Articles | Volume 17, issue 1
Atmos. Chem. Phys., 17, 531–549, 2017
Atmos. Chem. Phys., 17, 531–549, 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 et al.

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Cited articles

Angevine, W. M., Baltink, H. K., and Bosveld, F. C.: Observations of the morning transition of the convective boundary layer, Bound.-Lay. Meteorol., 101, 209–227, 2001.
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.,, 2016.
Ao, C. O., Waliser, D. E., Chan, S. K., Li, J. L., Tian, B., Xie, F., and Mannucci, A. J.: Planetary boundary layer heights from GPS radio occultation refractivity and humidity profiles, J. Geophys. Res.-Atmos., 117, D16117,, 2012.
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,, 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.
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).
Final-revised paper