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WRF simulation of a severe hailstorm over Baramati: a study into the space–time evolution

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Abstract

Space–time evolution of a severe hailstorm occurred over the western India as revealed by WRF-ARW simulations are presented. We simulated a specific event centered over Baramati (18.15°N, 74.58°E, 537 m AMSL) on March 9, 2014. A physical mechanism, proposed as a conceptual model, signifies the role of multiple convective cells organizing through outflows leading to a cold frontal type flow, in the presence of a low over the northern Arabian Sea, propagates from NW to SE triggering deep convection and precipitation. A ‘U’ shaped cold pool encircled by a converging boundary forms to the north of Baramati due to precipitation behind the moisture convergence line with strong updrafts (~15 ms−1) leading to convective clouds extending up to ~ 8 km in a narrow region of ~ 30 km. The outflows from the convective clouds merge with the opposing southerly or southwesterly winds from the Arabian Sea and southerly or southeasterly winds from the Bay of Bengal resulting in moisture convergence (maximum 80 × 10−3 g kg−1 s−1). The vertical profile of the area-averaged moisture convergence over the cold pool shows strong convergence above 850 hPa and divergence near the surface indicating elevated convection. Radar reflectivity (50–60 dBZ) and vertical component of vorticity maximum (~0.01–0.14 s−1) are observed along the convergence zone. Stratiform clouds ahead of the squall line and parallel wind flow at 850 hPa and nearly perpendicular flow at higher levels relative to squall line as evidenced by relatively low and wide-spread reflectivity suggests that organizational mode of squall line may be categorized as ‘Mixed Mode’ type where northern part can be a parallel stratiform while the southern part resembles with a leading stratiform. Simulated rainfall (grid scale 27 km) leads the observed rainfall by 1 h while its magnitude is ~2 times of the observed rainfall (grid scale ~100 km) derived from Kalpana-1. Thus, this study indicates that under synoptically favorable conditions, WRF-ARW could simulate thunderstorm evolution reasonably well although there is some space–time error which might, perhaps, be the reason for lower CAPE (observed by upper air sounding) on the simulation day.

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References

  • Agnihotri G, Dimri AP (2015a) Vertical structure of atmosphere in pre-monsoon season over Bangalore. J Earth Syst Sci 124:1563–1572. doi:10.1007/s12040-015-0612-7

    Article  Google Scholar 

  • Agnihotri G, Dimri AP (2015b) Vertical structure of atmosphere in pre-monsoon season over Banglore. J Earth Syst Sci 124(7):1563–1572

    Article  Google Scholar 

  • Anderson ME, Carey LD, Petersen WA, Knupp KR (2011) C-band dual-polarimetric radar signatures of hail. Electron J Operational Meteor 12(2):1–30

    Google Scholar 

  • Banacos PC, Schultz DM (2005) The use of moisture flux convergence in forecasting convective initiation: historical and operational perspectives. Weather Forecast 20:351–366. doi:10.1175/WAF858.1

    Article  Google Scholar 

  • Bothwell PD (1988) Forecasting convection with the AFOS Data Analysis Programs (ADAP-VERSION 2.0). NOAA Technical Memorandum NWS SR-122, NOAA/NWS Southern Region, Fort Worth

  • Ceperuelo M, Llasat MC, Rigo T (2006) Rainfall events and Hailstorms Analysis Program (RHAP). Adv Geosci 7(205–213):2006

    Google Scholar 

  • Chatterjee RN, Prakash P, Singh G (1995) Frequency of thunderstorm occurrence and their height distribution in different regions in India—a radar study. Vayu Mandal J Ind Meteorol Soc 25:41–46

    Google Scholar 

  • Chaudhuri S (2008) Preferred type of cloud in the genesis of severe thunderstorms—a soft computing approach. Atmos Res 88:149–156

    Article  Google Scholar 

  • Chevuturi A, Dimri AP (2015) Inter-comparison of physical processes associated with winter and non-winter hailstorms using the Weather Research and Forecasting (WRF) model. Model Earth Syst Environ. doi:10.1007/s40808-015-0014-5

    Google Scholar 

  • Colman BR (1990a) Thunderstorms above frontal surfaces in environments without positive CAPE. Part I: a climatology. Mon Weather Rev 118:1103–1121

