Skip to main content
Log in

Understanding convection features over Bay of Bengal using sea surface temperature and atmospheric variables

  • Original Paper
  • Published:
Theoretical and Applied Climatology Aims and scope Submit manuscript

Abstract

Tropical oceanic regions are frequently prone to deep convections. Hence, it is very essential to understand the features of convection with the help of oceanic and atmospheric variables such as sea surface temperature (SST), outgoing longwave radiation (OLR), rainfall, relative humidity, columnar water vapour (CWV) etc. and the linkage among them. In our present study, we have divided the Bay of Bengal (BoB) into ten different subregions (SR) and have attempted to study the connection between the above-stated variables during convective and non-convective events in the southwest monsoon (SWM) season (June to September) for the period 1998–2010. The monthly behaviour of SST/OLR decreased by 0.5 °C/14 W/m2 from May to June and increased by 0.1 °C/7 W/m2 from September to October. Among the ten SRs, SR 5 and SR 10 are observed to be coldest and warmest, respectively, based on the SST variations. Intra-seasonal oscillations of the above-mentioned variables show the influences of quasi-biweekly oscillations (QBWO) and Madden-Julian oscillations (MJO). As the threshold values for SST, OLR and rainfall were already reported, we have drawn our attention to deduce a threshold value for water vapour in lower level troposphere (water vapour density (WVD) at 850 mb) which highly influences the convection. In arriving at a threshold of low-level water vapour, we have analysed the convective and non-convective events of each central 1 × 1° grid in all the SRs for the period from 1998 to 2010, along with water vapour scale height. Our analysis inferred that the low-level water vapour density at 850 mb varied above 12 g/m3during convective days and below 12 g/m3during non-convective days. We noticed that the variability in water vapour density is more in non-convective days than in convective days over BoB. The results of the study may be useful to understand the water vapour dynamics with SST, OLR and rainfall.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6

Similar content being viewed by others

References

  • Bielli S, Hartmann DL (2004) On wind, convection, and SST variations in the northeastern tropical pacific associated with the Madden–Julian Oscillation. J Clim 17:4080–4088

    Article  Google Scholar 

  • Bretherton CS, Peters ME, Back LE (2004) Relationships between water vapor path and precipitation over the tropical oceans. J Clim 17:1517–1528

    Article  Google Scholar 

  • Daubechies I (1992) Ten lectures on wavelets, CBMS-NSF regional conference series in applied mathematics, 357

  • 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

    Article  Google Scholar 

  • Gadgil S, Joseph PV, Joshi NV (1984) Ocean-atmosphere coupling over monsoon regions. Nature 312:141–143

    Article  Google Scholar 

  • Goswami BN, Ajaya Mohan RS (2001) Intraseasonal oscillations and interannual variability of the Indian summer monsoon. J Clim 14:1180–1198

    Article  Google Scholar 

  • Han W, Timothy Liu W, Lin J (2006) Impact of atmospheric submonthly oscillations on sea surface temperature of the tropical Indian Ocean. Geophys Res Lett 33, L03609. doi:10.1029/2005GL025082

    Google Scholar 

  • Hareesh Kumar PV, Prasada Rao CVK, Swain J, Madhusoodanan P (2001) Intra-seasonal oscillations in the central Bay of Bengal during summer monsoon 1999. Curr Sci 80(6):786–790

    Google Scholar 

  • Holloway CE, Neelin JD (2009) Moisture vertical structure, column water vapor, and tropical deep convection. J Atmos Sci 66:1665–1683

    Article  Google Scholar 

  • Inamdar AK, Ramanathan S (1994) Physics of greenhouse effect and convection in warm oceans. J Clim 7:715–731

    Article  Google Scholar 

  • Keil C, Rpnack A, Craig GC, Schumann U (2008) Sensitivity of quantitative precipitation forecast to height dependent changes in humidity. Geophys Res Lett 35, L09812. doi:10.1029/2008GL033657

    Article  Google Scholar 

  • Krishnamurti TN, Ardanuy P (1980) The 10 to 20-day westward propagating mode and “Breaks in the Monsoon”. Tellus 32:15–26

    Article  Google Scholar 

  • Lafrenière M, Sharp M (2003) Wavelet analysis of inter-annual variability in the runoff regimes of glacial and nival stream catchments, Bow Lake, Alberta. Hydrol Process 17(6):1093–1118

    Article  Google Scholar 

  • Lanzante JR (1996) Lag relationships involving tropical sea surface temperatures. J Clim 9:2568–2578

    Article  Google Scholar 

  • Lau KM, Chan PH (1988) Intraseasonal and interannual variations of tropical convection: a possible link between the 40–50-day oscillation and ENSO? J Atmos Sci 45:506–521

    Article  Google Scholar 

  • Lawrence DM, Webster PJ (2001) Interannual variations of the intraseasonal oscillation in the south Asian summer monsoon region. J Clim 14:2910–2922

    Article  Google Scholar 

  • Mooley D, Shukla J (1989) Main features of the westward moving low pressure systems which form over the Indian region during the summer monsoon season and their relation to the monsoon rainfall. Mausam 40:137–152

