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Impact of domain size on the simulation of Indian summer monsoon in RegCM4 using mixed convection scheme and driven by HadGEM2

Impact of domain size on ISM simulations

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An Erratum to this article was published on 03 February 2015

Abstract

In this study, a smaller domain over India alone and a larger South Asia (SA) domain have been used in the Regional Climate Model version 4.2 (RegCM4.2) to examine the effect of the domain size on the Indian summer monsoon simulations. These simulations were carried out over a period of 36 years at 50 km horizontal resolution with the lateral boundary forcings of the UK Met Office Hadley Centre Global Circulation Model Version 2.0. Results show that the Indian summer monsoon rainfall is significantly reduced when the domain size for the model integration is reduced from SA to the Indian domain. In case of SA domain simulation, the Equitable Threat Scores have higher values in case of very light, light and moderate rainfall events than those in case of the Indian domain simulation. It is also found that the domain size of model integration has dominant impact on the simulated convective precipitation. The cross-equatorial flow and the Somali Jet are better represented in the SA simulation than those in the Indian domain simulation. The vertically integrated moisture flux over the Arabian Sea in the SA domain simulation is close to that in the NCEP/NCAR reanalysis while it is underestimated in the Indian domain simulation. It is important to note that when RegCM4.2 is integrated over the smaller Indian domain, the effects of the Himalayas and the moisture advection from the Indian seas are not properly represented in the model simulation and hence the monsoon circulation and associated rainfall are underestimated over India.

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References

  • Adler RF, Huffman GJ, Chang A, Ferraro R, Xie P, Janowiak J et al (2003) The version 2 global precipitation climatology project (GPCP) monthly precipitation analysis (1979–present). J Hydrometeorol 4:1147–1167

    Article  Google Scholar 

  • Anthes RA, Kuo Y-H, Hsie E-Y, Low-Nam S, Bettge TW (1989) Estimation of skill and uncertainty in regional numerical models. Q J R Meteorol Soc 115(488):763–806

    Article  Google Scholar 

  • Ashfaq M, Shi Y, Tung WW, Trapp RJ, Gao XJ, Pal JS, Diffenbaugh NS (2009) Suppression of south Asian summer monsoon precipitation in the 21st century. Geophys Res Lett 36:L01704. doi:10.1029/2008GL036500

    Google Scholar 

  • Bhaskaran B, Jones RG, Murphy JM, Noguer M (1996) Simulations of the Indian summer monsoon using a nested regional climate model: domain size experiments. Clim Dyn 12:573–587

    Article  Google Scholar 

  • Bhaskaran B, Ramachandran A, Jones R, Moufouma-Okia W (2012) Regional climate model applications on sub-regional scales over the Indian monsoon region: the role of domain size on downscaling uncertainty. J Geophys Res 117. ISSN: 0148-0227. doi:10.1029/2012JD017956

  • Browne NAK, Sylla MB (2012) Regional climate model sensitivity to domain size for the simulation of the West African monsoon rainfall. Int J Geophys, 625831. doi:10.1155/2012/625831

  • Collins WJ et al (2011) Development and evaluation of an earth-system model HadGEM2. Geosci Model Dev 4:997–1062

    Article  Google Scholar 

  • Dash SK, Shekhar MS, Singh GP (2006) Simulation of Indian summer monsoon circulation and rainfall using RegCM3. Theoret Appl Climatol 86(1–4):161–172

    Article  Google Scholar 

  • Dash SK, Sharma N, Pattnayak KC, Gao XJ, Shi Y (2012) Temperature and precipitation changes in the north-east India and their future projections. Global Planet Change 98–99:31–44

    Article  Google Scholar 

  • Dash SK, Mamgain A, Pattnayak KC, Giorgi F (2013) Spatial and temporal variations in Indian summer monsoon rainfall and temperature: an analysis based on RegCM3 simulations. Pure appl Geophys 170:655–674

    Article  Google Scholar 

  • Denis B, Laprise R, Caya D, Cote J (2002) Downscaling ability of one-way nested regional climate models: the Big-Brother Experiment. Clim Dyn 18:627–646

    Article  Google Scholar 

  • Denis B, Laprise R, Caya D (2003) Sensitivity of a regional climate model to the spatial resolution and temporal updating frequency of lateral boundary conditions. Clim Dyn 20:107–126

    Google Scholar 

  • Dickinson RE, Henderson-Sellers A, Kennedy PJ (1993) Biosphere-atmosphere transfer scheme (bats) version1e as coupled to the NCAR community climate model, Technical report, National Center for Atmospheric Research

  • Ding Y (2004) Seasonal march of the East-Asian summer monsoon. In: Chang CP (ed) East Asian Monsoon. World Scientific, Singapore, p 564

