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Deduction of temperature profile from MST radar observations of vertical wind
Author(s) -
Revathy K.,
Prabhakaran Nair S. R.,
Krisha Murthy B. V.
Publication year - 1996
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/96gl00086
Subject(s) - stratosphere , troposphere , altitude (triangle) , atmospheric sciences , potential temperature , radar , environmental science , meteorology , atmospheric temperature , geology , physics , telecommunications , geometry , mathematics , computer science
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.