn. Improvements of the measuring method show that the signal is significantly influenced by lower atmospheric layers. Mesospheric reflection is not the exclusive source of the measured behavior. Tropospheric influence can not be neglected. Taking this into account one has to conclude that the strong coherency of the SPH data to mesospheric heights is not as significant as previously assumed.</p>
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spelling doaj.art-e3e1de50af73407f838111e3fc0bf7372022-12-21T21:04:54ZdeuCopernicus PublicationsAdvances in Radio Science1684-99651684-99732019-09-011720521210.5194/ars-17-205-2019Estimation of ionospheric reflection height using long wave propagationD. Keuer<p>Phase height measurements of low frequency radio waves are used to study the long-term variability of the mesosphere over Europe. Phase height measurements use a characteristic pattern in field strength registration of radio waves interpreted as phase relations between sky wave and surface wave to obtain the apparent height of the reflection point, the Standard Phase Height (SPH). Based on this SPH-method a homogenized daily series was generated since 1959 at Kühlungsborn. Improvements of the measuring method show that the signal is significantly influenced by lower atmospheric layers. Mesospheric reflection is not the exclusive source of the measured behavior. Tropospheric influence can not be neglected. Taking this into account one has to conclude that the strong coherency of the SPH data to mesospheric heights is not as significant as previously assumed.</p>https://www.adv-radio-sci.net/17/205/2019/ars-17-205-2019.pdf
spellingShingle D. Keuer
Estimation of ionospheric reflection height using long wave propagation
Advances in Radio Science
title Estimation of ionospheric reflection height using long wave propagation
title_full Estimation of ionospheric reflection height using long wave propagation
title_fullStr Estimation of ionospheric reflection height using long wave propagation
title_full_unstemmed Estimation of ionospheric reflection height using long wave propagation
title_short Estimation of ionospheric reflection height using long wave propagation
title_sort estimation of ionospheric reflection height using long wave propagation
url https://www.adv-radio-sci.net/17/205/2019/ars-17-205-2019.pdf
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