    Google Scholar 

  • Elguindi N, Bi XQ, Giorgi F et al (2011) Regional climatic model RegCM user mannual version 4.1. The Abdus Salam International Centre for Theoretical Physics Strada Costiera, Trieste

    Google Scholar 

  • Emanuel KA (1991) A scheme for representing cumulus convection in large-scale models. J Atmos Sci 48(21):2313–2335

    Article  Google Scholar 

  • Emanuel KA, Zivkovic-Rothman M (1999) Development and evaluation of a convection scheme for use in climate models. J Atmos Sci 56:1766–1782

    Article  Google Scholar 

  • Fasullo J, Webster PJ (2003) A hydrological definition of Indian monsoon onset and withdrawal. J Clim 16(14):3200–3211

    Article  Google Scholar 

  • Findlater J (1969) A major low-level air current near the Indian Ocean during the northern summer. Q J R Meteorol Soc 95:362–380

    Article  Google Scholar 

  • Fritsch JM, Chappell CF (1980) Numerical prediction of convectively driven mesoscale pressure systems. Part I: convective parameterization. J Atmos Sci 37:1722–1733

    Article  Google Scholar 

  • Gao XJ, Shi Y, Zhang DF et al (2012) Uncertainties of monsoon precipitation projection over China: results from two high resolution RCM simulations. Clim Res 52:213–226

    Article  Google Scholar 

  • Giorgi F, Mearns LO (1999) Introduction to special section: regional climate modeling revisited. J Geophys Res 104:6335–6352

    Article  Google Scholar 

  • Giorgi F, Marinucci MR, Bates GT (1993a) Development of a second generation regional climate model (RegCM2). Part I: boundary-layer and radiative transfer processes. Mon Weather Rev 121:2794–2813

    Article  Google Scholar 

  • Giorgi F, Marinucci MR, Bates GT, De Canio G (1993b) Development of a second- generation regional climate model (RegCM2). Part II: convective processes and assimilation of lateral boundary conditions. Mon Weather Rev 121:2814–2832

    Article  Google Scholar 

  • Giorgi F, Diffenbaugh NS, Gao XJ, Coppola E, Dash SK, Frumento O, Rauscher SA, Remedio A, Sanda IS, Steiner A, Sylla B, Zakey AS (2008) The regional climate change hyper-matrix framework. Eos 89(45):445–456

    Article  Google Scholar 

  • Giorgi F et al (2012) RegCM4: model description and illustrative basic performance over selected CORDEX domains. Clim Res 52:7–29

    Article  Google Scholar 

  • Giorgi F, Coppola E, Raffaele F et al (2014) Changes in extremes and hydroclimatic regimes in the CREMA ensemble projections. Clim Change 125:39–51

    Article  Google Scholar 

  • Grell GA (1993) Prognostic evaluation of assumptions used by cumulus parameterizations. Mon Weather Rev 121:754–787

    Article  Google Scholar 

  • Holtslag AAM, de Bruijn EIF, Pan H-L (1990) A high resolution air mass transformation model for short-range weather forecasting. Mon Weather Rev 118:1561–1575

    Article  Google Scholar 

  • Jones RG, Murphy JM, Noguer M (1995) Simulation of climate change over Europe using a nested regional-climate model. I: assessment of control climate, including sensitivity to location of lateral boundaries. Q J R Meteorol Soc 121(526):1413–1449

    Google Scholar 

  • Kalnay E, Kanamitsu M, Kistler R, Collins W, Deaven D, Gandin L, Iredell M, Saha S, White G, Woollen J, Zhu Y, Chelliah M, Ebisuzaki W, Higgins W, Janowiak J, Mo KC, Ropelewski C, Wang J, Leetmaa A, Reynolds R, Jenne R, Joseph D (1996) The NMC/NCAR 40-Year Reanalysis Project. Bull Am Meteorol Soc 77:437–471

    Article  Google Scholar 

  • Keshavamurthy RN, Sankara Rao MS (1992) The physics of monsoons. Allied Publishers Ltd, New Delhi

    Google Scholar 

  • Kiehl JT, Hack JJ, Bonan GB, Boville BA, Breigleb BP, Williamson D, Rasch P (1996) Description of the ncar community climate model (ccm3), Technical Report of NCAR/TN-420? STR, National Center for Atmospheric Research

  • Kistler R et al (2001) The NCEP–NCAR 50-year reanalysis: monthly means CD-ROM and documentation. Bull Am Meteorol Soc 82:247–268

