Abstract
We report duration-related properties of rain events at a high-altitude site in the Western Ghats (WG) of India during the summer monsoon (June–September) season. Duration of rain events is inferred from disdrometer data collected during the years 2015–18. Vertical profiles of events of different durations are studied using data of an X-band radar available for 2017–18 monsoon seasons. Durations of rain events span from 0.1 to 160 h. Rain intensity (i.e., rain rate), mass weighted drop diameter, and rain liquid water content decrease with duration up to 1 h, remain steady between 1 and 20 h, and then increase for larger durations. Rain drop number concentration shows an increasing trend with duration up to around 10 h and then decreases. Rain events are categorized into short- (< 10 h) and long-duration (> 10 h) events based on rain drop characteristics. The long-duration events account for ~ 15% of the total number of events and contribute ~ 75% to the monsoon rainfall. The long-duration events have association with the monsoon rainfall over the Indian core monsoon zone with a correlation coefficient of 0.77. The frequency distribution of 18 dBZ radar echo top height exhibits bimodal structure (around 2 km and 4 km) for both short and long events with a longer tail in the case of former. The study is primarily focused on the summer monsoon season; however, we also report the rain duration features during the pre-monsoon (March–May) season.
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Data availability
The datasets generated during and/or analyzed during the current study are available from the corresponding author (Email: ambuj.cat@tropmet.res.in) on reasonable request.
References
Beard KV (1985) Simple altitude adjustments to raindrop velocities for doppler radar analysis. J Atmos Ocean Technol 2(4):468–471. https://doi.org/10.1175/1520-0426(1985)002%3c0468:saatrv%3e2.0.co;2
Bracken LJ, Cox NJ, Shannon J (2008) The relationship between rainfall inputs and flood generation in south-east Spain. Hydrol Processes 22:683–696
Bringi VN, Chandrasekar V (2001) Polarimetric doppler weather radar: principles and applications. Cambridge University Press, Cambridge, p 636
Chandrasekar V, Baldini L, Bharadwaj N, Smith P (2015) Calibration procedures for global precipitation-measurements ground-validation radars. Radio Sci Bull 355:45–73
Chen H, Zhou T, Yu R, Li J (2009) Summer rain fall duration and its diurnal cycle over the US Great Plains. Int J Climatol 29:1515–1519. https://doi.org/10.1002/joc.1806
Das SK, Krishna UVM, Kolte YK, Deshpande SM, Pandithurai G (2020) Assessment of ground-based X-band radar reflectivity: attenuation correction and its comparison with space-borne radars over the Western Ghats. India Earth Sp Sci. https://doi.org/10.1029/2019EA000861
Dash SK, Kulkarni MA, Mohanty UC, Prasad K (2009) Changes in the characteristics of rain events in India. J Geophys Res Atmos. https://doi.org/10.1029/2008JD010572
Dash SK, Nair AA, Kulkarni MA, Mohanty UC (2011) Characteristic changes in the long and short spells of different rain intensities in India. TheorApplClimatol 105:563–570. https://doi.org/10.1007/s00704-011-0416-x
Deshpande NR, Kulkarni A, Krishna Kumar K (2012) Characteristic features of hourly rainfall in India. Int J Climatol 32:1730–1744. https://doi.org/10.1002/joc.2375
Distromet (2002) Disdrometer RD-80 Instruction Manual. Distromet Ltd., Switzerland
Francis PA, Gadgil S (2006) Intense rainfall events over the west coast of India 42:27–42. https://doi.org/10.1007/s00703-005-0167-2
Goel NK, Kurothe RS, Mathur BS, Vogel RM (2000) A derived flood frequency distribution for correlated rainfall intensity and duration. J Hydrol 228:56–67. https://doi.org/10.1016/S0022-1694(00)00145-1
Grossman RL, Durran DR (1984) Interaction of low-level flow with the Western Ghat mountains and offshore convection in the summer monsoon. Mon Wea Rev 112:652–672
Gunn R, Kinzer GD (1949) The terminal velocity of the fall of droplets in stagnant air. J Meteor 6:243–248
Houze RA (1993) Cloud dynamics. Academic Press, Cambridge, p 496p
Houze RA (2004) Mesoscale convective systems. Rev Geophys. https://doi.org/10.1029/2004RG000150
Houze RA, Rasmussen KL, Zuluaga MD, Brodzik SR (2015) The variable nature of convection in the tropics and subtropics: a legacy of 16 years of the Tropical Rainfall Measuring Mission satellite. Rev Geophys 53:994–1021. https://doi.org/10.1002/2015RG000488
Joss J, Waldvogel A (1967) A spectrograph for raindrops with automatic interpretation. Pure Appl Geophys 68:240
Kalapureddy MCR, Deshpande S, Anand A, Das SK, Chakravarty K, Sonbawne SM, Maheskumar RS, Dani KK, Ernest Raj P (2017) An investigation of tropical Indian precipitating cloud systems using a Mobile X-band Scanning Polarimetric Radar: initial Results. J Neutral Atmos (1):59–81
Koteswaram P, De AC (1959) Study of premonsoon thunderstorms over GWB by radar. Ind J MeteorolGeophys 10:275–282
Kummerow C, Barnes W, Kozu T, Shiue J, Simpson J (1998) The Tropical Rainfall Measuring Mission (TRMM) sensor package. J Atmos Ocean Technol 15:809–817
