Abstract
The paper addresses observational aspects of widespread rain associated with the organized convection that forms over the southwest peninsular India during the pre-monsoon season. The evolution of the cloud band over the equatorial region, its northward propagation, development of cross equatorial flow near the Somalia coast, and appearance of equatorial westerly wind resemble closely to that of the monsoon organized convection. Low-level convergence, cyclonic vorticity, and ascending motion are other major characteristics of the cloud bands associated with the pre-monsoon organized convection which exhibits similarity with that of monsoon. The ascending motion plays vital role on the formation of cloud band that produces widespread rainfall persisting for more than a week. The vertical shear of meridional winds is found to co-exist with precipitation over the Arabian Sea off the southwest peninsular India. The velocity potential values derived from the winds at 850 and 200 hPa levels confirm the rising motion on the basis of low-level convergence and upper level divergence. Also, shifting of ascending limb of the local Hadley circulation to the north of the equator is observed during the days of the presence of organized convection over the southwest peninsular region. Noticeable shift in the Walker circulation rising limb is also identified during the same time.
Similar content being viewed by others
References
Abhik S, Halder M, Mukhopadhyay P, Jiang X, Goswami BN (2013) A possible new mechanism for northward propagation of boreal summer intraseasonal oscillations based on TRMM and MERRA reanalysis. Clim Dyn 40:1611–1624. https://doi.org/10.1007/s00382-012-1425-x
Ananthakrishnan R, Soman MK (1988) The onset of the southwest monsoon over Kerala: 1901-1980. Int J Climatol 8:283–296
Anjaneyalu TSS (1969) On the estimates of heat and moisture over the Indian monsoon trough zone. Tellus 21:64–75
Babu CA, Joseph PV (2002) Post-monsoon sea surface temperature and convection anomalies over Indian and Pacific oceans. Int J Climatol 22:559–567. https://doi.org/10.1002/joc.729
Chakraborty A, Nanjundiah RS, Srinivasan J (2006) Theoretical aspects of the onset of Indian summer monsoon from perturbed orography simulations in a GCM. Ann Geophys 24:2075–2089
Fieux M, Stommel H (1977) Onset of the southwest monsoon over the Arabian Sea from marine reports of surface winds: structure and variability. Mon Wea Rev 105:231–236
Findlater J (1969) A major low level current near the Indian Ocean during northern summer. Quart J Roy Meteor Soc 95:362–380
Flatau MK, Flatau PJ, Rudnick D (2001) The dynamics of double monsoon onsets. J Clim 14:4130–4146
Frieler K, Mainhausen M, Von Delmling T, Andrews T, Forster P (2011) Changes in global-mean precipitation in response to warming, greenhouse gas forcing and black carbon. Geophys Res Lett 38:L04702. https://doi.org/10.1029/2010GL045953
Ghanekar SP, Puranik PV, Bhide UV (2003) Forecasting the onset of monsoon over Kerala using the peak in pre-monsoon convective activity over south peninsular India. Mausam 54:645–652
Ghanekar SP, Puranik PV, Mujumdar VR (2010) Application of satellite-derived OLR data in the prediction of the onset of Indian summer monsoon. Theor Appl Climatol 99:457–468. https://doi.org/10.1007/s00704-009-0154-5
Goswami BN (2005) South Asian monsoon: intraseasonal variability of the atmosphere-ocean climate system. William K, Lau M, Waliser DE (ed) Chapter 2, Praxis, Springer Berlin Heidelberg, pp. 19–61
Goswami BN, Krishnamurthy V, Annamalai H (1999) A broad-scale circulation index for the interannual variability of the Indian summer monsoon. Quart J Roy Meteor Soc 125:611–633
Gruber A, Krueger AF (1984) The status of the NOAA outgoing long wave radiation data set. Bull Amer Meteor Soc 65:958–962
Hamza V, Harikumar R, Vishnu R, Sasi Kumar V, Sampath S, Murali Das S, Mohan Kumar G (2011) Observational study of cloud base height and its frequency over a tropical station, Thiruvananthapuram, using a ceilometer. Int. J Remote Sens 32:8505–8518
Jayakrishnan PR, Babu CA (2014) Assessment of convective activity using stability indices as inferred from radiosonde and MODIS data. J Atmos Clim Sci 4:122–130
Jiang X, Waliser DE, Li JL, Woods C (2011) Vertical cloud structures of the boreal summer intraseasonal variability based on CloudSat observations and ERA-interim reanalysis. Clim Dyn 36:2219–2232
Joseph PV, Pillai PV (1988) 40-day mode of equatorial trough for long range forecasting of Indian summer monsoon onset. Curr Sci 57:951–954
Joseph PV, Raman PL (1966) Existence of low-level westerly jet stream over peninsular India during July. Ind J Meteor Geophys 17:407–410
Joseph PV, Sooraj KP, Rajan CK (2003) Conditions leading to monsoon onset over Kerala and the associated Hadley cell. Mausam 54:55–164
Kalnay E, Kanamitsu M, Kistler R, Collins W, Deaven D, Gandin L, Iredell M, Saha S, White G, Woollen J, Zhu Y, Leetmaa A, Reynolds R, Chelliah M, Ebisuzaki W, Higgins W, Janowiak J, Mo KC, Ropelewski C, Wang J, Jenne R, Joseph D (1996) The NCEP/NCAR 40-year reanalysis project. Bull Amer Meteor Soc 77:437–471
