Abstract
Main objective of the present paper is to examine the role of various parameterization schemes in simulating the evolution of mesoscale convective system (MCS) occurred over south-east India. Using the Weather Research and Forecasting (WRF) model, numerical experiments are conducted by considering various planetary boundary layer, microphysics, and cumulus parameterization schemes. Performances of different schemes are evaluated by examining boundary layer, reflectivity, and precipitation features of MCS using ground-based and satellite observations. Among various physical parameterization schemes, Mellor–Yamada–Janjic (MYJ) boundary layer scheme is able to produce deep boundary layer height by simulating warm temperatures necessary for storm initiation; Thompson (THM) microphysics scheme is capable to simulate the reflectivity by reasonable distribution of different hydrometeors during various stages of system; Betts–Miller–Janjic (BMJ) cumulus scheme is able to capture the precipitation by proper representation of convective instability associated with MCS. Present analysis suggests that MYJ, a local turbulent kinetic energy boundary layer scheme, which accounts strong vertical mixing; THM, a six-class hybrid moment microphysics scheme, which considers number concentration along with mixing ratio of rain hydrometeors; and BMJ, a closure cumulus scheme, which adjusts thermodynamic profiles based on climatological profiles might have contributed for better performance of respective model simulations. Numerical simulation carried out using the above combination of schemes is able to capture storm initiation, propagation, surface variations, thermodynamic structure, and precipitation features reasonably well. This study clearly demonstrates that the simulation of MCS characteristics is highly sensitive to the choice of parameterization schemes.
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Abhilash S, Mohankumar K, Das S (2008) Simulation of microphysical structure associated with tropical cloud clusters using mesoscale model and comparison with TRMM observations. Int J Remote Sens 29:2411–2432
Arakawa A, Schubert WH (1974) Interaction of a cumulus cloud ensemble with the large-scale environment. Part I. J Atmos Sci 31:674–701
Betts AK, Miller MJ (1986) A new convective adjustment scheme. Part II: single column tests using GATE wave, BOMEX, ATEX and arctic airmass data sets. Q J Roy Meteor Soc 112:693–709
Chatterjee P, Pradhan D, De UK (2008) Simulation of hailstorm event using Mesoscale Model MM5 with modified cloud microphysics scheme. Ann Geophys 26:3545–3555
Cintineo R, Otkin JA, Xue M, Kong F (2014) Evaluating the performance of planetary boundary layer and cloud microphysical parameterization schemes in convection-permitting ensemble forecasts using synthetic GOES-13 satellite observations. Mon Weather Rev 142:163–182
Cohen AE, Cavallo SM, Coniglio MC, Brooks HE (2015) A review of planetary boundary layer parameterization schemes and their sensitivity in simulating Southeastern US cold season severe weather environments. Weather Forecast 30:591–612
Coniglio MC, Correia J Jr, Marsh PT, Kong F (2013) Verification of convection-allowing WRF model forecasts of the planetary boundary layer using sounding observations. Weather Forecast 28:842–862
Deb SK, Kishtawal CM, Bongirwar VS, Pal PK (2010) The simulation of heavy rainfall episode over Mumbai: impact of horizontal resolutions and cumulus parameterization schemes. Nat Hazards 52:117–142. doi:10.1007/s11069-009-9361-8
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
Dudhia J, Gill D, Manning K, Wang W, Bruyere C (2002) PSU/NCAR Mesoscale Modeling System (MM5 version 3) tutorial class notes and user’s guide. National Center for Atmospheric Research, Boulder, Colorado, USA
