Abstract
Dust storms commonly occur during the pre-monsoon (summer) season in north and northwest parts of India. Characteristics of dust events of the pressure gradient type are well understood. However, comprehensive studies on mechanism of convective dust storms in India are few. A convective dust storm which occurred on 21 April 2010 in association with a western disturbance over North India was hence studied. In the absence of in situ data, we used available satellite data to study the event. Dust storm that occurred on 20 April 2010 on the surface of the Thar Desert transported dust to northern and northwestern parts of India (Rajasthan, Haryana, Delhi and some parts of Uttar Pradesh). This formed a background of aerosols that affected the thunderstorm formed in association with western disturbance and the strong updraft in the thunderstorm carried the dust lingering in the atmosphere to higher altitudes. Large amount of aerosols carried to higher altitude suppressed the chance of precipitation by affecting the cloud top microphysics. Enhancement in evaporation due to an increase in aerosol concentration and strong downdrafts during dissipation of the thunderstorm resulted in emission of dust particles which led to the convective dust event of 21 April 2010.
Similar content being viewed by others
References
Andreae MO, Rosenfeld D (2008) Aerosol-cloud-precipitation interactions. Part 1. The nature and sources of cloud-active aerosols. Earth Sci Rev 89:13–41
Bollasina M, Nigam S (2009) Absorbing aerosols and pre-summer monsoon hydroclimate variability over the Indian subcontinent: the challenge in investigating links. Atmos Res 94:338–344
DeMott PJ, Sassen K, Poellet MR, Baumgardner D, Rogers DC, Brooks SD, Prenni AJ, Kreidenweis SM (2003) African dust aerosols as atmospheric ice nuclei. Geophys Res Lett 30:1732
Dessler AE, Yang P (2003) The distribution of tropical thin cirrus clouds inferred from Terra MODIS data. J Clim 16:1241–1247
Dey S, Tripathi SN, Singh RP, Holben BN (2004) Influence of dust storms on the Aerosol Optical Properties over Indo Gangetic Basin. J Geophys Res 109:D20211. doi:10.1029/2004JD004924
El-Askary H, Gautam R, Singh RP, Kafatos M (2006) Dust storm detection over Indo-Gangetic basin using multi sensor data. Adv Space Res 37:728–733
Flamant C, Chaboureau J-P, Parker DP, Taylor CM, Cammas JP, Bock O, Timouk F, Pelon J (2007) Airborne observations of the impact of a convective system on the planetary boundary-layer thermodynamics and aerosol distribution in the intertropical discontinuity region of the west African monsoon. Q J Royal Meteorol Soc 133:1175–1189
Gao B-C, Meyer K, Yang P (2004) A new concept on remote sensing of cirrus optical depth and effective ice particle size using water vapor absorption channels near 1.38 and 1.88 μm. IEEE Trans Geosci Remote Sens 42:1891–1899
Gautam R, Liu ZY, Singh RP, Hsu NC (2009) Two contrasting dust dominant periods over India observed from MODIS and CALIPSO data. Geophys Res Lett 36:L06813
Goudie AS (1978) Dust storms and their geomorphological implications. J Arid Env 1:291–310
Goudie AS, Middleton NJ (2001) Saharan dust storms : nature and consequences. Earth Sci Rev 56:179–204
Hall EF Jr, Neff WD, Frazier TV (1976) Wind shear observations in thunderstorm density currents. Nature 267:408–411
Hashino T (2008) Microphysical effects of Saharan dusts on orogenic thunderstorm. Adv Geosci 17:31–34
Horace RB, Roscoe RB (1948) Thunderstorm structure and circulation. J Meteorol 5:71–86
Kayetha VK, Senthilkumar J, Prasad AK, Singh RP (2007) Effect of dust storm on ocean color and snow parameters. J Indian Soc Remote Sens 35:1–9
Kidson JW (1997) The utility of surface and upper air data in synoptic climatological specification of surface climatic variables. Int J Climatol 17:399–413
Lee SS (2011) Dependence of aerosol-precipitation interactions on humidity in a multiple-cloud system. Atmos Chem Phys 11:2179–2196
Lindsey DT, Hillger DW, Grasso L, Knaff JA, Dostalek JF (2006) GOES climatology and analysis of thunderstorms with enhanced 3.9 μm reflectivity. Mon Weather Rev 134:2342–2353
Liou KN (1986) Influence of cirrus clouds on weather and climate processes: a global perspective. Mon Weather Rev 114:1167–1199
Littmann T (1991) Dust storm frequency in Asia: climatic control and variability. Int J Climatol 11:393–412
Miller S, Kuciauskas A, Liu M, Ji Q, Reid J, Breed D, Walker A, Mandoos A (2008) Haboob dust storms of the southern Arabian Peninsula. J Geophys Res 113:DO1202
Rodgers DM, Griffith CG (1989) Interpretation of GOES water vapor imagery and its application to forecasting thunderstorm. In: 3rd International Conference on the Aviation Weather System, 30 January to 3 February 1989, held at Anaheim, California, pp 351–355
Rosenfeld D, William LW, Lerner A, Kelman G, Linsey DT (2008) Satellite detection severe convective storms by their retrieved vertical profiles of cloud particle effective radius and thermodynamic phase. J Geophys Res 113:D04208
Rossow WB, Schiffer RA (1999) Advances in understanding clouds from ISCCP. Bull Am Meteorol Soc 80:2261–2287
Roy SS, Roy SS (2011) Regional variability of convection over northern India during the pre- monsoon season. Theor Appl Climatol 103:145–158
Smirnov A, Holben BN, Dubovik O, O’Neill Eck NT, Westphal TF, Goroch DL, Pietras AK, Slustker I (2000) Atmospheric aerosol optical properties in the Persian Gulf. J Atmos Sci 59:620–634
Sterk G (2002) Causes, consequences and control of wind erosion in Sahelian Africa: a review. Land Degrad Dev 14:95–108
Takemi T (1999) Structure and evolution of severe squall line over the arid region in northwest China. Mon Weather Rev 127:1301–1309
Tulet P, Crahan-Kaku K, Leriche M, Aouizerats B, Crumeyrolle S (2010) Mixing of dust aerosols into a mesoscale convective system: generation, filtering and possible feedbacks on ice anvils. Atmos Res 96:302–314
Winker D, Hunt W, McGill MJ et al (2007) Initial performance assessment of CALIOP. Geophys Res Lett 34:L19803
Wylie DP, Menzel WP (1999) Eight years of high cloud statistics using HIRS. J Clim 12:170–184
Acknowledgments
We acknowledge NASA for the AIRS and MODIS data, and NOAA-CIRES Climate Diagnostic Centre, Boulder, USA for the NCEP reanalysis data. The authors would like to also thank EUMETSAT for providing half hourly images. We are also very grateful to the reviewers for their painstaking review and the useful suggestions made that resulted in improving the manuscript.
Author information
Authors and Affiliations
Corresponding author
Additional information
Responsible editor: J. Fasullo.
Rights and permissions
About this article
Cite this article
Desouza, N.D., Kurchania, R. & Qureshi, M.S. Initiation of a convective dust storm over North India on 21 April 2010 inferred using satellite data. Meteorol Atmos Phys 122, 47–54 (2013). https://doi.org/10.1007/s00703-013-0271-7
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00703-013-0271-7