Abstract:Spectral Resonance Structures (SRS) of Ionospheric Alfven Resonator (IAR) are investigated by analysing the magnetic field data of a high sampling frequency induction coil magnetometer, installed at a low latitude Indian station, Shillong$$(25.56^\circ N, 91.86^\circ E, dipole L=1.08 )$$
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“…The Bharati (BRT) and Shillong (SHI) stations are operated by the Indian Institute of Geomagnetism. The low resolution (64 Hz) data from the low latitude SHI station in India have been used to study ionospheric Alfven resonances (IAR) (e.g., Adhitya et al., 2022) while high resolution (256 Hz) data from the Antarctic BRT station have been used to examine finer structures of electromagnetic ion cyclotron (EMIC) waves (e.g., Kakad et al., 2018; Upadhyay et al., 2022). The Eskdalemuir (ESK) station is operated by the British Geological Survey and is dedicated to study SRs and ionospheric Alfven resonances (see e.g., Beggan & Musur, 2018; Musur & Beggan, 2019).…”
Section: Methodsmentioning
confidence: 99%
“…The Bharati (BRT) and Shillong (SHI) stations are operated by the Indian Institute of Geomagnetism. The low resolution (64 Hz) data from the low latitude SHI station in India have been used to study ionospheric Alfven resonances (IAR) (e.g., Adhitya et al, 2022) while high resolution (256 Hz) 1.…”
The importance of lightning has long been recognized from the point of view of climate-related phenomena. However, the detailed investigation of lightning on global scales is currently hindered by the incomplete and spatially uneven detection efficiency of ground-based global lightning detection networks and by the restricted spatio-temporal coverage of satellite observations. We are developing different methods for investigating global lightning activity based on Schumann resonance (SR) measurements. SRs are global electromagnetic resonances of the Earth-ionosphere cavity maintained by the vertical component of lightning. Since charge separation in thunderstorms is gravity-driven, charge is typically separated vertically in thunderclouds, so every lightning flash contributes to the measured SR field. This circumstance makes SR measurements very suitable for climate-related investigations. In this study, 19 days of global lightning activity in January 2019 are analyzed based on SR intensity records from 18 SR stations and the results are compared with independent lightning observations provided by ground-based (WWLLN, GLD360, and ENTLN) and satellite-based (GLM, LIS/OTD) global lightning detection. Daily average SR intensity records from different stations exhibit strong similarity in the investigated time interval. The inferred intensity of global lightning activity varies by a factor of 2-3 on the time scale of 3-5 days which we attribute to continental-scale temperature changes related to cold air outbreaks from polar regions. While our results demonstrate that the SR phenomenon is a powerful tool to investigate global lightning, it is also clear that currently available technology limits the detailed quantitative evaluation of lightning activity on continental scales.
Plain Language SummaryLightning is recognized as a climate variable indicating the changing climate of the Earth. Surface temperature changes on the order of 1°C can result in a significant change in lightning frequency. Lightning activity is monitored on a global scale by satellites and by ground-based global lightning detection networks. However, the detection efficiency of these available technologies is limited which restricts the investigation of global lightning activity especially on the day-to-day time scale. In this study, we propose an alternative method to monitor day-to-day changes in global lightning activity based on Schumann resonance measurements and thus we compare SR-based observations with available global lightning monitoring techniques. We show that the overall intensity of global lightning activity can vary considerably (by a factor of 2-3) within a few days, further motivating our efforts to monitor such changes and understand BOZÓKI ET AL.
“…The Bharati (BRT) and Shillong (SHI) stations are operated by the Indian Institute of Geomagnetism. The low resolution (64 Hz) data from the low latitude SHI station in India have been used to study ionospheric Alfven resonances (IAR) (e.g., Adhitya et al., 2022) while high resolution (256 Hz) data from the Antarctic BRT station have been used to examine finer structures of electromagnetic ion cyclotron (EMIC) waves (e.g., Kakad et al., 2018; Upadhyay et al., 2022). The Eskdalemuir (ESK) station is operated by the British Geological Survey and is dedicated to study SRs and ionospheric Alfven resonances (see e.g., Beggan & Musur, 2018; Musur & Beggan, 2019).…”
Section: Methodsmentioning
confidence: 99%
“…The Bharati (BRT) and Shillong (SHI) stations are operated by the Indian Institute of Geomagnetism. The low resolution (64 Hz) data from the low latitude SHI station in India have been used to study ionospheric Alfven resonances (IAR) (e.g., Adhitya et al, 2022) while high resolution (256 Hz) 1.…”
The importance of lightning has long been recognized from the point of view of climate-related phenomena. However, the detailed investigation of lightning on global scales is currently hindered by the incomplete and spatially uneven detection efficiency of ground-based global lightning detection networks and by the restricted spatio-temporal coverage of satellite observations. We are developing different methods for investigating global lightning activity based on Schumann resonance (SR) measurements. SRs are global electromagnetic resonances of the Earth-ionosphere cavity maintained by the vertical component of lightning. Since charge separation in thunderstorms is gravity-driven, charge is typically separated vertically in thunderclouds, so every lightning flash contributes to the measured SR field. This circumstance makes SR measurements very suitable for climate-related investigations. In this study, 19 days of global lightning activity in January 2019 are analyzed based on SR intensity records from 18 SR stations and the results are compared with independent lightning observations provided by ground-based (WWLLN, GLD360, and ENTLN) and satellite-based (GLM, LIS/OTD) global lightning detection. Daily average SR intensity records from different stations exhibit strong similarity in the investigated time interval. The inferred intensity of global lightning activity varies by a factor of 2-3 on the time scale of 3-5 days which we attribute to continental-scale temperature changes related to cold air outbreaks from polar regions. While our results demonstrate that the SR phenomenon is a powerful tool to investigate global lightning, it is also clear that currently available technology limits the detailed quantitative evaluation of lightning activity on continental scales.
