Abstract
There are increasing efforts towards the prediction of high-impact weather systems and understanding of related dynamical and physical processes. High-resolution numerical model simulations can be used directly to model the impact at fine-scale details. Improvement in forecast accuracy can help in disaster management planning and execution. National Centre for Medium Range Weather Forecasting (NCMRWF) has implemented high-resolution regional unified modeling system with explicit convection embedded within coarser resolution global model with parameterized convection. The models configurations are based on UK Met Office unified seamless modeling system. Recent land use/land cover data (2012–2013) obtained from Indian Space Research Organisation (ISRO) are also used in model simulations. Results based on short-range forecast of both the global and regional models over India for a month indicate that convection-permitting simulations by the high-resolution regional model is able to reduce the dry bias over southern parts of West Coast and monsoon trough zone with more intense rainfall mainly towards northern parts of monsoon trough zone. Regional model with explicit convection has significantly improved the phase of the diurnal cycle of rainfall as compared to the global model. Results from two monsoon depression cases during study period show substantial improvement in details of rainfall pattern. Many categories in rainfall defined for operational forecast purposes by Indian forecasters are also well represented in case of convection-permitting high-resolution simulations. For the statistics of number of days within a range of rain categories between ‘No-Rain’ and ‘Heavy Rain’, the regional model is outperforming the global model in all the ranges. In the very heavy and extremely heavy categories, the regional simulations show overestimation of rainfall days. Global model with parameterized convection have tendency to overestimate the light rainfall days and underestimate the heavy rain days compared to the observation data.
Similar content being viewed by others
References
Baldauf, M., Seifert, A., Förstner, J., Majewski, D., Raschendorfer, M., & Reinhardt, T. (2011). Operational convective-scale numerical weather prediction with the COSMO model: description and sensitivities. Monthly Weather Review. https://doi.org/10.1175/MWR-D-10-05013.1.
Best, M. J., Pryor, M., Clark, D. B., Rooney, G. G., Essery, R. L. H., Ménard, C. B., et al. (2011). The joint UK land environment simulator (JULES), model description—part 1: Energy and water fluxes. Geoscientific Model Development, 4, 677–699.
Betts, A. K., & Jakob, C. (2002). Evaluation of the diurnal cycle of precipitation, surface thermodynamics, and surface fluxes in the ECMWF model using LBA data. Journal of Geophysical Research. https://doi.org/10.1029/2001JD000427.
Birch, C. E., Parker, D. J., Marsham, J. H., Copsey, D., & Garcia-Carreras, L. (2014). A seamless assessment of the role of convection in the water cycle of the West African monsoon. Journal of Geophysical Research Atmospheres, 119, 2890–2912. https://doi.org/10.1002/2013JD020887.
Birch, C. E., Roberts, M. J., Garcia-Carreras, L., Ackerley, D., Reeder, M. J., Lock, A. P., et al. (2015). Sea-breeze dynamics and convection initiation: The influence of convective parameterization in weather and climate model biases. Journal of Climate, 28, 8093–8108. https://doi.org/10.1175/JCLI-D-14-00850.1.
Biswadip, G. (2014). IRS-P6 AWiFS derived gridded land use/land cover data compatible to mesoscale models (MM5 and WRF) over Indian region. NRSC Technical Documentation, No. NRSC-ECSA-ACSGOCT-2014-TR-651, pp. 1–11.
Brown, A., Milton, S., Cullen, M., Golding, B., Mitchell, J., & Shelly, A. (2012). Unified modeling and prediction of weather and climate: A 25-year journey. Bulletin of the American Meteorological Society, 93, 1865–1877.
Bryan, G. H., Wyngaard, J. C., & Fritsch, J. M. (2003). Resolution requirements for the simulation of deep moist convection. Monthly Weather Review, 131, 2394–2416.
Clark, A. J., Gallus, W. A., Jr., & Weisman, M. L. (2010). Neighborhood-based verification of precipitation forecasts from convection-allowing NCAR WRF Model simulations and the operational NAM. Weather and Forecasting, 25, 1495–1509. https://doi.org/10.1175/2010WAF2222404.1.
