The Bonn University lidar at the Esrange: technical description and capabilities for atmospheric research
The Bonn University operates a Rayleigh/Mie/Raman backscatter lidar at the Esrange near the Swedish city of Kiruna, north of the Arctic circle. The lidar system covers the atmosphere from about 4 km to 100 km altitude and it is capable of measuring aerosols in the tropo-, strato-, and mesospher...
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doaj-cd19254a9c784572bd46b65299e2dd2e2020-11-24T22:10:11ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762005-07-01231645165810.5194/angeo-23-1645-2005The Bonn University lidar at the Esrange: technical description and capabilities for atmospheric researchU. Blum0U. Blum1K. H. Fricke2now at: Forsvarets forskningsinstitutt, Postboks 25, N-2027 Kjeller, NorwayPhysikalisches Institut der Universität Bonn, Nussallee 12, 53115 Bonn, GermanyPhysikalisches Institut der Universität Bonn, Nussallee 12, 53115 Bonn, GermanyThe Bonn University operates a Rayleigh/Mie/Raman backscatter lidar at the Esrange near the Swedish city of Kiruna, north of the Arctic circle. The lidar system covers the atmosphere from about 4 km to 100 km altitude and it is capable of measuring aerosols in the tropo-, strato-, and mesosphere, as well as of determining temperature profiles in the aerosol-free part of the atmosphere (i.e. above 30-km altitude). Density tuned fixed-spacer etalons provide daylight capability and thus increased sensitivity to noctilucent clouds during polar summer. Polarisation measurements allow liquid and solid phase discrimination for aerosol and cloud particles in the tropo- and stratosphere. The derived temperature profiles can be used for the detection and analysis of atmospheric gravity waves. Although several lidar experiments are situated in polar latitudes, a comprehensive instrument which covers the troposphere, stratosphere, and mesosphere, is daylight capable, and observes temperature profiles, as well as aerosols, is exceptional. In this article a technical description, in particular, of the optical configuration of this experiment is given, as well as an overview of achievable geophysical parameters. The potential for geophysical analyses is shown.<br><br> <b>Keywords.</b> Atmospheric composition and structure (Instruments and techniques; Aerosols and particles; Pressure, density and temperature) – Meteorology and atmospheric dynamics (Middle atmosphere dynamics)https://www.ann-geophys.net/23/1645/2005/angeo-23-1645-2005.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
U. Blum U. Blum K. H. Fricke |
spellingShingle |
U. Blum U. Blum K. H. Fricke The Bonn University lidar at the Esrange: technical description and capabilities for atmospheric research Annales Geophysicae |
author_facet |
U. Blum U. Blum K. H. Fricke |
author_sort |
U. Blum |
title |
The Bonn University lidar at the Esrange: technical description and capabilities for atmospheric research |
title_short |
The Bonn University lidar at the Esrange: technical description and capabilities for atmospheric research |
title_full |
The Bonn University lidar at the Esrange: technical description and capabilities for atmospheric research |
title_fullStr |
The Bonn University lidar at the Esrange: technical description and capabilities for atmospheric research |
title_full_unstemmed |
The Bonn University lidar at the Esrange: technical description and capabilities for atmospheric research |
title_sort |
bonn university lidar at the esrange: technical description and capabilities for atmospheric research |
publisher |
Copernicus Publications |
series |
Annales Geophysicae |
issn |
0992-7689 1432-0576 |
publishDate |
2005-07-01 |
description |
The Bonn University operates a Rayleigh/Mie/Raman backscatter
lidar at the Esrange near the Swedish city of Kiruna, north of the
Arctic circle. The lidar system covers the atmosphere from about
4 km to 100 km altitude and it is capable of measuring aerosols in
the tropo-, strato-, and mesosphere, as well as of determining
temperature profiles in the aerosol-free part of the atmosphere
(i.e. above 30-km altitude). Density tuned fixed-spacer etalons
provide daylight capability and thus increased sensitivity to
noctilucent clouds during polar summer. Polarisation measurements
allow liquid and solid phase discrimination for aerosol and cloud
particles in the tropo- and stratosphere. The derived temperature
profiles can be used for the detection and analysis of atmospheric
gravity waves. Although several lidar experiments are situated in
polar latitudes, a comprehensive instrument which covers the
troposphere, stratosphere, and mesosphere, is daylight capable,
and observes temperature profiles, as well as aerosols, is
exceptional. In this article a technical description, in particular,
of the optical configuration of this experiment is given, as well as
an overview of achievable geophysical parameters. The potential for
geophysical analyses is shown.<br><br>
<b>Keywords.</b> Atmospheric composition and structure (Instruments
and techniques; Aerosols and particles; Pressure, density
and temperature) – Meteorology and atmospheric dynamics
(Middle atmosphere dynamics) |
url |
https://www.ann-geophys.net/23/1645/2005/angeo-23-1645-2005.pdf |
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