Publications

Archeological sites

Lightning is one of the most prevalent atmospherically originated threats to the well-being of structures in tropics and oceans where the ground flash density is relatively high.

Characteristic features of Cloud flashes Published

Lightning is one of the most common and most fascinating atmospheric phenomena and occurs almost over any region of the globe. Although lightning is believed to be in existence well before the human civilization began on earth, it has not been fully understood to this date. 

Lives on Churiya range and Lesser Himalayas are extremely prone to the Lightning Hazards

Exact numbers on fatalities and injuries from lightning are not available for most countries. One estimate of global fatalities is several thousand [1], another 6000 fatalities per year [2], and the third 24,000 fatalities per year [3]

Multi fractal

Measurements of Lightning electromagnetic radiation have been extensively carried out and have revealed many features of lightning in time domain. For example, from lightning electric field waveform measurements, the average time between K-changes was observed in the range of 8–20 ms (Kitagawa and Brook, 1960; Miranda et al., 2003; Thottappillil et al.,1990).

Possible impact AOD

Lightning is one of the most common atmospheric activities that every human civilization has witnessed since time immemorial. The beginning of the scientific study of lightning is attributed to Benjamin Franklin, dating back to 1752.

Positive RS Kathmandu

Lightning positive ground flashes, in general, transport the positive charge from the cloud to the ground, occur very rarely. Of all the cloud to ground flashes, the positive ground flashes account for about 10% (Rakov and Uman, 2003). Considering the tripole structure of a thundercloud, the paucity of the positive ground flashes can easily be justified. 

Direct Lightning Impact Assessment on a Rural khadka et al.

Lightning has been one of the major threats to power distribution networks. Physical damages and insulation failure are the two major impacts due to lightning return strokes [1]. Physical damage is understood as damage incurred due to dissipated lightning energy, whereas insulation failure is the temporary situation where insulating materials within the distribution networks fail to insulate. 

Comparative Study

Satellite images of lightning activities show that the Himalayan region is one of the world’s lightning prone areas (https://ghrc.nsstc.nasa. gov/lightning/data/data_lis_trmm.html). Due to the topology, varied surface temperature, moisture, and atmospheric circulation, lightning flash density (LFD) over this region have a tremendous spatiotemporal variability. 

CloudFlashes Kathmandu

Lightning discharges in general which do not connect to the earth are termed as cloud flashes which include intra-cloud, inter-cloud and air discharges. Of all these cloud flashes, intra-cloud discharges occur most frequently. 

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