Articles | Volume 17, issue 1
https://doi.org/10.5194/acp-17-531-2017
https://doi.org/10.5194/acp-17-531-2017
Research article
 | 
11 Jan 2017
Research article |  | 11 Jan 2017

Diurnal variability of the atmospheric boundary layer height over a tropical station in the Indian monsoon region

Sanjay Kumar Mehta, Madineni Venkat Ratnam, Sukumarapillai V. Sunilkumar, Daggumati Narayana Rao, and Boddapaty V. Krishna Murthy

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Cited articles

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Anurose, T. J., Subrahamanyam, D. B., and Sunilkumar, S. V.: Two years observations on the diurnal evolution of coastal atmospheric boundary layer features over Thiruvananthapuram (8.5° N, 76.9° E), India, Theor. Appl. Climatol., https://doi.org/10.1007/s00704-016-1955-y, 2016.
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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.
Bianco, L., Djalalova, I., King, C., and Wilczak, J.: Diurnal evolution and annual variability of boundary-layer height and its correlation to other meteorological variables in California's Central Valley, Bound.-Lay. Meteorol., 140, 491–511, 2011.
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Short summary
Study of the diurnal variation of the atmospheric boundary layer (ABL) height is important for the knowledge of pollutant dispersion, crucial for all living beings. The most difficult part in the study of the diurnal variation is in identification of the stable boundary layer which occurs ~ 50% of times only and mostly during nighttime winter. Surface temperature and clouds directly affect the diurnal pattern of the ABL. Thus, stronger (weaker) diurnal variation found during pre-monsoon (winter).
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