基于EON的卫星磁设计仿真系统研究

卫星磁设计的三维规划是一项艰难的任务,利用虚拟仿真平台EON开发的卫星磁设计仿真系统有效地解决了这一问题。论述了在卫星磁设计仿真系统的总体结构和开发方法,并对系统开发涉及的仿真程序与应用程序间的数据通信技术,碰撞检测技术和事件路由机制等关键技术进行描述,利用这些方法开发的磁试验仿真系统可以满足用户的要求,有效地进行卫星的磁设计工作。     

Satellite Measurements of Middle Atmospheric Impacts by Solar Proton Events in Solar Cycle 23

Solar cycle 23 was extremely active with seven of the largest twelve solar proton events (SPEs) in the past forty years recorded. These events caused significant polar middle atmospheric changes that were observed by a number of satellites. The highly energetic protons produced ionizations, excitations, dissociations, and dissociative ionizations of the background constituents in the polar cap regions (>60 degrees geomagnetic latitude), which led to the production of HO_x (H, OH, HO₂) and NO_y (N, NO, NO₂, NO₃, N₂O₅, HNO₃, HO₂NO₂, BrONO₂, ClONO₂). The HO_x increases led to short-lived ozone decreases in the polar mesosphere and upper stratosphere due to the short lifetimes of the HO_x constituents. Polar middle mesospheric ozone decreases greater than 50 % were observed and computed to last for hours to days due to the enhanced HO_x. The NO_y increases led to long-lived polar stratospheric ozone changes because of the long lifetime of the NO_y family in this region. Upper stratospheric ozone decreases of >10 % were computed to last for several months past the solar events in the winter polar regions because of the enhanced NO_y.     

一种基于通信事件的机载分布式软件调试方法

多应用分区的开发与综合是IMA系统开发的核心工作之一，而如何控制和调试基于分区间通信的分布式协作行为是关键所在。引入”通信事件”对分区间通信活动进行抽象，提出通信事件调试方法，对分区间通信的源分区和目的分区进行同步控制和对通信活动进行协同调试。进而提出一种将通信事件调试和代码调试有机结合的混合调试方法，论述了方法的调试过程以及在实践中表现出来的优点与不足。     

基于Master/Detail构架的航电专用配置工具设计与实现

本文重点讲述如何利用Master/Details结构来实现航电专用配置工具,并介绍了实现该结构所需要的软件和硬件环境,以及Master/Details结构的实现过程。以解析XSD文档生成解析树和配置文件为例,验证了Master/Details结构能够很好得支持航电专用配置工具的实现。     

Comparison of the transport codes HZETRN,HETC and FLUKA for a solar particle event

The protection of astronauts and instrumentation from galactic cosmic rays and solar particle events is one of the primary constraints associated with mission planning in low earth orbit or deep space. To help satisfy this constraint, several computational tools have been developed to analyze the effectiveness of various shielding materials and structures exposed to space radiation. These tools are now being carefully scrutinized through a systematic effort of verification, validation, and uncertainty quantification. In this benchmark study, the deterministic transport code HZETRN is compared to the Monte Carlo transport codes HETC-HEDS and FLUKA for a 30 g/cm² water target protected by a 20 g/cm² aluminum shield exposed to a parameterization of the February 1956 solar particle event. Neutron and proton fluences as well as dose and dose equivalent are compared at various depths in the water target. The regions of agreement and disagreement between the three codes are quantified and discussed, and recommendations for future work are given.     

FY-1C/D极轨气象卫星空间粒子成分监测器及其在轨探测结果

介绍了风云一号(FY-1)C，D极轨气象卫星空间粒子成分监测器的任务目标、主要功能和工程指标。以及数据的获取和处理方法。给出了空间环境宁静期、地磁扰动事件、太阳质子事件、与太阳活动的关系和粒子长期变化等探测结果，并进行了相应的分析。对C，D星空间粒子成分监测器分别进行的5年和第二次在轨测试结果表明，两星监测器工作正常、性能稳定，探测数据可靠。     

2000年7月空间天气大事件对地磁场的影响

2000年7月空间大事件对地磁场产生了巨大影响，7月15日至18日发生大磁暴(K=9)．磁暴为急始型，在我国地区初相期变幅有200—300nT，主相最大幅度有500—600nT，为多年来所罕见．在行星际磁场Bz由北向转向南向时，磁暴主相开始；南向分量达到最大值后大约2h，地磁H分量达到最小值，恢复相开始．并且，这次磁暴与太阳风也存在一定的对应关系。     

“风云一号（B）”卫星探测到的太阳质子事件

我国“风云一号(B)”气象卫星于1990年9月3日发射入轨,该星载有粒子成分监测器,用来探测空间粒子辐射环境,其中包括测量太阳耀斑时产生的太阳质子事件及其重粒子丰度;银河宇宙线异常成分与强度;内辐射带磁异常区的粒子通量及重粒子成分,“风云一号(B)”卫星运行半年来,我们已获取了上述有关的粒子辐射资料,在卫星上获得这些资料在我国尚属首次,本文主要分析观测到的太阳质子事件。     

AR5395和AR5629X射线事件的太阳射电辐射特征

ＡＲ５３９５和ＡＲ５６２９Ｘ射线事件的太阳射电辐射特征吴洪敖，孙九祯（中同科学院紫金山天文台，南京２１０００８）关键词太阳耀斑，Ｘ射线事件，射电事件一、概况本文选用的典型事件是１９８９年３月的ＡＲ５３９５和８月的ＡＲ５６２９的射电缓变和爆发分量，及其...     

First results of ozone profiles between 35 and 65 km retrieved from SCIAMACHY limb spectra and observations of ozone depletion during the solar proton events in October/November 2003

Ozone density profiles between 35 and 65 km altitude are derived from scattered sunlight limb radiance spectra measured by the SCIAMACHY instrument on the Envisat satellite. The method is based on the inversion of normalized limb radiance profiles in the Hartley absorption bands of ozone at selected wavelengths between 250 and 310 nm. It employs a non-linear Newtonian iteration version of Optimal Estimation (OE) coupled with the radiative transfer model SCIARAYS. The limb scatter technique combined with a classical OE retrieval in the short-wave UV-B and long-wave UV-C delivers reliable results as shown by a first comparison with MIPAS V4.61 profiles yielding agreement within 10% between 38 and 55 km. An overview of the methodology and an initial error analysis are presented. Furthermore the effect of the solar proton storm between 28 October and 6 November 2003 on the ozone concentration profiles is shown. They indicate large depletion of ozone of about 60% at 50 km in the Northern hemisphere, a weaker depletion in the Southern hemisphere and a dependence of the depletion on the Earth’s magnetic field.