Articles | Volume 15, issue 5
https://doi.org/10.5194/acp-15-2709-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-2709-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Evidence for tropospheric wind shear excitation of high-phase-speed gravity waves reaching the mesosphere using the ray-tracing technique
M. Pramitha
National Atmospheric Research Laboratory (NARL), Gadanki, India
M. Venkat Ratnam
CORRESPONDING AUTHOR
National Atmospheric Research Laboratory (NARL), Gadanki, India
National Atmospheric Research Laboratory (NARL), Gadanki, India
B. V. Krishna Murthy
B1, CEBROS, Chennai, India
D. Pallamraju
Physical Research Laboratory (PRL), Ahmadabad, India
S. Vijaya Bhaskar Rao
Department of Physics, Sri Venkateswara University, Tirupati, India
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37 citations as recorded by crossref.
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- Radar observations of simultaneous traveling ionospheric disturbances and atmospheric gravity waves T. Nygrén et al. 10.1002/2014JA020794
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Latest update: 24 Dec 2024
Short summary
Sources and propagation characteristics of high-frequency gravity waves observed in the mesosphere using airglow emissions from Gadanki and Hyderabad, India, are investigated using reverse ray tracing. Wave amplitudes are also traced back, including both radiative and diffusive damping. Interestingly, large vertical shears in the horizontal wind are noticed near the ray terminal points (at 10-12km altitude) and are thus identified to be the source for generating the observed gravity waves.
Sources and propagation characteristics of high-frequency gravity waves observed in the...
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