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Seasonal Variation of Polar Ice: Implications for Ultrahigh Energy Neutrino Detectors
The upper $100 \, \mathrm{m}$ to $150 \, \mathrm{m}$ of the polar ice sheet, called the firn, has a time-dependent density due to seasonal variations in the surface temperature, snow accumulation and surface melt events. We present RF simulations of an in-ice neutrino-induced radio source that show
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