2017
DOI: 10.1016/j.elstat.2017.05.001
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Global Electric Circuit research at Graciosa Island (ENA-ARM facility): First year of measurements and ENSO influences

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Cited by 11 publications
(3 citation statements)
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“…On the one hand, the quasi‐static potential difference of ∼250 kV between the Earth and the lower ionosphere is maintained partly by electric charges that are separated in thunderclouds (Slyunyaev et al., 2019). The vertical electric field (or its negative, the atmospheric electric potential gradient, PG) corresponding to this potential difference can be measured relatively easily also near the surface and it carries the possibility in special circumstances to broadly infer the global state of the DC GEC (Lopes et al., 2017; Nicoll, 2012). On the other hand, lightning strokes in thunderstorms produce radio waves which form the AC part of the GEC as they propagate in the Earth‐ionosphere waveguide (EIWG; Barr et al., 2000; Le Vine, 1987).…”
Section: Introductionmentioning
confidence: 99%
“…On the one hand, the quasi‐static potential difference of ∼250 kV between the Earth and the lower ionosphere is maintained partly by electric charges that are separated in thunderclouds (Slyunyaev et al., 2019). The vertical electric field (or its negative, the atmospheric electric potential gradient, PG) corresponding to this potential difference can be measured relatively easily also near the surface and it carries the possibility in special circumstances to broadly infer the global state of the DC GEC (Lopes et al., 2017; Nicoll, 2012). On the other hand, lightning strokes in thunderstorms produce radio waves which form the AC part of the GEC as they propagate in the Earth‐ionosphere waveguide (EIWG; Barr et al., 2000; Le Vine, 1987).…”
Section: Introductionmentioning
confidence: 99%
“…The first measurements of a predominantly experimental nature began more than 150 years ago. The modern level of instrumentation contributed to the organization of global systematic observations of electrical quantities such as the potential gradient, electrical conductivity of air, ion concentration, current density, and others [1][2][3][4][5][6][7][8]. Today, ground-based measurements provide information about the electrical state of the atmosphere, and different approaches to data selection and processing have allowed us to draw fundamental conclusions about the influence of fair weather and disturbed weather conditions [6,[11][12][13][14][15][16][17][18][19][23][24][25][26][27][28][29][30][31][32][33][34][35][36][37][38][39][40] on the surface atmospheric electricity.…”
Section: Introductionmentioning
confidence: 99%
“…The first measurements of a predominantly experimental nature began more than 150 years ago. Improvements to existing instrumentation contributed to the organization of global systematic observations of electrical quantities such as the potential gradient (φ), electrical conductivity of air, ion concentration, current density, and others [1][2][3][4][5][6][7][8]. Today, numerous ground-based measurements provide information about the electrical state of the atmosphere,and different approaches [1,6,9] to data selection and processing have allowed us to draw fundamental conclusions about the influence of fair-weather and disturbed weather conditions [6,[11][12][13][14][15][16][17][18][19][22][23][24][25][26][27][28][29][30][31][32][33][34][35][36][37][38] on the surface atmospheric electricity.…”
Section: Introductionmentioning
confidence: 99%