Seasonal and Altitude Dependence of Thermospheric Metastable Helium Densities Measured by Fluorescence Lidar

Abstract Airglow originating from metastable helium He(23S) at 1,083 nm has been used to study the upper thermosphere since its discovery in 1959, yielding insights into, for example, solar EUV intensities and thermospheric photoelectron densities. For over 6 decades, these measurements were made pa...

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Main Authors: C. Geach, B. Kaifler
Format: Article
Language:English
Published: Wiley 2025-01-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2024GL112885
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author C. Geach
B. Kaifler
author_facet C. Geach
B. Kaifler
author_sort C. Geach
collection DOAJ
description Abstract Airglow originating from metastable helium He(23S) at 1,083 nm has been used to study the upper thermosphere since its discovery in 1959, yielding insights into, for example, solar EUV intensities and thermospheric photoelectron densities. For over 6 decades, these measurements were made passively, relying on solar illumination of the He(23S) layer to produce a detectable signal, resulting in a column integration of the He(23S) layer. Recently, the first height‐resolved measurements of He(23S) density were made by fluorescence lidar, opening a new window for studying the upper thermosphere. We report on a series of 51 measurements by this instrument spanning an entire winter season and extending to an altitude of 1,000 km, revealing a broad He(23S) layer that peaks at higher altitudes than previously expected.
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publishDate 2025-01-01
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series Geophysical Research Letters
spelling doaj-art-7793bb2aafa6462da1ebfa7e6792e1dc2025-01-20T13:05:57ZengWileyGeophysical Research Letters0094-82761944-80072025-01-01521n/an/a10.1029/2024GL112885Seasonal and Altitude Dependence of Thermospheric Metastable Helium Densities Measured by Fluorescence LidarC. Geach0B. Kaifler1Deutsches Zentrum für Luft‐ und Raumfahrt Institut für Solar‐Terrestrische Physik Neustrelitz GermanyDeutsches Zentrum für Luft‐ und Raumfahrt Institut für Physik der Atmosphäre Oberpfaffenhofen GermanyAbstract Airglow originating from metastable helium He(23S) at 1,083 nm has been used to study the upper thermosphere since its discovery in 1959, yielding insights into, for example, solar EUV intensities and thermospheric photoelectron densities. For over 6 decades, these measurements were made passively, relying on solar illumination of the He(23S) layer to produce a detectable signal, resulting in a column integration of the He(23S) layer. Recently, the first height‐resolved measurements of He(23S) density were made by fluorescence lidar, opening a new window for studying the upper thermosphere. We report on a series of 51 measurements by this instrument spanning an entire winter season and extending to an altitude of 1,000 km, revealing a broad He(23S) layer that peaks at higher altitudes than previously expected.https://doi.org/10.1029/2024GL112885thermospherelidarheliumionospherespace weather
spellingShingle C. Geach
B. Kaifler
Seasonal and Altitude Dependence of Thermospheric Metastable Helium Densities Measured by Fluorescence Lidar
Geophysical Research Letters
thermosphere
lidar
helium
ionosphere
space weather
title Seasonal and Altitude Dependence of Thermospheric Metastable Helium Densities Measured by Fluorescence Lidar
title_full Seasonal and Altitude Dependence of Thermospheric Metastable Helium Densities Measured by Fluorescence Lidar
title_fullStr Seasonal and Altitude Dependence of Thermospheric Metastable Helium Densities Measured by Fluorescence Lidar
title_full_unstemmed Seasonal and Altitude Dependence of Thermospheric Metastable Helium Densities Measured by Fluorescence Lidar
title_short Seasonal and Altitude Dependence of Thermospheric Metastable Helium Densities Measured by Fluorescence Lidar
title_sort seasonal and altitude dependence of thermospheric metastable helium densities measured by fluorescence lidar
topic thermosphere
lidar
helium
ionosphere
space weather
url https://doi.org/10.1029/2024GL112885
work_keys_str_mv AT cgeach seasonalandaltitudedependenceofthermosphericmetastableheliumdensitiesmeasuredbyfluorescencelidar
AT bkaifler seasonalandaltitudedependenceofthermosphericmetastableheliumdensitiesmeasuredbyfluorescencelidar