Deduction of temperature profile from MST radar observations of vertical wind

Deduction of temperature profile from MST radar observations of vertical wind

From the temporal spectra of vertical wind obtained from MST radar observations, the Brunt‐Vaisala frequency is identified. Altitude profile of temperature in troposphere and lower stratosphere is derived from the altitude profile of the Brunt‐Vaisala frequency thus obtained.

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Veröffentlicht in:Geophysical research letters 1996-02, Vol.23 (3), p.285-288
Hauptverfasser: Revathy, K., Prabhakaran Nair, S. R., Krisha Murthy, B. V.
Format: Artikel
Sprache:eng
Schlagworte:
Altitude
Brunt-Vaisala frequency
Earth, ocean, space
Exact sciences and technology
External geophysics
Geophysics
Meteorology
Other topics in atmospheric geophysics
Radar
Spectra
Stratosphere
Temporal logic
Troposphere
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Beschreibung
Zusammenfassung:From the temporal spectra of vertical wind obtained from MST radar observations, the Brunt‐Vaisala frequency is identified. Altitude profile of temperature in troposphere and lower stratosphere is derived from the altitude profile of the Brunt‐Vaisala frequency thus obtained.
ISSN:0094-8276
1944-8007
DOI:10.1029/96GL00086