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Simplified Relations for the Martian Night-Time OH Suitable for the Interpretation of Observations
by
Hartogh, Paul
, Sonnemann, Gerd Reinhold
, Shaposhnikov, Dmitry S.
, Medvedev, Alexander S.
, Grygalashvyly, Mykhaylo
in
Airglow
/ Altitude
/ Ambient temperature
/ Atmosphere
/ Atomic oxygen
/ Carbon dioxide
/ Concentration gradient
/ Emissions
/ excited hydroxyl
/ General circulation models
/ Mars
/ Mars atmosphere
/ Martian atmosphere
/ Night
/ nightglow
/ Nitrogen
/ Remote sensing
/ Temperature
2022
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Simplified Relations for the Martian Night-Time OH Suitable for the Interpretation of Observations
by
Hartogh, Paul
, Sonnemann, Gerd Reinhold
, Shaposhnikov, Dmitry S.
, Medvedev, Alexander S.
, Grygalashvyly, Mykhaylo
in
Airglow
/ Altitude
/ Ambient temperature
/ Atmosphere
/ Atomic oxygen
/ Carbon dioxide
/ Concentration gradient
/ Emissions
/ excited hydroxyl
/ General circulation models
/ Mars
/ Mars atmosphere
/ Martian atmosphere
/ Night
/ nightglow
/ Nitrogen
/ Remote sensing
/ Temperature
2022
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Simplified Relations for the Martian Night-Time OH Suitable for the Interpretation of Observations
by
Hartogh, Paul
, Sonnemann, Gerd Reinhold
, Shaposhnikov, Dmitry S.
, Medvedev, Alexander S.
, Grygalashvyly, Mykhaylo
in
Airglow
/ Altitude
/ Ambient temperature
/ Atmosphere
/ Atomic oxygen
/ Carbon dioxide
/ Concentration gradient
/ Emissions
/ excited hydroxyl
/ General circulation models
/ Mars
/ Mars atmosphere
/ Martian atmosphere
/ Night
/ nightglow
/ Nitrogen
/ Remote sensing
/ Temperature
2022
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Simplified Relations for the Martian Night-Time OH Suitable for the Interpretation of Observations
Journal Article
Simplified Relations for the Martian Night-Time OH Suitable for the Interpretation of Observations
2022
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Overview
Observations of excited hydroxyl (OH*) emissions are broadly used for inferring information about atmospheric dynamics and composition. We present several analytical approximations for characterizing the excited hydroxyl layer in the Martian atmosphere. They include the OH* number density at the maximum and the height of the peak, along with the relations for assessing different impacts on the OH* layer under night-time conditions. These characteristics are determined by the ambient temperature, atomic oxygen concentration, and their vertical gradients. The derived relations can be used for the analysis of airglow measurements and the interpretation of their variations.
Publisher
MDPI AG
Subject
MBRLCatalogueRelatedBooks
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