Clark, D. B., Mercado, L. M., Sitch, S., Jones, C. D., Gedney, N., Best, M. J., et al. (2011). The joint UK land environment simulator (JULES), model description—part 2: Carbon fluxes and vegetation dynamics. Geoscientific Model Development, 4, 701–722.
Dai, A. (2006). Precipitation characteristics in eighteen coupled climate models. Journal of Climate, 19, 4605–4630. https://doi.org/10.1175/JCLI3884.1.
Dash, S. K., Ashu, Mamgain, Pattnayak, K. C., & Giorgi, F. (2013). Spatial and temporal variations in Indian summer monsoon rainfall and temperature: An analysis based on RegCM3 simulations. Pure and Applied Geophysics, 170(4), 655–674.
Dash, S. K., Pattnayak, K. C., Panda, S. K., Vaddi, Deepika, & Mamgain, Ashu. (2015). Impact of domain size on the simulation of Indian summer monsoon in RegCM4 using mixed convection scheme and driven by HadGEM2. Climate Dynamics, 44, 961. https://doi.org/10.1007/s00382-014-2420-1.
Dash, S. K., Shekher, M. S., Singh, G. P., & Vernekar, A. D. (2002). Relationship between surface fields over Indian Ocean and monsoon rainfall over homogeneous zones of India. Mausam, 53, 133–144.
De, U. S., Dube, R. K., & Prakasa Rao, G. S. (2005). Extreme weather events over India in the last 100 years. Journal of Indian Geophysics Union, 9(3), 173–187.
Dirmeyer, P. A., Cash, B. A., Kinter, J. L., III, Jung, T., Marx, L., SatohM, Stan C., et al. (2012). Simulating the diurnal cycle of rainfall in global climate models: Resolution versus parameterization. Climate Dynamics, 39, 399–418. https://doi.org/10.1007/s00382-011-1127-9.
Essery, R. L. H., Best, M. J., Betts, R. A., Cox, P. M., & Taylor, C. M. (2003). Explicit representation of subgrid heterogeneity in a GCM land surface scheme. Journal of Hydrometeorology, 4, 530–543. https://doi.org/10.1175/1525-7541(2003)004<0530:EROSHI>2.0.CO;2.
George, J. P., Indira Rani, S., Jayakumar, A., Mohandas, S., Mallick, S., Lodh, A., Rakhi, R., Sreevathsa, M. N. R., & Rajagopal, E. N. (2016). NCUM data assimilation system. Monsoon Report, NMRF/TR/01/2016.
GEWEX Cloud System Science Team. (1993). The GEWEX cloud system study (GCSS). Bulletin of the American Meteorological Society, 74, 387–399. https://doi.org/10.1175/1520-0477(1993)074<0387:TGCSS>2.0.CO;2.
Goswami, B. N., Venugopal, V., Sengupta, D., Madhusoodanan, M. S., & Xavier Prince, K. (2006). Increasing trend of extreme rain events over India in a warming environment. Science, 314, 1442–1445.
Gregory, D., & Rowntree, P. R. (1990). A mass flux convection scheme with representation of cloud ensemble characteristics and stability-dependent closure. Monthly Weather Review, 118(7), 1483–1506. https://doi.org/10.1175/1520-0493(1990)118<1483:AMFCSW>2.0.CO;2.
Guichard, F., Petch, J. C., Redelsperger, J.-L., Bechtold, P., Chaboureau, J. P., Cheinet, S., et al. (2004). Modelling the diurnal cycle of deep precipitating convection over land with cloud-resolving models and single-column models. Quarterly Journal of the Royal Meteorological Society, 130(604C), 3139–3172.
Halder, M., Hazra, A., Mukhopadhyay, P., & Siingh, D. (2015). Effect of the better representation of the cloud ice-nucleation in WRF microphysics schemes: A case study of a severe storm in India. Atmospheric Research, 154, 155–174.
Hastings, D. A., & Dunbar, P. K. (1999). Global land one-kilometer base elevation (GLOBE) digital elevation model, documentation (Vol. 1). Boulder: National Oceanic and Atmospheric Administration (NOAA), National Geophysical Data Center.
