Published April 11, 2023 | Version v1
Journal article Open

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

  • 1. Equatorial Geophysical Research Laboratory, Indian Institute of Geomagnetism, Krishnapuram, Tirunelveli 627 011, India
  • 2. Department of Physics School of Science, University of Bahrain, Bahrain
  • 3. Indian Institute of Geomagnetism, Panvel, Navi Mumbai 410 218, India
  • 4. Indian Institute of Tropical Meteorology, Dr. Homi Bhabha Road, Pashan, Pune, 411008.
  • 5. Department of Physics, Tripura University, Suryamaninagar 799022, India
  • 6. Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts, USA,
  • 7. Ministry of Earth Sciences, Prithvi Bhawan, Lodhi Road, New Delhi, 110 003

Description

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 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 x 10-14 mho m-1, the AEPs represented the signatures of the global thunderstorm and electrified shower cloud activities.

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