Dudhia J, Hong SY, Lim KS (2008) A new method for representing mixed-phase particle fall speeds in bulk microphysics parameterizations. J Meteorol Soc Jpn 86A:33–44
Fabry F (2006) The spatial variability of moisture in the boundary layer and its effect on convection initiation: project-long characterization. Mon Weather Rev 134:79–91
Fadnavis S, Deshpande M, Ghude SD, Raj PE (2014) Simulation of severe thunderstorm event: a case study over Pune, India. Nat Hazards 72:927–943
Ferreira JA, Carvalho AC, Carvalheiro L, Rocha A, Castanheira JM (2014) On the influence of physical parameterisations and domains configuration in the simulation of an extreme precipitation event. Dynam Atmos Oceans 68:35–55
Flaounas E, Bastin S, Janicot S (2011) Regional climate modelling of the 2006 West African monsoon: sensitivity to convection and planetary boundary layer parameterisation using WRF. Clim Dynam 36:1083–1105
Gilliland EK, Rowe CM (2007) A comparison of cumulus parameterization schemes in the WRF model. In: Proceedings of the 87th AMS Annual Meeting and 21th Conference on Hydrology (Vol. 2)
Grell GA, Devenyi D (2002) A generalized approach to parameterizing convection combining ensemble and data assimilation techniques. Geophys Res Lett 29:14
Hong SY, Pan HL (1996) Nonlocal boundary layer vertical diffusion in a medium-range forecast model. Mon Weather Rev 124:2322–2339
Hong SY, Dudhia J, Chen SH (2004) A revised approach to ice microphysical processes for the bulk parameterization of clouds and precipitation. Mon Weather Rev 132:103–120
Hong S, Noh Y, Dudhia J (2006) A new vertical diffusion package with an explicit treatment of entrainment processes. Mon Weather Rev 134:2318–2341. doi:10.1175/MWR3199.1
Hong SY, Sunny Lim KS, Kim JH, Jade Lim JO, Dudhia J (2009) Sensitivity study of cloud-resolving convective simulations with WRF using two bulk microphysical parameterizations: ice-phase microphysics versus sedimentation effects. J Appl Meteorol Clim 48:61–76
Hu Xiao-Ming, John W, Nielsen-Gammon Zhang F (2010) Evaluation of three planetary boundary layer schemes in the WRF model. J Appl Meteorol Clim 49:1831–1844
Hubbert JC, Dixon M, Ellis SM, Meymaris G (2009) Weather radar ground clutter. Part I: identification, modeling, and simulation. J Atmos Oceanic Technol 26:1165–1180
Janjić ZI (1994) The step-mountain Eta coordinate model: further developments of the convection, viscous sublayer, and turbulence closure schemes. Mon Weather Rev 122:927–945
Jankov I, Gallus WA Jr, Segal M, Shaw B, Koch SE (2005) The impact of different WRF model physical parameterizations and their interactions on warm season MCS rainfall. Weather Forecast 20:1048–1060
Kain JS (2004) The Kain–Fritsch convective parameterization: an update. J App Meteorol 43:170–181
Kain J, Fritsch M (1993) Convective parameterization for mesoscale models: The Kain– Fritsch scheme. In: Eaanual KA, Raymond DJ (eds) The Representation of Cumulus Convection in Numerical Models, Meteorological monographs, chap 16. American Meteorological Society, Boston, pp 165–170
Kain JS, Baldwin ME, Weiss SJ (2003) Parameterized updraft mass flux as a predictor of convective intensity. Weather Forecast 18:106–116
Krieger JR, Zhang J, Atkinson DE, Shulski MD, Zhang X (2009) Sensitivity of WRF model forecasts to different physical parameterizations in the Beaufort Sea region. Preprints, Eighth Conf. on Coastal Atmospheric and Oceanic Prediction and Processes, Phoenix, AZ, Amer Meteor Soc P1.2
Kumar RA, Dudhia J, Roy Bhowmik SK (2010) Evaluation of physics options of the Weather Research and Forecasting (WRF) Model to simulate high impact heavy rainfall events over Indian Monsoon region. Geofizika 27:101–125
Lin YL, Farley RD, Orville HD (1983) Bulk Parameterization of the snow field in a cloud model. J App Meteorol 22:1065–1092
