The airglow layer emission altitude cannot be determined unambiguously from temperature comparison with lidars
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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The airglow layer emission altitude cannot be determined unambiguously from temperature comparison with lidars ; volume:18 ; number:9 ; year:2018 ; pages:6691-6697
Atmospheric chemistry and physics ; 18, Heft 9 (2018), 6691-6697
- Creator
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Dunker, Tim
- DOI
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10.5194/acp-18-6691-2018
- URN
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urn:nbn:de:101:1-2018061515221770063114
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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15.08.2025, 7:25 AM CEST
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Associated
- Dunker, Tim
Other Objects (12)
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The Temporal Phasing of Rapid Dansgaard–Oeschger Warming Events Cannot Be Reliably Determined
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Vehicle Hydrocarbons’ Emission Characteristics Determined Using the Monte Carlo Method
Variations of the 630.0 nm airglow emission with meridional neutral wind and neutral temperature around midnight
Variations of the 630.0 nm airglow emission with meridional neutral wind and neutral temperature around midnight
Undetermined? Determined, very determined
It cannot be
Response of the airglow OH emission, temperature and mesopause wind to the atmospheric wave propagation over Shigaraki, Japan
The OH * (3–1) layer emission altitude cannot be determined unambiguously from temperature comparison with lidars
Radiation belt particles and OII emissions determined as contaminations of geocoronal helium airglow observations
Daytime sodium airglow emission measurements over Trivandrum using a scanning monochromator: first results
The Temporal Phasing of Rapid Dansgaard–Oeschger Warming Events Cannot Be Reliably Determined
Chest compressions at altitude are of decreased quality, require more effort and cannot reliably be self-evaluated
Why $$\alpha _s$$ αs cannot be determined from hadronic processes without simultaneously determining the parton distributions
Vehicle Hydrocarbons’ Emission Characteristics Determined Using the Monte Carlo Method
Variations of the 630.0 nm airglow emission with meridional neutral wind and neutral temperature around midnight
Variations of the 630.0 nm airglow emission with meridional neutral wind and neutral temperature around midnight
Undetermined? Determined, very determined
It cannot be
Response of the airglow OH emission, temperature and mesopause wind to the atmospheric wave propagation over Shigaraki, Japan
The OH * (3–1) layer emission altitude cannot be determined unambiguously from temperature comparison with lidars
Radiation belt particles and OII emissions determined as contaminations of geocoronal helium airglow observations
Daytime sodium airglow emission measurements over Trivandrum using a scanning monochromator: first results
The Temporal Phasing of Rapid Dansgaard–Oeschger Warming Events Cannot Be Reliably Determined
Chest compressions at altitude are of decreased quality, require more effort and cannot reliably be self-evaluated
Why $$\alpha _s$$ αs cannot be determined from hadronic processes without simultaneously determining the parton distributions
Vehicle Hydrocarbons’ Emission Characteristics Determined Using the Monte Carlo Method
Variations of the 630.0 nm airglow emission with meridional neutral wind and neutral temperature around midnight
Variations of the 630.0 nm airglow emission with meridional neutral wind and neutral temperature around midnight
Undetermined? Determined, very determined
It cannot be