2012
DOI: 10.1007/978-3-642-13296-4
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Global Tropical Cyclogenesis

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Cited by 23 publications
(10 citation statements)
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“…3a and Fig. 3b, primarily due to their dissimilar strength at different stage of CLC (Sharkov, 2012). This evolution in Ne concentration at the ionospheric heights helps to infer that the ionosphere have close link with the lower atmosphere.…”
Section: Daily Variation In Olr and Vertical Ne Concentrationmentioning
confidence: 76%
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“…3a and Fig. 3b, primarily due to their dissimilar strength at different stage of CLC (Sharkov, 2012). This evolution in Ne concentration at the ionospheric heights helps to infer that the ionosphere have close link with the lower atmosphere.…”
Section: Daily Variation In Olr and Vertical Ne Concentrationmentioning
confidence: 76%
“…It was already reported in one of our previous studies (Mondal et al 2014) that during Cyclone Genesis Period (CGP) (Sharkov, 2012) Table 1. To curtail the effect of diurnal variability in the ionospheric signature to be detected, if any, we finally calculate daily weighted mean and standard deviation of each parameter using equation (2).…”
Section: Methodologiesmentioning
confidence: 96%
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“…Globally, September is the most active period-when cyclone formation frequency is the highest-and May is the least active period-when cyclone formation frequency is the lowest (Sharkov, 2000). (Neumann et al, 1993).…”
Section: Tropical Cyclone Formation Basins and Their Characteristicsmentioning
confidence: 99%