The global representativeness of fair-weather atmospheric electricity parameters from the coastal station Maitri, Antarctica

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dc.contributor.author Jeeva, K.
dc.contributor.author Sinha, A. K.
dc.contributor.author Seemala, Gopi K.
dc.contributor.author Pawar, S. D.
dc.contributor.author Guha, A.
dc.contributor.author Kamra, A. K.
dc.contributor.author Williams, E. R.
dc.contributor.author Ravichandran, M.
dc.date.accessioned 2023-08-07T07:52:52Z
dc.date.available 2023-08-07T07:52:52Z
dc.date.issued 2023
dc.identifier.citation JGR-Atmospheres, https://doi.org/10.1029/2022JD037696 en_US
dc.identifier.uri http://library.iigm.res.in:8080/xmlui/handle/123456789/1720
dc.description.abstract Atmospheric electricity parameters (AEP) measurements from Antarctica predominantly feature either the potential gradient (PG) and/or air-Earth current (AEC) density. We report for the first time simultaneous measurements of the bipolar ions concentration/conductivity, PG, and AEC density. AEP measurements were carried out at Maitri (70.8°S, 11.8°E) from December 2018 to November 2019. We formulated a few criteria, irrespective of the weather conditions, to select the electrically quiet days and some additional criteria based on the conductivity measurements to discern globally representative data (GRD) from such days. The measurements of the PG and AEC density over the Antarctic plateau demonstrated the diurnal curves similar to the Carnegie pattern, which represents the global thunderstorms and electrified shower clouds (ESCs) occurring on different continents and oceans, we regard the data having such trend as GRD. We found significant variability in the concentration of small bipolar ions/conductivity in the austral summer which in turn affects GRD. However, the concentration of bipolar ions is nearly consistent at ∼250 negative ions cm−3 and ∼300 positive ions cm−3 in winter and enhances the probability of GRD. Such differences can arise out of the prevalent planetary boundary layer processes in the two seasons. When the PG varied between ∼50 Vm−1 and ∼150 Vm−1 and the maximum range of conductivity variations was ∼0.2 × 10−14 ℧ m−1, the AEPs represented the signatures of the global thunderstorm and ESC activities. en_US
dc.language.iso en en_US
dc.subject Global electric circuit en_US
dc.subject Atmospheric electricity parameters en_US
dc.subject Fair weather en_US
dc.subject Maitri en_US
dc.subject Antarctica en_US
dc.title The global representativeness of fair-weather atmospheric electricity parameters from the coastal station Maitri, Antarctica en_US
dc.type Article en_US


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