Krishnan R, Zhang C, Sugi M (2000) Dynamics of breaks in the Indian summer monsoon. J Atmos Sci 57:1354–1372
Kumar MRR (2004) Forecasting of onset of southwest monsoon over Kerala coast using satellite data. IEEE Trans Geosci Remote Sens 1:265–267
Lal DM, Pawar SD (2009) Relationship between rainfall and lightning over central Indian region in monsoon and premonsoon seasons. Atmos Res 92:402–410
Lawrence DM, Webster PJ (2002) The boreal summer intraseasonal oscillation: relationship between northward and eastward movement of convection. J Atmos Sci 59:1593–1606
Mao J, Wu G (2007) Interannual variability in the onset of the summer monsoon over the eastern Bay of Bengal. Theor Appl Climatol 89:155–170
Matsumoto J, Murakami T (2000) Annual changes of tropical convective activities as revealed from equatorially symmetric OLR data. J Meteor Soc Japan 78:543–561
Medina S, Houze RA Jr, Kumar A, Niyogi D (2010) Summer monsoon convection in the Himalayan region: terrain and land cover effects. Quart J Roy Meteor Soc 136:593–616
Menon A, Levermann A, Schewe J, Lehmann J, Frieler K (2013) Consistent increase in Indian monsoon rainfall and its variability across CMIP-5 models. Earth Sys Dyn 4:287–300
Mukhopadhyay P (2004) Idealized simulation of a thunderstorm over Kolkata using RAMS. J Ind Geophys Union 8:253–266
Neema CP, Hareeshkumar PV, Babu CA (2012) Characteristics of Arabian Sea mini warm pool and Indian summer monsoon. Clim Dyn 38:2073–2087
Orlanski I (1975) A rational subdivision scales for atmospheric processes. Bull Amer Meteor Soc 56:527–530
Puranik SS, Sinha Ray KC, Sen PN, Pradeep Kumar P (2013) An index for predicting the onset of monsoon over Kerala. Curr Sci 105:954–961
Ranalkar MR, Chaudhari HS (2009) Seasonal variation of lightning activity over the Indian subcontinent. Meteor Atmos Phys 104:125–134. https://doi.org/10.1007/s00703-009-0026-7
Rao YP (1976) Southwest Monsoon, Meteorological Monograph-Synoptic Meteorology No. 1/1976, India Meteorological Department, 367 pp.
Sathiyamoorthy V, Shukla BP, Pal PK (2010) Increase in the pre-monsoon rainfall over the Indian summer monsoon region. Atmos Sci Lett 11:313–318
Sherwood SC, Minnis P, McGill M (2004) Deep convective cloud top heights and their thermodynamic control during CRYSTAL-FACE. J Geophys Res 109:D20119. https://doi.org/10.1029/2004JD004811
Shin SH, Chung IIU, Kim HJ (2012) Relationship between the expansion of dry lands and the intensification of Hadley circulation during the twentieth century. Meteorog Atmos Phys 118:117–128
Sikka DR, Gadgil S (1980) On the maximum clod zone and the ITCZ over Indian longitudes during the southwest monsoon. Mon Wea Rev 108:1840–1853
Sikka DR, Paul DK, Deshpande VR, Puranik PV (1986) Sub-seasonal scale fluctuations of the ITCZ over Indo-Pacific region during summer monsoon season—part I features of Indian region. Pro Indian Acad Sci (Earth Planet Sci) 95:47–73
Srinivasan J, Gadgil S, Webster PJ (1993) Meridional propagation of large-scale monsoon convective zones. Meteor Atmos Phys 52:15–35
Srivastava AK, Sinha Ray KC (1999) Role of CAPE and CINE in modulating the convective activities during April over India. Mausam 50:257–262
Trenberth KE, Stepanik DP, Caron JM (2000) The global monsoon as seen through the divergent atmospheric circulation. J Clim 13:3969–3993
Tyagi A (2007) Thunderstorm climatology over Indian region. Mausam 58:189–212
Vishnu R, Anil Kumar V, Varikoden H, Sarath Krishnan K, Sreekanth TS, Subi Symon VN, Murali Das S, Mohan Kumar G (2013) Convective thundercloud development over the Western Ghats mountain slope in Kerala. Curr Sci 104:1506–1514
Waliser DE, Graham NE (1993) Convective cloud systems and warmpool sea surface temperatures: coupled interactions and self-regulation. J Geophys Res 98:12881–12893
Wallace JM, Hobbs PV (2006) Atmospheric Science: an introductory Survey, 2nd edn. Academic Press, Cambridge, p 483
Williams E, Renno N (1993) An analysis of the conditional instability of the tropical atmosphere. Mon Wea Rev 121:21–36
Yamane Y, Hayashi T (2006) Evaluation of environmental conditions for the formation of severe local storms across the Indian subcontinent. Geophys Res Lett 33:L17806
Zhang C (1993) Large scale variability of atmospheric deep convection in relation to sea surface temperature in the tropics. J Clim 6:1898–1913
Acknowledgements
PN Sreelekha acknowledges the Department of Science and Technology for providing the INSPIRE Fellowship and CA Babu acknowledges the ISRO for providing the financial support in the form of the RESPOND Project (No.4/638) for carrying out the research analysis. The authors also acknowledge the India Meteorological Department for providing the rainfall data, NCEP/NCAR for providing the Reanalysis data and NOAA for providing OLR data.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Sreelekha, P.N., Babu, C.A. Organized convection over southwest peninsular India during the pre-monsoon season. Theor Appl Climatol 135, 1279–1293 (2019). https://doi.org/10.1007/s00704-018-2446-0
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00704-018-2446-0