Plain Language SummaryLightning is recognized as a climate variable indicating the changing climate of the Earth. Surface temperature changes on the order of 1°C can result in a significant change in lightning frequency. Lightning activity is monitored on a global scale by satellites and by ground-based global lightning detection networks. However, the detection efficiency of these available technologies is limited which restricts the investigation of global lightning activity especially on the day-to-day time scale. In this study, we propose an alternative method to monitor day-to-day changes in global lightning activity based on Schumann resonance measurements and thus we compare SR-based observations with available global lightning monitoring techniques. We show that the overall intensity of global lightning activity can vary considerably (by a factor of 2-3) within a few days, further motivating our efforts to monitor such changes and understand BOZÓKI ET AL.
“…This is called a spectral resonance structure (SRS) and was found by Belyaev et al [1,2] for the first time at a midlatitude station with an L value of 2.65. The SRSs were detected at high (L ¼ 5.2) [3], mid (L ¼ 2.1) [4], and low latitudes (L ¼ 1.3, 1.2, 1.08) [5][6][7]. All the SRSs were observed during the night [3][4][5][6][7], and the occurrence rate was high during the September to January periods [3,4].…”
Section: Introductionmentioning
confidence: 94%
“…The SRSs were detected at high (L ¼ 5.2) [3], mid (L ¼ 2.1) [4], and low latitudes (L ¼ 1.3, 1.2, 1.08) [5][6][7]. All the SRSs were observed during the night [3][4][5][6][7], and the occurrence rate was high during the September to January periods [3,4]. The frequency difference between adjacent maxima increased in winter [4,5].…”
The data were obtained using an induction magnetometer with the sensor placed in the North-South direction at a sampling frequency of 128 Hz, and they were Fourier transformed every 8 s, and averaged for 2 min. The dynamic spectra showed structured enhancements at approximately 1, 2, 2.5, 3.5, and 4.5 Hz. The occurrence of the spectral resonance structure in Kawatabi was restricted to the nighttime from 17 to 06 LT. Although the data coverage was limited to as low as 51%, nearly two decades of observations show a clear anticorrelation between the occurrence of the spectral resonance structures and the sunspot number, which is consistent with the model of an ionospheric cavity with minimum Alfvén velocity.
“…The BRT and SHI stations are operated by the Indian Institute of Geomagnetism. The low resolution (64 Hz) data from the low latitude SHI station in India have been used to study ionospheric Alfven resonances (IAR) (e.g., Adhitya et al, 2022) while high resolution ( 256Hz) data from the Antarctic BRT station have been used to examine finer structures of electromagnetic ion cyclotron (EMIC) waves (e.g., .…”
The importance of lightning has long been recognized from the point of
view of climate-related phenomena. However, the detailed investigation
of lightning on global scales is currently hindered by the incomplete
and spatially uneven detection efficiency of ground-based global
lightning detection networks and by the restricted spatio-temporal
coverage of satellite observations. We are developing different methods
for investigating global lightning activity based on Schumann resonance
(SR) measurements. SRs are global electromagnetic resonances of the
Earth-ionosphere cavity maintained by the vertical component of
lightning. Since charge separation in thunderstorms is gravity-driven,
charge is typically separated vertically in thunderclouds, so every
lightning flash contributes to the measured SR field. This circumstance
makes SR measurements very suitable for climate-related investigations.
In this study, 19 days of global lightning activity in January 2019 are
analyzed based on SR intensity records from 18 SR stations and the
results are compared with independent lightning observations provided by
ground-based (WWLLN, GLD360 and ENTLN) and satellite-based (GLM,
LIS/OTD) global lightning detection. Daily average SR intensity records
from different stations exhibit strong similarity in the investigated
time interval. The inferred intensity of global lightning activity
varies by a factor of 2-3 on the time scale of 3-5 days which we
attribute to continental-scale temperature changes related to cold air
outbreaks from polar regions. While our results demonstrate that the SR
phenomenon is a powerful tool to investigate global lightning, it is
also clear that currently available technology limits the detailed
quantitative evaluation of lightning activity on continental scales.
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