Hohenegger, C., Brockhaus, P., & Schär, C. (2008). Towards climate simulations at convection permitting scales. Meteorologische Zeitschrift, 17, 383–394.
Holloway, C. E., Woolnough, S. J., & Lister, G. M. S. (2012). Precipitation distributions for explicit versus parametrized convection in a large-domain high-resolution tropical case study. Quarterly Journal of the Royal Meteorological Society, 138, 1692–1708. https://doi.org/10.1002/qj.1903.
Hou, A. Y., Kakar, R. K., Neeck, S., Azarbarzin, A. A., Kummerow, C. D., Kojima, M., et al. (2014). The global precipitation measurement mission. Bulletin of the American Meteorological Society, 95, 701–722. https://doi.org/10.1175/BAMS-D-13-00164.1.
Huffman, G. (2015). GPM L3 IMERG Final 1 month 0.1 degree × 0.1 degree precipitation. Greenbelt: Goddard Earth Sciences Data and Information Services Center (GES DISC). https://doi.org/10.5067/gpm/imerg/month/3b.
Janjic, Z. I., Black, T. L., Pyle, M., Chuang, H. Y., Rogers, E., & DiMego, G. (2007). An evolutionary approach to nonhydrostatic modeling. Retrieved from http://www.Wrfmodel.org/wrfadmin/publications/Chuang_Janjic_NWP50yearsfinalshort.pdf.
Jeong, J. H., Song, S. K., Lee, H. W., & Kim, Y. K. (2012). Effects of high-resolution land cover and topography on local circulations in two different coastal regions of Korea: a numerical modeling study. Meteorology and Atmospheric Physics, 118(1–2), 1–20.
Kain, J. S., Weiss, S. J., Bright, D. R., Baldwin, M. E., Levit, J. J., Carbin, G. W., et al. (2008). Some practical considerations regarding horizontal resolution in the first generation of operational convection allowing NWP. Weather and Forecasting, 23, 931–952.
Kumar, A., Chen, F., Barlage, M., Ek, M. B., & Niyogi, D. (2014). Assessing impacts of integrating MODIS vegetation data in the weather research and forecasting (WRF) model coupled to two different canopy-resistance approaches. Journal of Applied Meteorology and Climatology, 53(6), 1362–1380.
Larson, V. E., Schanen, D. P., Wang, M., Ovchinnikov, M., & Ghan, S. (2012). PDF parameterization of boundary layer clouds in models with horizontal grid spacings from 2 to 16 km. Monthly Weather Review, 140, 285–306.
Lean, H. W., Clark, P. A., Dixon, M., Roberts, N. M., Fitch, A., Forbes, R., et al. (2008). Characteristics of high-resolution versions of the Met Office unified model for forecasting convection over the United Kingdom. Monthly Weather Review, 136, 3408–3424.
Litta, A. J., Mohanty, U. C., Das, S., & Idicula, S. M. (2012). Numerical simulation of severe local storms over east India using WRF-NMM mesoscale model. Atmospheric Research, 116, 161–184.
Liu, C., & Moncrieff, M. W. (2007). Sensitivity of cloud-resolving simulations of warm-season convection to cloud microphysics parameterizations. Monthly Weather Review, 135, 2854–2868.
Lock, A. P., Brown, A. R., Bush, M. R., Martin, G. M., & Smith, R. N. B. (2000). A new boundary layer mixing scheme. Part I: Scheme description and single-column model tests. Monthly Weather Review, 128, 3187–3199. https://doi.org/10.1175/1520-0493(2000)128<3187:ANBLMS>2.0.CO;2.
Love, B. S., Matthews, A. J., & Lister, G. M. S. (2011). The diurnal cycle of precipitation over the Maritime Continent in a high-resolution atmospheric model. Quarterly Journal of the Royal Meteorological Society, 137, 934–947. https://doi.org/10.1002/qj.809.
Mamgain, A., Unnikrishnan, C. K., & Rajagopal, E. N. (2016). Recent land use/land cover changes and their impact on the evolution and structure of thunderstorm in New Delhi, Proceedings SPIE 9882, Remote Sensing and Modeling of the Atmosphere, Oceans, and Interactions (Vol. 9882, p. 98820), May 3, 2016. https://doi.org/10.1117/12.2223602.