Lenderink G, van Meijgaard E (2008) Increase in hourly precipitation extremes beyond expectations from temperature changes. Nat Geosci 1:511–514
Li J, Yu R, Zhou T (2008) Seasonal variation of the diurnal cycle of rainfall in southern contiguous China. J Clim 21:6036–6043. https://doi.org/10.1175/2008JCLI2188.1
Mukherjee AK, Sen PN (1983) Dependence of diurnal variation of thunderstorm on physical features. Vayu Mandal (special Issue) 13:105–108
Murali Krishna UV, Das SK, Sulochana EG, Bhowmik U, Deshpande SM, Pandithurai G (2021) Statistical characteristics of raindrop size distribution over the Western Ghats of India: wet versus dry spells of the Indian summer monsoon. Atmos Chem Phys 21:4741–4757. https://doi.org/10.5194/acp-21-4741-2021
Nandargi S, Mulye SS (2012) Relationships between rainy days, mean daily intensity, and seasonal rainfall over the Koyna catchment during 1961–2005. Sci World J. https://doi.org/10.1100/2012/894313
Nesbitt SW, Anders AM (2009) Very high-resolution precipitation climatologies from the Tropical Rainfall Measuring Mission precipitation radar. Geophys Res Lett 36:1–5. https://doi.org/10.1029/2009GL038026
Pai DS, Sridhar L, Rajeevan M, Sreejith OP, Satbhai NS, Mukhopadhyay B (2014) Development of a new high spatial resolution (0.25° × 0.25°) long period (1901–2010) daily gridded rainfall data set over India and its comparison with existing data sets over the region. Mausam 1:1–18
Rajeevan M, Gadgil S, Bhate J (2010) Active and break spells of the Indian Summer Monsoon. NCC research report: March 2008. J Earth Syst Sci 119:229–247
Rakhecha PR, Pisharoty PR (1996) Heavy rainfall during monsoon season: point and spatial distribution. Curr Sci 71:179–186
Raman PK, Raghavan K (1961) Diurnal variation of thunderstorm in india during different seasons. Indian J Met Geophys 12:115
Rao TN, Saikranthi K, Radhakrishna B, Bhaskara Rao SV (2016) Differences in the climatological characteristics of precipitation between active and break spells of the Indian Summer Monsoon. J Clim 29(21):7797–7814. https://doi.org/10.1175/JCLI-D-16-0028.1
Roca R, Fiolleau T (2020) Extreme precipitation in the tropics is closely associated with long-lived convective systems. Commun Earth Environ 1:18. https://doi.org/10.1038/s43247-020-00015-4
Roca R, Fiolleau T, Bouniol D (2017) A simple model of the life cycle of mesoscale convective systems cloud shield in the tropics. J Clim 30:4283–4298. https://doi.org/10.1175/JCLI-D-16-0556.1
Romatschke U, Medina S, Houze RA (2010) Regional, seasonal, and diurnal variations of extreme convection in the south Asian region. J Clim 23:419–439
Sukanya P, Kalapureddy MCR (2021) Cloud radar observations of multi-scale variability of cloud vertical structure associated with Indian summer monsoon over a tropical location. ClimDyn 56:1055–1081. https://doi.org/10.1007/s00382-020-05520-y
Tokay A, Petersen WA, Gatlin P, Wingo M (2013) Comparison of raindrop size distribution measurements by collocated disdrometers. J Atmos Ocean Technol 30:1672–1690. https://doi.org/10.1175/JTECH-D-12-00163.1
Tyagi A (2007) Thunderstorm climatology over Indian region. Mausam 2:189–212
Utsav B, Deshpande SM, Das SK, Pandithurai G, Niyogi D (2019) Observed vertical structure of convection during dry and wet summer Monsoon Epochs over the Western Ghats. J Geophys Res Atmos 124:1352–1369. https://doi.org/10.1029/2018JD028960
Westra S, Fowler HJ, Evans JP, Alexander LV, Berg P, Johnson F, Roberts NM (2014) Future changes to the intensity and frequency of short-duration extreme rainfall. Rev Geophys 52:522–555. https://doi.org/10.1002/2014RG000464
Yu R, Xu Y, Zhou T, Li J (2007) Relation between rainfall duration and diurnal variation in the warm season precipitation over central eastern China. Geophys Res Lett 34:10–13. https://doi.org/10.1029/2007GL030315
Yuan W, Yu R, Chen H, Li J, Zhang M (2010) Subseasonal characteristics of diurnal variation in summer monsoon rainfall over central Eastern China. J Clim 23:6684–6695. https://doi.org/10.1175/2010JCLI3805.1
Yuter SE, Houze RA (1995) Three-dimensional kinematic and microphysical evolution of Florida cumulonimbus. Part II: frequency distributions of vertical velocity, reflectivity, and differential reflectivity. Mon Weather Rev 123:1941–1963. https://doi.org/10.1175/1520-0493(1995)123%3c1941:TDKAME%3e2.0.CO;2
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Indian Institute of Tropical Meteorology (IITM), Pune is an autonomous organization and fully funded by the Ministry of Earth Sciences (MoES), Govt. of India. Authors are thankful to the Director, IITM, for the wholehearted support and encouragement in this work. The sincere efforts of technical staff involved in observations and maintenance at HACPL and radar site are thankfully acknowledged.
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Ambuj, J.K., Kalapureddy, M.C.R., Bhat, G.S. et al. Characteristics of rain events of different durations at a high-altitude site in the Western Ghats of India. Meteorol Atmos Phys 134, 63 (2022). https://doi.org/10.1007/s00703-022-00902-9
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DOI: https://doi.org/10.1007/s00703-022-00902-9