    Article  Google Scholar 

  • Colman BR (1990b) Thunderstorms above frontal surfaces in environments without positive CAPE. Part II: organization and instability mechanisms. Mon Weather Rev 118:1123–1144

    Article  Google Scholar 

  • Dalal S, Lohar D, Sarkar S, Sadhukhan I, Debnath GC (2012) Organizational modes of squall-type mesoscale convective systems during premonsoon season over eastern India. Atmos Res 106:120–138

    Article  Google Scholar 

  • Dimri AP, Niyogi D, Barros AP, Ridley J, Mohanty UC, Yasunari T, Sikka DR (2015) Western disturbance: a review. Rev Geophys. doi:10.1002/2014RG000460

    Google Scholar 

  • Doswell CA III (1982) The operational meteorology of convective weather, volume 1; Operational mesoanalysis, NOAA Technical Memorandum NWS heavy rainfall over the central United States. Weather Forecast 18:861–878

    Google Scholar 

  • Dudhia J (1989) Numerical study of convection observed during the winter monsoon experiment using a mesoscale two-dimensional model. J Atmos Sci 46:3077–3107

    Article  Google Scholar 

  • Gilleland E, Ahijevych DA, Brown BG, Ebert EE (2010) Verifying forecasts spatially. Bull Am Soc 91:1365–1373

    Article  Google Scholar 

  • Hirt WD (1982) Short-term prediction of convective development using dew-point convergence. In: Ninth conference on weather forecasting and analysis, Seattle. Amer. Meteor. Soc, pp 201–205 (preprints)

  • Houze RA Jr (1993) Cloud dynamics. Academic Press, New York

    Google Scholar 

  • Houze RA Jr (2012) Orographic effects on precipitating clouds. Rev Geophys 50:RG1001. doi:10.1029/2011RG000365

    Article  Google Scholar 

  • Hudson HR (1971) On the relationship between horizontal moisture convergence and convective cloud formation. J Appl Meteorol 10:755–762

    Article  Google Scholar 

  • Koteswaram P, Srinivasan V (1958) Thunderstorms over Gangetic West Bengal in the pre-monsoon season and the synoptic factors favorable for their formation. Ind J Meteorol Geophys 9:301–312

    Google Scholar 

  • Kulkarni JR, Morwal SB, Narkhedkar SG, Maheskumar RS, Padmakumari B, Sunitha Devi S, Rajeevan M (2015) Unprecedented hailstorms over north peninsular India during February–March 2014. J Geophys Res Atmos. doi:10.1002/2015JD023093

    Google Scholar 

  • Litta AJ, Mohanty UC (2008) Simulation of a severe thunderstorm event during the field experiment of STORM programme 2006, using WRFNMM model. Curr Sci 95(2):204–215

    Google Scholar 

  • Madala S, Satyanarayana ANV, Narayana Rao T (2014) Performance evaluation of PBL and cumulus parameterization schemes of WRF ARW model in simulating severe thunderstorm events over Gadanki MST radar facility—case study. Atmos Res 139:1–17. doi:10.1016/j.atmosres.2013.12.017

    Article  Google Scholar 

  • Mlawer EJ, Taubman SJ, Brown PD, Iacano MJ, Clough SA (1997) Radiative transfer for inhomogeneous atmosphere: RRTM, a validate correlated-k model for the longwave. J Geophys Res 102:16663–16682

    Article  Google Scholar 

  • Moore JT, Glass FH, Graves CE, Rochette SM, Singer MJ (2003) The environment of warm season elevated thunderstorms associated with heavy rainfall over the central United States. Weather Forecast 18:861–878

    Article  Google Scholar 

  • Morrison H, Thompson G, Tatarskii V (2009) Impact of cloud microphysics on the development of trailing stratiform precipitation in a simulated squall line: comparison of one and two-moment schemes. Mon Weather Rev 137:991–1006

    Article  Google Scholar 

  • Murthy BS, Latha R, Sreeja P (2013) Boundary layer jet on the lee side of Western Ghats during southwest monsoon as revealed by high resolution solar winds. J Atmos Solar Terrest Phys. doi:10.1016/j.jastp.2013.09.002

    Google Scholar 

  • Newman WR (1971) The relationship between horizontal moisture convergence and severe storm occurrences. M.S. thesis, School of Meteorology, University of Oklahoma. Available from School of Meteorology, University of Oklahoma, 100 E. Boyd, Rm. 1310, Norman, OK 73019