Mandke, S., Sahai, A. K., Shinde, M. A., Joseph, Susmitha, & Chattopadhyay, R. (2007). Simulated changes in active/break spells during the Indian summer monsoon due to enhanced CO2 concentrations: Assessment from selected coupled atmosphere–ocean global climate models. International Journal of Climatology, 27, 837–859.
Marsham, J. H., Dixon, N. S., Garcia-Carreras, L., Lister, G. M. S., Parker, D. J., Knippertz, P., et al. (2013). The role of moist convection in the West African monsoon system: Insights from continental-scale convection-permitting simulations. Geophysical Research Letters, 40, 1843–1849. https://doi.org/10.1002/grl.50347.
Mitra, A. K., Rajagopal, E. N., Iyengar, G. R., Mahapatra, D. K., Momin, I. M., Gera, A., et al. (2013). Prediction of monsoon using a seamless coupled modelling system. Current Science, 104(10), 1369–1379.
Murakami, T., Nakazawa, T., & He, T. (1984). On the 40–50 day oscillation during the 1979 northern hemisphere summer. Part II: Heat and moisture budget. Journal of the Meteorological Society of Japan, 62, 469–484.
Pearson, K. J., Lister, G. M. S., Birch, C. E., Allan, R. P., Hogan, R. J., & Woolnough, S. T. (2014). Modelling the diurnal cycle of tropical convection across the ‘grey zone’. Quarterly Journal of the Royal Meteorological Society, 140, 491–499. https://doi.org/10.1002/qj.2145.
Petch, J. C. (2006). Sensitivity studies of developing convection in a cloud-resolving model. Quarterly Journal of the Royal Meteorological Society, 132, 345–358.
Prakash, S., Mitra, A. K., Pai, D. S., & AghaKouchak, A. (2016). From TRMM to GPM: How well can heavy rainfall be detected from space? Advances in Water Resources. https://doi.org/10.1016/j.advwatres.2015.11.008.
Rajeevan, M., Kesarkar, A., Thampi, S. B., Rao, T. N., Radhakrishna, B., & Rajasekhar, M. (2010). Sensitivity of WRF cloud microphysics to simulations of a severe thunderstorm event over Southeast India. Annales Geophysicae, 28, 603–619. https://doi.org/10.5194/angeo-28-603-2010.
Randall, D., Khairoutdinov, M., Arakawa, A., & Grabowski, W. (2003). Breaking the cloud parameterization deadlock. Bulletin of the American Meteorological Society, 84, 1547–1564. https://doi.org/10.1175/BAMS-84-11-1547.
Saito, K., Fujita, T., Yamada, Y., Ishida, J.-I., Kumagai, Y., Aranami, K., et al. (2006). The operational JMA nonhydrostatic mesoscale model. Monthly Weather Review, 134, 1266–1298.
Sato, T., Miura, H., Satoh, M., Takayabu, Y. N., & Wang, Y. (2009). Diurnal cycle of precipitation in the tropics simulated in a global cloud-resolving model. Journal of Climate, 22(18), 4809–4826. https://doi.org/10.1175/2009JCLI2890.1.
Schwartz, C. S. (2016). Improving large-domain convection-allowing forecasts with high-resolution analyses and ensemble data assimilation. Monthly Weather Review, 144(5), 1777–1803.
Sikka, D. R. (1977). Some aspects of the life history, structure and movement of monsoon depressions. Pure and Applied Geophysics, 115, 1501–1529.
Smith, S. A., Vosper, S. B., & Field, P. R. (2015). Sensitivity of orographic precipitation enhancement to horizontal resolution in the operational Met Office Weather forecasts. Meteorological Applications. https://doi.org/10.1002/met.1352.
Tao, W. K., & Moncrieff, M. W. (2009). Multiscale cloud system modeling. Reviews of Geophysics. https://doi.org/10.1029/2008rg000276.
