Articles | Volume 18, issue 16
https://doi.org/10.5194/acp-18-11709-2018
https://doi.org/10.5194/acp-18-11709-2018
Research article
 | 
17 Aug 2018
Research article |  | 17 Aug 2018

Cloud vertical structure over a tropical station obtained using long-term high-resolution radiosonde measurements

Nelli Narendra Reddy, Madineni Venkat Ratnam, Ghouse Basha, and Varaha Ravikiran

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Cited articles

Basha, G. and Ratnam, M. V.: Identification of atmospheric boundary layer height over a tropical station using high-resolution radiosonde refractivity profiles: Comparison with GPS radio occultation measurements, J. Geophys. Res.-Atmos., 114, D16101, https://doi.org/10.1029/2008JD011692, 2009. 
Basha, G. and Ratnam, M. V.: Moisture variability over Indian monsoon regions observed using high resolution radiosonde measurements, Atmos. Res., 132–133, 35–45, https://doi.org/10.1016/j.atmosres.2013.04.004, 2013. 
Behrangi, A., Kubar, T., and Lambrigtsen, B.: Phenomenological Description of Tropical Clouds Using CloudSat Cloud Classification, Mon. Weather Rev., 140, 3235–3249, https://doi.org/10.1175/MWR-D-11-00247.1, 2012. 
Biondi, R., Randel, W. J., Ho, S.-P., Neubert, T., and Syndergaard, S.: Thermal structure of intense convective clouds derived from GPS radio occultations, Atmos. Chem. Phys., 12, 5309–5318, https://doi.org/10.5194/acp-12-5309-2012, 2012. 
Biondi, R., Ho, S.-P., Randel, W. J., Neubert, T., and Syndergaard, S.: Tropical cyclone cloud-top height and vertical temperature structure detection using GPS radio occultation measurements, J. Geophys. Res.-Atmos., 118, 5247–5259, https://doi.org/10.1002/jgrd.50448, 2013. 
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Short summary
Cloud vertical structure affects large-scale atmosphere circulation by altering gradients in total diabatic heating and cooling and latent heat release. Detailed cloud vertical structure in all seasons, including diurnal variation over the Indian region, is made for the first time. The detected cloud layers are verified with independent observations using cloud particle sensor sonde. Heating and cooling in the troposphere and lower stratosphere due to these cloud layers are also investigated.
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