Litta AJ, Mohanty UC (2008) Simulation of a severe thunderstorm event during the field experiment of STORM programme 2006, using WRF–NMM model. Curr Sci 95:204–215
Madala S, Satyanarayana AN, Srinivas CV, Tyagi B (2016) Performance evaluation of PBL schemes of ARW model in simulating thermo-dynamical structure of pre-monsoon convective episodes over kharagpur using STORM Data Sets. Pure appl Geophys 173:1803–1827
Madhulatha A, Rajeevan M, Venkat Ratnam M, Bhate J, Naidu CV (2013) Nowcasting severe convective activity over southeast India using ground-based microwave radiometer observations. J Geophys Res. doi:10.1029/2012JD018174
Melissa AG, Mullen SL (2005) Evaluation of QPF from a WRF ensemble system during the southwest monsoon. In: 6th WRF/15th MM5 users’ workshop, June (pp. 27-30)
Mellor GL, Yamada T (1982) Development of a turbulence closure model for geophysical fluid problems. Rev Geophys Space Phys 20:851–875
Mlawer EJ, Taubman SJ, Brown PD, Iacono MJ, Clough SA (1997) Radiative transfer for inhomogeneous atmosphere: RRTM, a validated correlated-k model for the longwave. J Geophys Res 102:16663–16682
Mohan M, Bhati S (2011) Analysis of WRF model performance over subtropical region of Delhi. Adv Meteorol, India. doi:10.1155/2011/621235
Mohan TS, Rao TN (2012) Variability of the thermal structure of the atmosphere during wet and dry spells over southeast India. Q J Roy Meteor Soc 138:1839–1851
Morrison H, Milbrandt J (2011) Comparison of two-moment bulk microphysics schemes in idealized supercell thunderstorm simulations. Mon Weather Rev 139:1103–1130
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 137:991–1007
Mukhopadhyay P, Taraphdar S, Goswami BN (2011) Influence of moist processes on track and intensitybforecast of cyclones over the north Indian Ocean. Geophys Res 116:D05116. doi:10.1029/2010JD014700
Nakanishi M, Niino H (2004) An improved Mellor–Yamada level- 3 model with condensation physics: its design and verification. Bound-Lay Meteorol 112:1–31
Okamoto K, Iguchi T, Takahashi N, Iwanami K, Ushio T (2005) The Global Satellite Mapping of Precipitaion (GSMaP) project. In: 25th IGARSS Proceeding, pp 3414–3416
Otkin J, Huang HL, Seifert A (2006) A comparison of microphysical schemes in the WRF model during a severe weather event. In Papers delivered at 7th WRF Users’ Workshop, Boulder, CO, USA, pp. 19–22
Pattanayak S, Mohanty UC (2008) A comparative study on performance of MM5 and WRF models in simulation of tropical cyclones over Indian seas. Curr Sci 95:923–936
Pennelly C, Reuter G, Flesch T (2014) Verification of the WRF model for simulating heavy precipitation in Alberta. Atmos Res 135–136:172–192
Pleim JE (2007) A combined local and nonlocal closure model for the atmospheric boundary layer. Part II: application and evaluation in a mesoscale meteorological model. J Appl Meteor Climatol 46:1396–1409
Pleim JE, Chang JS (1992) A non-local closure model for vertical mixing in the convective boundary layer. Atmos Environ 26A:965–981
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 south-east India. Ann Geophys 28:603–619
Rama Rao YV, Hatwar HR, Salah AK, Sudhakar Y (2007) An experiment using the high resolution Eta and WRF models to forecast heavy precipitation over India. Pure Appl Geophys 164:1593–1615
Rao DVB, Prasad DH (2007) Sensitivity of tropical cyclone intensification to boundary layer and convective processes. Nat Hazards 41:429–445
Ruiz Juan J, Celeste S, Julia NP (2010) WRF Model sensitivity to choice of parameterization over South America: validation against Surface Variables. Mon Weather Rev 138:3342–3355
Rutledge SA, Hobbs PV (1984) The mesoscale and microscale structure and organization of clouds and precipitation in midlatitude cyclones. XII: a diagnostic modeling study of precipitation development in narrow cold-frontal rainbands. J Atmos Sci 41:2949–2972