Trenberth, K. E., Dai, A., Rasmussen, R. M., & Parsons, D. B. (2003). The changing character of precipitation. Bulletin of the American Meteorological Society, 84, 1205–1217.
Turner, A. G., & Slingo, J. M. (2009). Subseasonal extremes of precipitation and active-break cycles of the Indian summer monsoon in a climate-change scenario. Quarterly Journal of the Royal Meteorological Society, 135, 549–567.
Unnikrishnan, C. K., Biswadip, G., Mohandas, S., Mamgain, A., Rajagopal, E. N., Iyengar, G. R., et al. (2016). Recent changes on land use/land cover over Indian region and its impact on the weather prediction using Unified model. Atmospheric Science Letters, 17, 1–7.
Walters, D., Boutle, I., Brooks, M., Thomas, M., Stratton, R., Vosper, S., et al. (2017). The Met Office unified model global atmosphere 6.0/6.1 and JULES global land 6.0/6.1 configurations. Geoscientific Model Development, 10(4), 1487. https://doi.org/10.5194/gmd-2016-194.
Webster, S., Chan, S., Hassim, M. E., Kendon, E., Marzin, C., Sahany, S., & Scannell, C. (2015). Convective-scale modelling. Singapore’s second national climate change study: Climate projections to 2100, Meteorological Service Singapore Rep., pp. 1–21. Retrieved from http://ccrs.weather.gov.sg/wp-content/uploads/2015/07/V2_Ch6_Convective_Scale_Modelling.pdf.
Webster, P. J., Magana, V. O., Palmer, T. N., Shukla, J., Tomas, R. A., Yanai, M. U., et al. (1998). Monsoons: Processes, predictability, and the prospects for prediction. Journal of Geophysical Research Oceans, 103, 14451–14510.
Weisman, M. L., Davis, C. A., Wang, W., Manning, K. W., & Klemp, J. B. (2008). Experiences with 0–36 h explicit convective forecasts with the WRF-ARW model. Weather and Forecasting, 23, 407–437. https://doi.org/10.1175/2007WAF2007005.1.
Weisman, M. L., Skamarock, W. C., & Klemp, J. B. (1997). The resolution dependence of explicitly modeled convective systems. Monthly Weather Review, 125, 527–548.
Willetts, P. D., Marsham, J. H., Birch, C. E., Parker, D. J., Webster, S., & Petch, J. (2017). Moist convection and its upscale effects in simulations of the Indian monsoon with explicit and parametrised convection. Quarterly Journal of the Royal Meteorological Society, 143, 1073–1085. https://doi.org/10.1002/qj.2991.
Wilson, D. R., & Ballard, S. P. (1999). A microphysically based precipitation scheme for the UK Meteorological Office unified model. Quarterly Journal of the Royal Meteorological Society, 125(557), 1607–1636. https://doi.org/10.1002/qj.49712555707.
Wood, N., Staniforth, A., White, A., Allen, T., Diamantakis, M., Gross, M., et al. (2014). An inherently mass-conserving semi-implicit semi-Lagrangian discretization of the deep-atmosphere global non-hydrostatic equations. Quarterly Journal of the Royal Meteorological Society, 140, 1505–1520. https://doi.org/10.1002/qj.2235.
Yang, G. Y., & Slingo, J. (2001). The diurnal cycle in the tropics. Monthly Weather Review, 129, 784–801.
Acknowledgements
The authors would like to thank Director, NRSC/ISRO for Lu/Lc data. We acknowledge the NASA for the GPM IMERG data product. This study is a part of the MoES-NERC INCOMPASS project. Authors thank the anonymous reviewers for their constructive comments, which helped us to improve the manuscript.
Author information
Authors and Affiliations
Corresponding author
Electronic supplementary material
Below is the link to the electronic supplementary material.
Rights and permissions
About this article
Cite this article
Mamgain, A., Rajagopal, E.N., Mitra, A.K. et al. Short-Range Prediction of Monsoon Precipitation by NCMRWF Regional Unified Model with Explicit Convection. Pure Appl. Geophys. 175, 1197–1218 (2018). https://doi.org/10.1007/s00024-017-1754-0
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00024-017-1754-0