    Article  Google Scholar 

  • Koteswaram P (1958) The easterly jet stream in the tropics. Tellus 10:43–57

    Article  Google Scholar 

  • Li WP (1999) Moisture flux and water balance over the South China Sea during late boreal spring and summer. Theor Appl Climatol 641:179–187

    Article  Google Scholar 

  • May W (2002) Simulated changes of the Indian summer monsoon under enhanced greenhouse gas conditions in a global time-slice experiment. Geophys Res Lett 29(7):1118. doi:10.1029/2001GL013808

    Article  Google Scholar 

  • Meehl GA, Arblaster JM (2003) Mechanisms for projected future changes in south Asian monsoon precipitation. Clim Dyn 21:659–675

    Article  Google Scholar 

  • 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. J Meteorol Soc Jpn 62:469–484

    Google Scholar 

  • Pattnayak KC, Panda SK, Dash SK (2013) Comparative study of regional rainfall characteristics simulated by RegCM3 and recorded by IMD. Global Planet Change 106:111–122

    Article  Google Scholar 

  • Pisharoty PR (1965) Evaporation over the Arabian Sea and the Indian Southwest Monsoon. In: Proceedings of International Indian Ocean Expedition, P. R. Pisharoty, Ed., pp 43–54

  • Raghavan K (1973) Tibetan anticyclone and tropical easterly jet. Pure appl Geophys 110:2130–2142

    Article  Google Scholar 

  • Rajeevan M, Bhate Jyoti (2009) A high resolution daily gridded rainfall dataset (1971–2005) for mesoscale meteorological studies. Curr Sci 96(4):558–562

    Google Scholar 

  • Ratnam JV, Giorgi F, Kaginalkar A, Cozzini S (2009) Simulation of the Indian monsoon using the RegCM3-ROMS regional coupled model. Clim Dyn 33:119–139

    Article  Google Scholar 

  • Saha KR, Bavadekar SN (1973) Water vapour budget and precipitation over the Arabian Sea during the northern summer. Q J R Mereorol Soc 99:273–278

    Article  Google Scholar 

  • Schaefer JT (1990) The critical success index as an indicator of warning skill. Weather Forecast 5:570–575

    Article  Google Scholar 

  • Shekhar MS, Dash SK (2005) Effect of Tibetan spring snow on the Indian summer monsoon circulation and associated rainfall. Curr Sci 88:1840–1844

    Google Scholar 

  • Singh GP, Oh JH (2007) Impact of Indian Ocean sea-surface temperature anomaly on Indian summer monsoon precipitation using a regional climate model. Int J Climatol 27:1455–1465

    Article  Google Scholar 

  • Sperber KR, Palmer TN (1996) Interannual tropical rainfall variability in general circulation model simulations associated with the atmospheric model inter-comparison project. J Clim 9:2727–2750

    Article  Google Scholar 

  • Sundqvist H, Berge E, Kristjansson JE (1989) The effects of domain choice on summer precipitation simulation and sensitivity in a regional climate model. J Clim 11:2698–2712

    Google Scholar 

  • Zeng X (2005) A prognostic scheme of sea surface skin temperature for modeling and data assimilation. Geophys Res Lett 32:l14605

    Google Scholar 

  • Zeng X, Zhao M, Dickinson RE (1998) Intercomparison of bulk aerodynamic algorithms for the computation of sea surface fluxes using TOGA COARE and TAO data. J Clim 11:2628–2644

    Article  Google Scholar 

  • Zhang DF, Gao XJ, Ouyang LC (2008) Simulation of present climate over China by a regional climate model. J Trop Meteorol 14:19–23

    Google Scholar 

Download references

Acknowledgments

The authors are thankful to the organizations from which datasets are obtained for conducting this study. The initial and boundary conditions to integrate RegCM4.2 are obtained from the Abdus Salam International Centre for Theoretical Physics (ICTP) website http://clima-dods.ictp.it/data/d8/cordex/HadGEM2/. The gridded rainfall data have been obtained from the India Meteorological Department (IMD). The atmospheric fields are obtained from the NCEP/NCAR reanalyzed dataset. Thanks are due to Dr. Erika Coppola, Mr. Graziano Giuliani and Mr. Ivan Girotto for providing the computing facility at ICTP to conduct the additional simulations suggested by the reviewer. The authors are also thankful to the anonymous reviewers for their valuable suggestions to improve the quality of the paper. This study has been undertaken as part of a research project sponsored by the Department of Science and Technology, Government of India.

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Dash, S.K., Pattnayak, K.C., Panda, S.K. et al. Impact of domain size on the simulation of Indian summer monsoon in RegCM4 using mixed convection scheme and driven by HadGEM2. Clim Dyn 44, 961–975 (2015). https://doi.org/10.1007/s00382-014-2420-1

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