    Google Scholar 

  • Roxy M (2014) Sensitivity of precipitation to sea surface temperature over the tropical summer monsoon region—and its quantification. Clim Dyn 43:1159–1169

    Article  Google Scholar 

  • Roxy M, Tanimoto Y (2007) Role of SST over the Indian Ocean in influencing the intraseasonal variability of the Indian summer monsoon. J Meteor Soc Japan 85(3):349–358

    Article  Google Scholar 

  • Roxy M, Tanimoto Y, Preethi B, Pascal T, Krishnan R (2013) Intraseasonal SST-precipitation relationship and its spatial variability over the tropical summer monsoon region. Clim Dyn 41(1):45–61

    Article  Google Scholar 

  • Satheesan K, Krishnamurthy BV (2005) Modulation of tropical tropopause by wave disturbances. J Atmos Sol-Terr Phy 67:878–883

    Article  Google Scholar 

  • Shankar D, Shetye SR, Joseph PV (2007) Link between convection and meridional gradient of sea surface temperature in the Bay of Bengal. J Earth Syst Sci 116(5):385–406

    Article  Google Scholar 

  • Shenoi SSC, Shankar D and Shetye SR (2002) Differences in heat budgets of the near-surface Arabian Sea and Bay of Bengal: implications for the summer monsoon. J Geophys Res. 107 doi:10.1029/2000JC000679

  • Sherwood SC (1999) Convective precursors and predictability in the tropical western Pacific. Mon Weather Rev 127:2977–2991

    Article  Google Scholar 

  • Sherwood SC, Roca R., Weckwerth TM and Andronova NG (2010) Tropospheric water vapor, convection and climate. Rev Geophys, 48(2), doi:10.1029/2009RG00301

  • Sifuzzaman M, Islam SR, Ali MZ (2009) Applications of wavelet transform and its advantages compared to Fourier transform. J Phy Sci 13:121–134

    Google Scholar 

  • Sud YC, Walker GK, Lau KM (1999) Mechanisms regulating sea surface temperatures and deep convection in the tropics. Geophys Res Lett 26:1019–1022

    Article  Google Scholar 

  • Tomasi C (1984) Vertical distribution features of atmospheric water vapor in the Mediterranean, Red Sea and Indian Ocean. J Geophys Res 89(D2):2536–2566

    Article  Google Scholar 

  • Torrence C, Compo GP (1998) A practical guide to wavelet analysis. Bull Am Meteorol Soc 79:61–78.4

    Article  Google Scholar 

  • Uma R, Lakshmi Kumar TV, Narayanan MS, Bhate J, Rajeevan M, Niranjan Kumar K (2013) Large scale features and assessment of spatial scale correspondence between TMPA and IMD rainfall data sets over Indian landmass. J Earth Syst Sci 122(3):573–588

    Article  Google Scholar 

  • Vinayachandran PN, Shetye SR (1991) The warm pool in the Indian Ocean. Proc Indain Acad Sci (Earth Planet Sci) 100(2):165–175

    Google Scholar 

  • Vinayachandran PN, Neema CP, Simi Mathew and Remya R (2012) Mechanisms of summer intraseasonal sea surface temperature oscillations in the Bay of Bengal. J Geophys Res: Oceans (1978–2012) 117(C1)

  • Waliser DE, Graham NE (1993) Convective cloud systems and warm pool seas surface temperatures: coupled interactions and self-regulation. J Geophys Res 98(12):12,881–12,893

    Article  Google Scholar 

  • Wang B, Wang Y (1996) Temporal structure of the southern oscillation as revealed by waveform and wavelet analysis. J Clim 9:1586–1598

    Article  Google Scholar 

  • Weckwerth TM, Pettet CR, Fabry F, Park S, LeMone MA, Wilson JW (2005) Radar refractivity retrieval: validation and application to short-term forecasting. J Appl Meteorol 44:285–300

    Article  Google Scholar 

  • Zelinka MD, Hartman DL (2009) Response of humidity and clouds to tropical convection. J Clim 22:2389–2404

    Article  Google Scholar 

  • Zhang C (1993) Large-scale variability of atmospheric deep convection with respect to sea surface temperature in the tropics. J Clim 6:1898–1912

    Article  Google Scholar 

  • Zhang GJ, Ramanathan V, McPhaden MJ (1995) Convection-evaporation feedback in the equatorial pacific. J Clim 8:3040–3051

    Article  Google Scholar 

Download references

Acknowledgment

This work is supported by a grant received from ISRO RESPOND, Gov’t. of India. We gratefully acknowledge Dr. B.V. Krishnamurthy, former director of SPL, VSSC, Trivandrum, for his useful suggestions and encouragement. We thank D. Selvaraj, Senior Research Fellow, SRM University, for programming assistance. Our sincere thanks to the anonymous reviewers for their constructive comments.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to T. V. Lakshmi Kumar.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Uma, R., Lakshmi Kumar, T.V. & Narayanan, M.S. Understanding convection features over Bay of Bengal using sea surface temperature and atmospheric variables. Theor Appl Climatol 125, 469–478 (2016). https://doi.org/10.1007/s00704-015-1518-7

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00704-015-1518-7

Keywords

Navigation