Shin HH, Hong SY (2011) Intercomparison of planetary boundary-layer parametrizations in the WRF model for a single day from CASES-99. Bound-Layer Meteorol 139:261–281
Skamarock W, Klemp JB, Dudhia J, Gill D, Barker D, Duda M, Huang X, Wang, Powers J (2008) A description of the advanced research WRF version 3. NCAR Technical Note, NCAR/TN\u2013475+STR, p 123
Stoelinga MT, Woods CP, Locatelli JD, Hobbs PV (2005) On the representation of snow in bulk microphysical parameterization schemes. Preprints, Joint WRF/MM5 Users’ Workshop, Boulder,Colorado, June 2005. NCAR Mesocale and Microscale Meteorology Division
Stull RB (1988) An introduction to boundary layer meteorology. Kluwer Academic Publishers, Dordrecht
Stull RB, Driedonks AGM (1987) Applications of the transilient turbulence parameterization to atmospheric boundary-layer simulations. Bound-Lay Meteorol 40:209–239
Thompson G, Rasmussen RM, Manning K (2004) Explicit forecasts of winter precipitation using an improved bulk microphysics scheme. Part I: description and sensitivity analysis. Mon Weather Rev 132:519–542
Thompson G, Field PR, Rasmussen RM, Hall WD (2008) Explicit forecasts of winter precipitation using an improved bulk microphysics scheme. Part II: implementation of a new snow parameterization. Mon Weather Rev 136:5095–5115
Vaidya SS, Kulkarni JR (2007) Simulation of heavy precipitation over Santacruz, Mumbai on 26 July 2005, using mesoscale model. Meteorol Atmos Phys 98:55–66
Wang W, Seaman LN (1996) A comparison study of convective parameterization schemes in a Mesoscale model. Mon Weather Rev 125:252–278
Weverberg VK, Vogelmann MA, Lin W, Luke PE, Cialella A, Minnis P, Khaiyer M, Boer ER, Jensen PM (2012) The role of cloud microphysics parameterization in the simulation of mesoscale convective system clouds and precipitation in the tropical western pacific. J Atmos Sci 70:1104–1128
Wisse JSP, de Arellano JVG (2004) Analysis of the role of the planetary boundary layer schemes during a severe convective storm. Ann Geophys 22:1861–1874
Wu D, Dong X, Xi B, Feng Z, Kennedy A, Mullendore G, Gilmore M, Tao WK (2013) Impacts of microphysical scheme on convective and stratiform characteristics in two high precipitation squall line events. J Geophys Res Atmos 118:11119–11135 doi:10.1002/jgrd.50798
Acknowledgements
We are thankful to scientific data centers NCEP, GES DISC, JAXA, and ISRO. WRF USERS page is greatly acknowledged for making the WRF model freely accessible to the user community. This research was funded by National Atmospheric Research Laboratory (NARL) under the Junior Research Fellowship (JRF) program sponsored by Department of Space (DOS), India. The first author was funded to carry out her Ph.D. thesis work under this program. Authors gratefully acknowledge Dr A. Jayaraman, Director NARL for his support and encouragement in providing High Performance Computing facilities and necessary observations to carry out this work. Special thanks to Dr. S.B. Thampi of Doppler Weather Radar Division, India, Meteorological Department (IMD), Chennai, India for providing DWR data. The in situ observations and DWR data utilised in this study can be available on special request at http://www.narl.gov.in and http://www.imd.gov.in respectively. We would like to thank two anonymous reviewers and editor for their helpful suggestions.
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Madhulatha, A., Rajeevan, M. Impact of different parameterization schemes on simulation of mesoscale convective system over south-east India. Meteorol Atmos Phys 130, 49–65 (2018). https://doi.org/10.1007/s00703-017-0502-4
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DOI: https://doi.org/10.1007/s00703-017-0502-4