2013
DOI: 10.1016/j.jastp.2013.09.006
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Studies on the seasonal variation of atmospheric electricity parameters at a tropical station in Kolkata, India

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Cited by 16 publications
(3 citation statements)
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“…Daily curve measurements performed at land stations are generally different when compared to the Carnegie curve due to local phenomena, such as pollution and aerosols. Similarly, measurement performed at different stations do not show the same minimum and maximum times as in the Carnegie curve (Yeboah-Amankwah, 1989; Kamra et al, 1994;Harrison, 2003;Kumar et al, 2009;Guha et al, 2010;De et al, 2013). Nevertheless, in some cases good correlations have been found (Israelsson and Tammet, 2001;Harrison, 2003;Marcz and Harrison, 2003).…”
Section: Installation Of the New Network Data Processing And First Re...mentioning
confidence: 90%
“…Daily curve measurements performed at land stations are generally different when compared to the Carnegie curve due to local phenomena, such as pollution and aerosols. Similarly, measurement performed at different stations do not show the same minimum and maximum times as in the Carnegie curve (Yeboah-Amankwah, 1989; Kamra et al, 1994;Harrison, 2003;Kumar et al, 2009;Guha et al, 2010;De et al, 2013). Nevertheless, in some cases good correlations have been found (Israelsson and Tammet, 2001;Harrison, 2003;Marcz and Harrison, 2003).…”
Section: Installation Of the New Network Data Processing And First Re...mentioning
confidence: 90%
“…These signals are recorded through a PCI 1050, 16 channel 12 bit DAS card and then processed and stored in a computer. The receiver bandwidth used for the 7 and 9 kHz signals is set to 100 Hz to make the measurement sensitive to modal interference patterns (De et al 2013a).…”
Section: Vlf Sferics and Vlf Transmitted Sub-ionospheric Signalsmentioning
confidence: 99%
“…Thus, in the polluted urban environment, the surface values of the potential gradientare higher than those in the countryside and are subject to additional fluctuations due to changes in concentration. This effect has been found in many cities around the world [2,6,9,40,41]. The lofting of smoke plumes from wildland fires [42], intense dust storms [43,44], and eruptive clouds from volcanoes [45] spreading in middle and upper atmosphere are all factors contributing to a decrease in the potential gradient.…”
Section: Introductionmentioning
confidence: 97%