HiCal 2: An instrument designed for calibration of the ANITA experiment and for Antarctic surface reflectivity measurements
arXiv:1710.11175 · doi:10.1016/j.nima.2018.11.092
Abstract
The NASA supported High-Altitude Calibration (HiCal)-2 instrument flew as a companion balloon to the ANITA-4 experiment in December 2016. Based on a HV discharge pulser producing radio-frequency (RF) calibration pulses, HiCal-2 comprised two payloads, which flew for a combined 18 days, covering 1.5 revolutions of the Antarctic continent. ANITA-4 captured over 10,000 pulses from HiCal, both direct and reflected from the surface, at distances varying from 100-800 km, providing a large dataset for surface reflectivity measurements. Herein we present details on the design, construction and performance of HiCal-2.
arXiv commentPublished in NIM-A, final version
References in corpus (3)
- The Antarctic Impulsive Transient Antenna Ultra-high Energy Neutrino Detector Design, Performance, and Sensitivity for 2006-2007 Balloon Flight
- Observation of Ultra-high-energy Cosmic Rays with the ANITA Balloon-borne Radio Interferometer
- Energy and Flux Measurements of Ultra-High Energy Cosmic Rays Observed During the First ANITA Flight
Cited by in corpus (9)
- Constraints on the ultra-high energy cosmic neutrino flux from the fourth flight of ANITA
- The Payload for Ultrahigh Energy Observations (PUEO): A White Paper
- A search for cosmogenic neutrinos with the ARIANNA test bed using 4.5 years of data
- Reflections On the Anomalous ANITA Events: The Antarctic Subsurface as a Possible Explanation
- Looking at the axionic dark sector with ANITA
- Long-baseline horizontal radio-frequency transmission through polar ice
- TAROGE-M: Radio Antenna Array on Antarctic High Mountain for Detecting Near-Horizontal Ultra-High Energy Air Showers
- Experimental tests of sub-surface reflectors as an explanation for the ANITA anomalous events
- General Treatment of Reflection of Spherical Electromagnetic Waves from a Spherical Surface and its Implications for the ANITA Anomalous Polarity Events