2021
DOI: 10.1016/j.atmosres.2021.105683
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Regional variation of electrical and lightning properties of thunderclouds during the pre-monsoon season over the north-eastern and eastern part of India

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Cited by 10 publications
(5 citation statements)
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“…The result is in agreement with the Biswasharma et al . (2021), where it is reported that over the eastern and northeastern part of India, occurrence as well as intensity of the thunderclouds is maximum during 1500 to 1800 IST. The present result is also consistent with the Cecil and Blankenship (2012).…”
Section: Resultsmentioning
confidence: 99%
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“…The result is in agreement with the Biswasharma et al . (2021), where it is reported that over the eastern and northeastern part of India, occurrence as well as intensity of the thunderclouds is maximum during 1500 to 1800 IST. The present result is also consistent with the Cecil and Blankenship (2012).…”
Section: Resultsmentioning
confidence: 99%
“…Multiscale interaction of circulation with local topography plays an important role in shaping the weather and climate in this region (Goswami et al ., 2010). This region is highly vulnerable to the occurrence of extreme weather events such as heavy rainfall, hail, lightning, and strong wind during the premonsoon season (March through May) (Koteswaram and Srinivasan, 1958; Sen and Basu, 1961; Chaudhury and Banerjee, 1983; Ono, 1998; Karmakar and Alam, 2006; Kumar and Mohapatra, 2006; Yamane et al ., 2009; Dalal et al ., 2012; Mahanta et al ., 2013; Choudhury et al ., 2016; Mahanta and Yamane, 2020; Biswasharma et al ., 2021), causing fatalities and damage to agriculture as well as to property (De et al ., 2005; Bhardwaj et al ., 2017). Hailstorms, in particular, are one of the primary contributors to these losses (Chattopadhyay et al ., 2017; Rymbai et al ., 2019; Raihan et al ., 2020).…”
Section: Introductionmentioning
confidence: 99%
“…The pre‐monsoon thunderstorms are more intense, especially along the Meghalaya plateau and sub‐Himalayan foothills, where Z ratios are slightly higher (more than 4) than in other parts. Also, the northeastern region, due to steep orography and continuous moisture availability from Bay‐of‐Bengal, exhibits a broader stratiform cloud with lower convective updraft in monsoon (Houze et al., 2007), which is responsible for less IC lightning and significantly less Z ratio (Biswasharma et al., 2021). Many nocturnal thunderstorms form in the northeastern region due to radiative cooling at night (Murugavel et al., 2014; Pawar et al., 2015), which may be characterized as elevated thunderstorms.…”
Section: Resultsmentioning
confidence: 99%
“…There are five distinctly identifiable thunderstorm-prone regions-Northeast India (NEI), Southern Peninsula (SP), Central India (CI), East Coast of India (ECI), and Northwest India (NWI) [26]. Each thunderstorm-prone region is defined based on its trigger mechanism, lightning structure, microphysical, and dynamical properties [2,[26][27][28][29][30][31][32].…”
Section: Introductionmentioning
confidence: 99%