Articles | Volume 21, issue 6
Atmos. Chem. Phys., 21, 4741–4757, 2021
Atmos. Chem. Phys., 21, 4741–4757, 2021
Research article
26 Mar 2021
Research article | 26 Mar 2021

Statistical characteristics of raindrop size distribution over the Western Ghats of India: wet versus dry spells of the Indian summer monsoon

Uriya Veerendra Murali Krishna et al.

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Statistical characteristics of raindrop size distribution over Western Ghats of India: wet versus dry spells of Indian Summer Monsoon
Uriya Veerendra Murali Krishna, Subrata Kumar Das, Ezhilarasi Govindaraj Sulochana, Bhowmik Utsav, Sachin Madhukar Deshpande, and Govindan Pandithurai
Atmos. Chem. Phys. Discuss.,,, 2019
Revised manuscript not accepted
Retrieval of convective available potential energy from INSAT-3D measurements: comparison with radiosonde data and their spatial–temporal variations
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Subject: Clouds and Precipitation | Research Activity: Field Measurements | Altitude Range: Troposphere | Science Focus: Physics (physical properties and processes)
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Cited articles

Atlas, D. and Ulbrich, C. W.: An observationally based conceptual model of warm oceanic convective rain in the tropics, J. Appl. Meteorol., 39, 2165–2181, 2000. a
Atlas, D., Ulbrich, C. W., Marks Jr., F. D., Amitai, E., and Williams, C. R.: Systematic variation of drop size and radar-rainfall relations, J. Geophys. Res.-Atmos., 104, 6155–6169, 1999. a
Bringi, V., Chandrasekar, V., Hubbert, J., Gorgucci, E., Randeu, W., and Schoenhuber, M.: Raindrop size distribution in different climatic regimes from disdrometer and dual-polarized radar analysis, J. Atmos. Sci., 60, 354–365, 2003. a, b, c
Bringi, V. N. and Chandrasekar, V.: Polarimetric Doppler Weather Radar: principles and applications, Cambridge University Press, Cambridge (MA), 2001. a
Cao, Q. and Zhang, G.: Errors in estimating raindrop size distribution parameters employing disdrometer and simulated raindrop spectra, J. Appl. Meteorol. Clim., 48, 406–425, 2009. a
Short summary
Indian summer monsoon (ISM) rainfall exhibits sub-seasonal variability as active spells with good rainfall (wet spell) and weak spells or breaks with little to no rainfall (dry spell). Studies have shown that during the wet and dry periods of the ISM, there are contrasting behaviors in the formation of weather systems and large-scale instability. Thus, it is worth investigating how the raindrop size distribution varies during intra-seasonal timescale variations of the ISM in the Western Ghats.
Final-revised paper