Parametrization of the Relative Amplitude of Geomagnetic and Askaryan Radio Emission from Cosmic-Ray Air Showers using CORSIKA/CoREAS Simulations

E. Paudel, A. Coleman, F. Schroeder
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引用次数: 1

Abstract

Cosmic rays are messengers from highly energetic events in the Universe. These rare ultra-highenergy particles can be detected efficiently and in an affordable way using large arrays of radio antennas. Linearly polarized geomagnetic emission is the dominant emission mechanism produced when charged particles in air showers get deflected in the Earth’s magnetic field. The sub-dominant Askaryan emission is radially polarized and produced due to the time-varying negative-charge excess in the shower front. The relative amplitude of these two emission components depends on various air shower parameters, such as the arrival direction and the depth of the shower maximum. We studied these dependencies using CoREAS simulations of the radio emission from air showers at the South Pole using a star-shaped antenna layout. On the one hand, the parametrization of the Askaryan-to-geomagnetic ratio can be used as input for a more accurate reconstruction of the shower energy. On the other hand, if measured precisely enough, this ratio may provide a new method to reconstruct the atmospheric depth of the shower maximum.
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利用CORSIKA/CoREAS模拟宇宙射线空气阵雨地磁和阿斯卡良射电发射相对振幅的参数化
宇宙射线是宇宙中高能事件的信使。这些罕见的超高能量粒子可以使用大型无线电天线阵列以一种经济实惠的方式有效地探测到。线极化地磁发射是空气阵雨中的带电粒子在地球磁场中偏转时产生的主要发射机制。亚主导的阿斯卡良发射是径向极化的,是由于阵雨锋面中随时间变化的负电荷过剩而产生的。这两种发射分量的相对振幅取决于不同的风淋点参数,如到达方向和最大雨淋点深度。我们使用CoREAS模拟了南极的星形天线布局的空气阵雨的无线电发射,研究了这些依赖关系。一方面,阿斯卡良地磁比的参数化可以作为输入,更精确地重建阵雨能量。另一方面,如果测量得足够精确,这个比值可以提供一种重建最大流星雨的大气深度的新方法。
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