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Characterization of tropical precipitation using drop size distribution and rain rate-radar reflectivity relation

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Abstract

Characterization of precipitation is important for proper interpretation of rain information from remotely sensed data. Rain attenuation and radar reflectivity (Z) depend directly on the drop size distribution (DSD). The relation between radar reflectivity/rain attenuation and rain rate (R) varies widely depending upon the origin, topography, and drop evolution mechanism and needs further understanding of the precipitation characteristics. The present work utilizes 2 years of concurrent measurements of DSD using a ground-based disdrometer at five diverse climatic conditions in Indian subcontinent and explores the possibility of rain classification based on microphysical characteristics of precipitation. It is observed that both gamma and lognormal distributions are performing almost similar for Indian region with a marginally better performance by one model than other depending upon the locations. It has also been found that shape-slope relationship of gamma distribution can be a good indicator of rain type. The Z-R relation, Z = ARb, is found to vary widely for different precipitation systems, with convective rain that has higher values of A than the stratiform rain for two locations, whereas the reverse is observed for the rest of the three locations. Further, the results indicate that the majority of rainfall (>50%) in Indian region is due to the convective rain although the occurrence time of convective rain is low (<10%).

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References

  • Asen W (2002) A comparison of rain attenuation and drop size distributions measured in Chilbolton and Singapore. Radio Sci 37(3):1034

    Article  Google Scholar 

  • Bringi VN, Huang G-J, Munchak SJ, Kummerow CD, Marks DA, Wolff DB (2012) Comparison of drop size distribution parameter (D0) and rain rate from S-band dual-polarized ground radar, TRMM precipitation radar (PR), and combined PR–TMI: two events from Kwajalein atoll. J Atmos Ocean Technol 29:1603–1616

    Article  Google Scholar 

  • Campos EF, Zawadzki I, Petitdidier M, Fernández W (2006) Measurement of raindrop size distributions in tropical rain at Costa Rica. J Hydrol 328(1–2):98–109

    Article  Google Scholar 

  • Caracciolo C, Porcu F, Prodi F (2008) Precipitation classification at mid-latitudes in terms of drop size distribution parameters, adv. In Geoscience 16:11–17

    Google Scholar 

  • Churchill DD, Houze RA (1984) Development and structure of winter monsoon cloud clusters on winter monsoon cloud clusters on 10 December 1978. Journal of atmospheric science 41:933–960

    Article  Google Scholar 

  • Das S, Ghosh D (2016) Dependency of rain integral parameters on specific rain drop sizes and its seasonal behaviour. J Atmos Sol Terr Phys 149:15–20

    Article  Google Scholar 

  • Das S, Maitra A, Shukla AK (2010a) Rain attenuation modeling in the 10-100 GHz frequency using drop size distributions for different climatic zones in tropical India. Progress In Electromagnetics Research B 25:211–224

    Article  Google Scholar 

  • Das S, Shukla AK, Maitra A (2010b) Investigation of vertical profile of rain microstructure at Ahmedabad in Indian tropical region. Adv Space Res 45(10):1235–1243. doi:10.1016/j.asr.2010.01.001

    Article  Google Scholar 

  • Fabry F, Zawadzki I (1995) Long-term radar observations of the melting layer of precipitation and their interpretation. J. Atmos.Sci. 52:838–851

    Article  Google Scholar 

  • Fujiwara M (1965) Rain drop size distribution from individual storms. J Atmos Sci 22:585–591

    Article  Google Scholar 

  • Gamache JF, Houze RA (1982) Mesoscale air motions associated with tropical sqall line. Mon Weather Rev 110:118–135

    Article  Google Scholar 

  • Gunn R, Kinzer GD (1949) The terminal velocity of fall for water droplets in stagnant air. J Meteorol 6:243–248. doi:10.1175/1520-0469(1949)006<0243:TTVOFF>2.0.CO;2

    Article  Google Scholar 

  • Hazenberg P, Yu N, Boudevillain B, Delrieu G, Uijlenhoet R (2011) Scaling of raindrop size distributions and classification of radar reflectivity–rain rate relations in intense Mediterranean precipitation. J Hydrol 402(3–4):179–192

    Article  Google Scholar 

  • Houze RA (1993) Cloud dynamics. Academic, San Diego

  • Johnson RH, Hamilton PJ (1988) The relationship of surface features to the precipitation and air flow structure of an intense midlatitude squall line. Mon Weather Rev 116:1444–1472

    Article  Google Scholar 

  • Joss J, Waldvogel A (1969) Rain drop size distribution and sampling size errors. J Atmos Sci 26:566–569

    Article  Google Scholar 

  • Kozu T, Nakamura K (1991) Rainfall parameter estimation from dual radar measurements combining reflectivity profile and path-integrated attenuation. J Atmos Ocean Technol 8:259–271

