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Study of mean vertical motions over Gadanki (13.5°N, 79.2°E), a tropical station, using Indian MST radar
Author(s) -
Jagannadha Rao V. V. M.,
Venkat Ratnam M.,
Narayana Rao D.
Publication year - 2002
Publication title -
radio science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.371
H-Index - 84
eISSN - 1944-799X
pISSN - 0048-6604
DOI - 10.1029/2001rs002505
Subject(s) - stratosphere , troposphere , atmospheric sciences , geology , monsoon , radar , gravity wave , mesosphere , range (aeronautics) , wind speed , climatology , vertical velocity , geodesy , physics , gravitational wave , telecommunications , materials science , computer science , astrophysics , composite material , oceanography , mechanics
Long‐term mean vertical velocities observed by the Mesosphere‐Stratosphere‐Troposphere (MST) radar over a tropical station, Gadanki, India (13.5°N, 79.2°E), are presented for the first time in this paper. Profiles of mean vertical velocities show wave like structure with a vertical wavelength of ∼6 km, and the observed values range from 3 to 20 cm s −1 on average. During monsoon and postmonsoon seasons, larger magnitudes are observed up to 20 cm s −1 . From the present study, an interesting feature, reversal in vertical velocities from downward to upward between 5 and 10 km during the monsoon season, is observed. This upward motion in long term averaged vertical velocity is thought to be due to reversal in wind direction around this height range and also due to horizontal velocity convergence, which is frequently observed over this region. One more reversal is observed near the Tropical Easterly Jet (TEJ) (around 16 km), which is from downward to upward and always showing minimum vertical velocities close to zero. This reversal can be attributed to instabilities associated with the jet streams. Large negative values are observed in the lower troposphere below 6 km, which are attributed to large vertical wind variances observed in this region indicating gravity wave activity.