Abstract

We present a statistical analysis of ULF (1-100 mHz) geomagnetic measurements conducted during years 2003- 2006 at the Italian/French base of Concordia at Dome C, close to the geomagnetic pole, and at the Italian base «Mario Zucchelli» at Terra Nova Bay, also located in the polar cap, but at lower latitude. Our analysis shows that high latitude ULF pulsation power is largely controlled by the solar wind speed. At Terra Nova Bay the power shows a maximum at local noon, clearly related to cusp and closed field lines phenomena. At few mHz, the polarization pattern indicates field line resonances driven, just equatorward with respect to the station, by waves propagating tailward; the polarization of higher frequency pulsations, mostly originated from interplanetary upstream waves, suggests waves propagating sunward from the night sector. At Dome C the wave power shows a small enhancement in the local morning, more pronounced for mid-frequency pulsations; the polarization pattern, at all frequencies, appears to indicate waves propagating sunward from the night sector, suggesting a propagation channel to the ground via the magnetotail lobes.

Highlights

  • Geomagnetic field measurements at very high latitudes are important to understand some physical processes controlling the energy transfer from the solar wind (SW) to the magnetosphere

  • This paper presents a statistical analysis of low and mid-frequency pulsations observed at DMC and at TNB during years 2003-2006, in the declining phase of the solar cycle and discuss the magnetic local time (MLT) dependence of the spectral power as well as the aspects of the polarization pattern

  • At TNB the ULF wave power and polarization are controlled by the position of the station which approaches closed field lines in the daytime hours and the cusp at noon

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Summary

Introduction

Geomagnetic field measurements at very high latitudes are important to understand some physical processes controlling the energy transfer from the solar wind (SW) to the magnetosphere. Several analyses of TNB data, available since 1994, have demonstrated that the polar cap is an active area for ULF wave activity in the low and mid frequency range, from Pc5 (1-7 mHz) up to Pc4 (7-22 mHz) and Pc3 (22-100 mHz) pulsations (Villante et al, 2000a; 2000b; Francia et al, 2005) According to these investigations, it is found that, independently of frequency, the ULF power maximizes around noon, when the station approaches the cusp and closed field lines; in conflict with simultaneous observations at a cusp station (South Pole, ~74°S), no evidence for substorm related activity is detected in the nighttime sector. This paper presents a statistical analysis of low and mid-frequency pulsations observed at DMC and at TNB during years 2003-2006, in the declining phase of the solar cycle and discuss the magnetic local time (MLT) dependence of the spectral power as well as the aspects of the polarization pattern

Instrumentation and data analysis
Observations and experimental results
Summary and conclusions
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