    Article  Google Scholar 

  • Kozu T, Reddy KK, Mori S, Thurai M, Ong JT, Rao DN, Shimomai D (2006) Seasonal and diurnal variations of raindrop size distribution in Asian monsoon region. J Meteorol Soc Jpn. doi:10.2151/jmsj.84A.195

    Google Scholar 

  • Maitra A (2000) Three-parameter raindrop size distribution modelling at a tropical location. Electron Lett. doi:10.1049/el:20000667

    Google Scholar 

  • Maitra A, Das S, Shukla AK (2009) Joint statistics of rain rate and event duration for a tropical location in India. Indian Journal of Radio and Space Physics 38:253–260

    Google Scholar 

  • Marshall JS, Palmer WM (1948) The distribution of rain drop with size. J Meteorol 5:165–166

    Article  Google Scholar 

  • Narayana Rao T, Narayana RD, Raghavan S (1999) Tropical precipitating systems observed with Indian MST radar. Radio Sci 5:1125–1139

    Google Scholar 

  • Obiyemi OO, Ibiyemi TS, Ojo JS (2016) On validation of the rain climatic zone designations for Nigeria. Theor Appl Climatol. doi:10.1007/s00704-016-1787-9

    Google Scholar 

  • Prat OP, Barros AP (2010) Ground observations to characterize the spatial gradients and vertical structure of orographic precipitation – experiments in the inner region of the great Smoky Mountains. J Hydrol 391(1–2):141–156

    Article  Google Scholar 

  • Rao TN, Rao DN, Mohan K, Raghavan S (2002) Classification of tropical precipitating systems and associated Z-R relationships. JGeophys Res 106:17,699–17,711

    Article  Google Scholar 

  • Sekhon RS, Srivastava RC (1971) Doppler radar observations of drop-size distributions in a thunderstorm. J AtmosSci 28:983–994

    Article  Google Scholar 

  • Short DA, Kozu T, Nakamura K (1990) Rainrate and raindrop size distribution observations in Darwin, Australia in proceedings of URSI commission F open symposium on regional factors in predicting Radiowave attenuation due to rain. Int. Union of Radio Sci. Comm, Rio de Janeiro, pp 35–40

  • Sivaramakrishnan MV (1961) Studies of raindrop size characteristics in different types of tropical rain using a simple raindrop recorder, Indian J. Meteorol Geophys 12:189–217

    Google Scholar 

  • Tenório RS, Moraes MCDS, Sauvageot H (2012) Raindrop size distribution and radar parameters in coastal tropical rain systems of Northeastern Brazil. J Appl Meteorol Climatol 51:1960–1970

    Article  Google Scholar 

  • Testud J, Oury S, Blank RA, Amayenc P, Dou X (2001) The concept of “normalized” distribution to describe rain drop spectra: a tool for cloud physics and cloud remote sensing. J Appl Met 40:1118–1140

    Article  Google Scholar 

  • Thurai M, Bringi VN, May PT (2010) CPOL radar-derived drop size distribution statistics of stratiform and convective rain for two regimes in Darwin, Australia. J Atmos Ocean Technol 27:932–942. doi:10.1175/2010JTECHA1349.1

    Article  Google Scholar 

  • Timothy KI, Ong JT, Choo EBL (2002) Rain drop size distribution using method of moments for terrestrial and satellite communication applications in Singapore. IEEE Transaction on Antennas and Propagation 50(10):1420–1424

    Article  Google Scholar 

  • Tokay A, Short D (1996) Evidence from tropical rain drop spectra of the origin of rain from stratiform versus convective. J Appl Meteor 35:355–371

    Article  Google Scholar 

  • Ulbrich C (1983) Natural variations in the analytical form of the rain drop size distribution. J Clim And Appl Meterol 22:1764–1775

    Article  Google Scholar 

  • Waldvogel A (1974) The N0 jump of rain drop spectra. J Atmos Sci 31:1067–1078

    Article  Google Scholar 

  • Williams CR, Ecklund WL, Gage KS (1995) Classification of precipitating clouds in the tropics using 915 MHz wind profilers. Journal of Atmospheric Oceanic Technology 12:996–1012

    Article  Google Scholar 

  • Zawadski I, Monteiro E, Fabry F (1994) The development of drop size distributions in light rain. J Atm Sci 51:1100–1113

    Article  Google Scholar 

Download references

Acknowledgements

One of the authors (S. Das) thankfully acknowledge the financial support provided by the Department of Science and Technology, Govt. of India under INSPIRE Faculty Scheme. Authors also acknowledge the SAC, ISRO for the contribution in data collections.

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Correspondence to Saurabh Das.

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Das, S., Maitra, A. Characterization of tropical precipitation using drop size distribution and rain rate-radar reflectivity relation. Theor Appl Climatol 132, 275–286 (2018). https://doi.org/10.1007/s00704-017-2073-1

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