The recent research has revealed a basic understanding of the scale selection and northward propagation of the BSISOs. But the complete understanding about the organization and intensification of BSISOs remains elusive. We have attempted to investigate the dynamical, physical processes, the effect of scale interaction and circulation-heating feedback during the organization and intensification of BSISOs. (Sarkar S., Mukhopadhyay P., Dutta S., International Journal of Climatology, Online, February 2017)
Read MoreThe objectives of the Winter Fog Experiment (WIFEX) over the Indo-Gangetic Plains of India are to develop better now-casting and forecasting of winter fog on various time- and spatial scales. The microwave radiometer profiles of temperature and liquid water indicate a mini-convective boundary layer structure, which sustained turbulence at the bottom and top of the fog layer. Imminent fog could be identified with the help of equivalent potential temperature at least 2–3 h prior to the event. (Ghude S.D., Bhat G.S., Prabha T., Jenamani R.K., Chate D.M., Safai P.D., Karipot A.K., Konwar M., Pithani P., Sinha V., Rao P.S.P., Dixit S.A., Tiwari S., Todekar K., Varpe S., Srivastava A.K., Bisht D.S., Hazra A., Nigam N., Shende U., Lal D.M., Acharja P., Kulkarni R., Subharthi C., Balaji B., Varghese M., Bera S., Rajeevan M., Current Science, 112, February 2017)
Read MoreThe influence of strong horizontal electric field (EH) on different stages of deformation and eventual breakup of the large water drops of 6.6, 7.0, and 7.25mm diameter has been observed in avertical wind tunnel using high-speed photography. Dumbbell, filament, and bag modes of drop breakup areobserved when EH = 0. However, drops elongate in horizontal direction, mostly develop sharp curvature attheir ends, eject a fine jet spray of tiny droplets, and ultimately break up into several droplets in EH = 500kVm-1. Extremeelongation up to 29mm is observed for a 7.0mm diameter drop. Results suggest that theeffect of EH in final oscillation before breakup overcomes the effect of hydrodynamic and aerodynamicforces in elongating the drop. Also, no breakup of bag type is observed in EH = 500 kVm-1. Moreover, the fragments formed after the drop breakup and tiny droplets ejected by their fragments carry electrical chargesof polarity determined by the induced charge on the parent drop in EH. The significance of the results isdiscussed in modifying the drop growth and the radar echo-precipitation relationships in thunderclouds. (Bhalwankar R., Deshpande C.G., Kamra A.K., Journal of Geophysical Research, 122, February 2017)
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