Dyer C S, Lei F, Clucas S N, Smart D F, Shea M A
Space Department, QinetiQ, Farnborough, UK.
Adv Space Res. 2003;32(1):81-93. doi: 10.1016/s0273-1177(03)90374-7.
Solar particle events can give greatly enhanced radiation at aircraft altitudes, but are both difficult to predict and to calculate retrospectively. This enhanced radiation can give significant dose to aircrew and greatly increase the rate of single event effects in avionics. Validation of calculations is required but only very few events have been measured in flight. The CREAM detector on Concorde detected the event of 29 September 1989 and also four periods of enhancement during the events of 19-24 October 1989. Instantaneous rates were enhanced by up to a factor ten compared with quiet-time cosmic rays, while flight-averages were enhanced by up to a factor six. Calculations are described for increases in radiation at aircraft altitudes using solar particle spectra in conjunction with Monte Carlo radiation transport codes. In order to obtain solar particle spectra with sufficient accuracy over the required energy range it is necessary to combine space data with measurements from a wide range of geomagnetically dispersed, ground-level neutron monitors. Such spectra have been obtained for 29 September 1989 and 24 October 1989 and these are used to calculate enhancements that are compared with the data from CREAM on Concorde. The effect of cut-off rigidity suppression by geomagnetic activity is shown to be significant. For the largest event on record on 23 February 1956, there are no space data but there are data from a number of ground-level cosmic-ray detectors. Predictions for all events show very steep dependencies on both latitude and altitude. At high latitude and altitude (17 km) calculated increases with respect to cosmic rays are a factor 70 and 500 respectively for 29 September 1989 and 23 February 1956. The levels of radiation for high latitude, subsonic routes are calculated, using London to Los Angeles as an example, and can exceed 1 mSv, which is significantly higher than for Concorde routes from Europe to New York. The sensitivity of the calculations to spectral fitting, geomagnetic activity and other assumptions demonstrates the requirement for widespread carriage of radiation monitors on aircraft.
太阳粒子事件会在飞机飞行高度产生大幅增强的辐射,但这种事件既难以预测,也难以进行追溯计算。这种增强的辐射会给机组人员带来显著剂量,并大幅增加航空电子设备中单次事件效应的发生率。虽然需要对计算结果进行验证,但在飞行中仅测量到极少数此类事件。协和式飞机上的宇宙射线高能电子和原子核成分探测器(CREAM)探测到了1989年9月29日的事件,以及1989年10月19日至24日事件期间的四个增强期。与平静时期的宇宙射线相比,瞬时辐射率提高了一个数量级,而飞行平均辐射率提高了一个数量级。文中描述了利用太阳粒子能谱结合蒙特卡罗辐射传输代码来计算飞机飞行高度辐射增加情况的方法。为了在所需能量范围内获得足够准确的太阳粒子能谱,有必要将空间数据与来自广泛分布于不同地磁位置的地面中子监测器的测量数据相结合。现已获得了1989年9月29日和1989年10月24日的此类能谱,并用于计算增强情况,将计算结果与协和式飞机上CREAM探测器的数据进行比较。结果表明,地磁活动对截止刚度的抑制作用显著。对于1956年2月23日有记录以来最大的事件,没有空间数据,但有来自多个地面宇宙射线探测器的数据。对所有事件的预测结果显示,辐射增强程度对纬度和高度都有非常强烈的依赖关系。在高纬度和高海拔(17千米)地区,对于1989年9月29日和1956年2月23日的事件,相对于宇宙射线计算得出的辐射增强倍数分别为70倍和500倍。以伦敦至洛杉矶航线为例,计算了高纬度亚音速航线的辐射水平,其可能超过1毫希沃特,这明显高于协和式飞机从欧洲至纽约航线的辐射水平。计算结果对能谱拟合、地磁活动及其他假设的敏感性表明,飞机上广泛配备辐射监测器是很有必要的。