Reflections on the anomalous ANITA events: the Antarctic subsurface as a possible explanation

被引:16
|
作者
Shoemaker, Ian M. [1 ]
Kusenko, Alexander [2 ,3 ]
Kuipers Munneke, Peter [4 ]
Romero-Wolf, Andrew [5 ]
Schroeder, Dustin M. [6 ,7 ]
Siegert, Martin J. [8 ,9 ]
机构
[1] Virginia Tech, Dept Phys, Ctr Neutrino Phys, Blacksburg, VA 24061 USA
[2] Univ Calif Los Angeles, Dept Phys & Astron, Los Angeles, CA 90095 USA
[3] Univ Tokyo, UTIAS, Kavli Inst Phys & Math Universe WPI, Kashiwa, Chiba 2778583, Japan
[4] Univ Utrecht, Inst Marine & Atmospher Res, Utrecht, Netherlands
[5] CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USA
[6] Stanford Univ, Dept Geophys, Stanford, CA 94305 USA
[7] Stanford Univ, Dept Elect Engn, Stanford, CA 94305 USA
[8] Imperial Coll London, Grantham Inst, London SW7 2AZ, England
[9] Imperial Coll London, Dept Earth Sci & Engn, London SW7 2AZ, England
关键词
Antarctic glaciology; Ice physics; Snow physics; LAKE VOSTOK; X-RAY; ICE; RADAR; PHASE; FIRN; LAYERS; MODEL; SNOW; WIDE;
D O I
10.1017/aog.2020.19
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The Antarctic Impulsive Transient Antenna (ANITA) balloon experiment was designed to detect radio signals initiated by high-energy neutrinos and cosmic ray (CR) air showers. These signals are typically discriminated by the polarization and phase inversions of the radio signal. The reflected signal from CRs suffer phase inversion compared to a direct 'tau neutrino' event. In this paper, we study subsurface reflection, which can occur without phase inversion, in the context of the two anomalous up-going events reported by ANITA. It is found that subsurface layers and firn density inversions may plausibly account for the events, while ice fabric layers and wind ablation crusts could also play a role. This hypothesis can be tested with radar surveying of the Antarctic region in the vicinity of the anomalous ANITA events. Future experiments should not use phase inversion as a sole criterion to discriminate between down-going and up-going events, unless the subsurface reflection properties are well understood.
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页码:92 / 98
页数:7
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