  • Parker MD, Johnson RH (2000) Organizational modes of midlatitude mesoscale convective systems. Mon Weather Rev 128:3413–3436

    Article  Google Scholar 

  • Parker MD, Johnson RH (2004) Simulated convective lines with leading precipitation. Part II: evolution and maintenance. J Atmos Sci 61:1656–1673

    Article  Google Scholar 

  • Poljack G, Prtenjak MT, Kvakić M, Strelec Mahović N, Babić K (2014) Wind patterns associated with the development of daytime thunderstorms over Istria. Ann Geophys 32(401–420):2014. doi:10.5194/angeo-32-401-2014

    Google Scholar 

  • Rajeevan M, Kesarkar A, Thampi SB, Rao TN, Radhakrishna B, Rajasekhar M (2010) Sensitivity of WRF cloud microphysics to simulations of a severe thunderstorm event over Southeast India. Ann Geophys 28:603–619

    Article  Google Scholar 

  • Sadhukhan I, Lohar D, Pal DK (2000) Premonsoon season rainfall variability over Gangetic West Bengal and its neighbourhood, India. Int J Climatol 20:1485–1493

    Article  Google Scholar 

  • Singh H, Singh OP (2013) Satellite derived precipitation estimates over Indian region during southwest monsoons. J Ind Geophys Union 17:65–74

    Google Scholar 

  • Smolarkiewicz PK, Rotunno R (1989) Low Froude number flow past three dimensional obstacles: part I. Baroclinically generated lee vortices. J Atmos Sci 46:1154–1164. doi:10.1175/1520-0469

    Article  Google Scholar 

  • Srinivasan V, Ramamurthy K, Nene YR (1973) Summer-Nor’westers and Andhis and large scale convective activity over peninsular and central parts of the country. IMD Forecasting Manual, FMU Rep. No. III-2.2, Discussion of typical synoptic weather situations

  • Tyagi B, Satyanarayana ANV, Vissa NK (2013) Thermodynamical structure of atmosphere during pre-monsoon thunderstorm season over Kharagpur as revealed by STORM data. Pure Appl Geophys 170:675–687

    Article  Google Scholar 

  • Waldstreicher JS (1989) A guide to utilizing moisture flux convergence as a predictor of convection. Nat Weather Dig 14(4):20–35

    Google Scholar 

  • Wang D, Miao J, Tan Z (2013) Impacts of topography and land cover change on thunderstorm over the Huangshan (Yellow Mountain) area of China. Nat Hazards 67:675–699. doi:10.1007/s11069-013-0595-0

    Article  Google Scholar 

  • Wang D, Miao J, Zhang D (2015) Numerical simulations of local circulation and its response to land cover changes over the Yellow Mountains of China. J Meteorol Res 29:667–681. doi:10.1007/s13351-015-4070-6

    Article  Google Scholar 

  • Weston KJ (1972) The dryline of northern India and its role in cumulonimbus convection. Q J R Meteorol Soc 98:519–531

    Article  Google Scholar 

Download references

Acknowledgements

The authors would like to thank India Meteorological Department for providing daily weather reports and Kalpana-1 rainfall. NCEP/NCAR is thankfully acknowledged for reanalysis charts. QPE and OLR images were obtained from ISRO’s MOSDAC site.

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Authors and Affiliations

  1. Indian Institute of Tropical Meteorology, Dr Homi Bhabha Road, Pune, 411008, India

    B. S. Murthy, R. Latha & H. Madhuparna

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  1. B. S. Murthy
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  2. R. Latha
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  3. H. Madhuparna
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Correspondence to B. S. Murthy.

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Responsible Editor: J.-F. Miao.

Electronic supplementary material

Below is the link to the electronic supplementary material.

Time evolution of various parameters at every 30 min interval is explained with figures (referred as SFigure or SFig) provided in ‘supplementary material’. Important figures illustrating convection initiation and its peak stage just before precipitation only are given in the main paper.

Supplementary material 1 (DOCX 935 kb)

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Murthy, B.S., Latha, R. & Madhuparna, H. WRF simulation of a severe hailstorm over Baramati: a study into the space–time evolution. Meteorol Atmos Phys 130, 153–167 (2018). https://doi.org/10.1007/s00703-017-0516-y

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