...
首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Predictions of energetic particle radiation in the close Martian environment
【24h】

Predictions of energetic particle radiation in the close Martian environment

机译:近距离火星环境中高能粒子辐射的预测

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

Intense, prolonged solar flare activity during March 1989 was used to provide a retrospective scenario for predictions of associated interplanetary shocks and accompanying particle radiation at planet Mars. Shocks from five major flares were simulated to hit both the Earth and Mars during the interval 9–23 March 1989. The simulated scenario was provided by the Hakamada-Akasofu-Fry version 2 (HAFv.2) solar wind model. Since part of the generally required inputs for the model (specifically metric radio Type II coronal shock speeds) were not available, the shock speeds were iteratively determined via a “calibration” that uses limited IMP 8 particle and sudden storm commencement (SSC) data as proxies for shock arrival at the Earth. The shocks from four major solar flares were, thereby, found to arrive at Mars at times that are appropriate to explain solar energetic particle (SEP) and energetic storm particle (ESP) events recorded in situ by the particle radiation detector experiments Solar Low Energy Detector (SLED) and Low Energy Telescope (LET) aboard Phobos-2. Supporting measurements were provided by the magnetometer (MAGMA) and plasma spectrometer (TAUS) experiments. A gap in the spacecraft records occurred at the simulated time of arrival of the fifth flare-associated shock. There were some uncertainties attending the selection of certain of the events deemed to be “parent” flares. Such uncertainty can be expected in view of the incomplete set of energetic particle, plasma, and magnetic field measurements made at relevant times at both the Earth and Mars (the latter planet was then located at a distance of 1.6 AU, at about 78° east of the Sun-Earth line). Use of the HAFv.2 solar wind model affords a 4-day lead time between predicted and measured space weather events at Mars, with an error of approximately ±12 hours. Solar radiation events of the magnitude studied occur often enough to warrant consideration in the design of both manned and unmanned expeditions to Mars.
机译:1989年3月期间强烈的,长时间的太阳耀斑活动被用于提供回顾性情景,以预测相关的行星际撞击以及火星上伴随的粒子辐射。在1989年3月9日至23日之间,模拟了来自五个主要耀斑的冲击波袭击了地球和火星。模拟情景由Hakamada-Akasofu-Fry 2版(HAFv.2)太阳风模型提供。由于该模型通常无法提供部分输入(特定的II型无线电无线电冠状波冲击速度),因此通过“校准”来迭代确定冲击速度,该“校准”使用有限的IMP 8粒子和突如其来的暴风雨开始(SSC)数据作为冲击到达地球的代理。因此,发现了来自四个主要太阳耀斑的冲击到达火星的时间恰好可以解释由粒子辐射探测器实验现场记录的太阳高能粒子(SEP)和高能风暴粒子(ESP)事件。 (SLED)和低能量望远镜(LET)装在Phobos-2上。磁力计(MAGMA)和等离子体光谱仪(TAUS)实验提供了支持性测量。在模拟第五次耀斑相关冲击到达时,航天器记录出现了间隙。在选择某些被视为“父母”耀斑的事件时,存在一些不确定性。考虑到在相关时间在地球和火星上进行的高能粒子,等离子体和磁场测量的不完整集合,这样的不确定性可以预料到(后者的行星位于东约78°处,距离1.6 AU天地线的位置)。使用HAFv.2太阳风模型可以在火星预测和测量的太空天气事件之间提供4天的提前期,误差约为±12小时。如此数量级的太阳辐射事件经常发生,足以在设计载人和无人火星探险时考虑到。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号