Radar Absorption, Basal Reflection, Thickness, and Polarization Measurements from the Ross Ice Shelf
arXiv:1410.7134
Abstract
Radio-glaciological parameters from Moore's Bay, in the Ross Ice Shelf, have been measured. The thickness of the ice shelf in Moore's Bay was measured from reflection times of radio-frequency pulses propagating vertically through the shelf and reflecting from the ocean, and is found to be m. Introducing a baseline of 5437 m between radio transmitter and receiver allowed the computation of the basal reflection coefficient, , separately from englacial loss. The depth-averaged attenuation length of the ice column, is shown to depend linearly on frequency. The best fit (95% confidence level) is m (20 dB/km), for the frequencies [0.100-0.850] GHz, assuming no reflection loss. The mean electric-field reflection coefficient is (-1.7 dB reflection loss) across [0.100-0.850] GHz, and is used to correct the attenuation length. Finally, the reflected power rotated into the orthogonal antenna polarization is less than 5% below 0.400 GHz, compatible with air propagation. The results imply that Moore's Bay serves as an appropriate medium for the ARIANNA high energy neutrino detector.
10 pages, 6 figures
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- Development Toward a Ground-Based Interferometric Phased Array for Radio Detection of High Energy Neutrinos
- Reconstructing non-repeating radio pulses with Information Field Theory
- Improving sensitivity of the ARIANNA detector by rejecting thermal noise with deep learning
- The Next-Generation Radio Neutrino Observatory -- Multi-Messenger Neutrino Astrophysics at Extreme Energies
- Performance of the ARIANNA Hexagonal Radio Array