大气密度对运载火箭飞行的qαmax精度影响及建模分析

基于运载火箭是在真实大气密度中飞行,本文以2017年8月1日-2019年7月31日高垂直分辨率探空资料为例,分析参考大气密度与真实大气密度、以及对应的qαmax之间差异特征,最后建立订正模型,研究结果表明:1)密度偏差、相对偏差随高度变化特征与季节有关,有较明显的年内变化特征;2)qαmax偏差随时间呈现"M"字型变化...     

地球低纬区边缘大气密度的预测

基于NRLMSISE-00大气模型讨论日地空间环境对地球低纬度地区边缘大气密度的影响,提出预测地球低纬地区边缘大气日平均密度的简化模型法和经验法。简化模型法利用地磁活动和太阳活动的11年准周期特性,通过预测地磁活动和太阳活动的变化规律以预测地球边缘大气密度。经验法则直接利用第23个太阳活动周期的日平均密度变化曲线经过傅里叶变换处理得到日平均密度变化规律曲线,然后将曲线拟合得到不同高度下的密度昼夜波动规律,再利用预测得到的日平均密度即可计算出具体当地时间对应的密度情况。误差分析说明经验预测法比简化模型法精度更高。两种方法均具有较高的精度并且使用方便,可用于地球边缘大气密度的工程化预测计算。     

基于精确星光大气折射观测模型的轨道摄动研究

基于星光折射间接敏感地平自主导航方法,改进了现有的大气密度模型和固定高度(25km)的观测模型,建立了自适应连续高度(20km～50km)的星光折射观测模型,并在此观测模型的基础上深入分析研究了影响导航精度的各种轨道摄动力,包括地球形状各阶摄动力、不同高度的大气阻力摄动力、太阳光辐射压力等.提出一种精简的大气模式--静止变标高球面大气,解决了由于高层大气密度的求解复杂,使大气阻力摄动模型不精确的问题,由此取得了较好的导航定位精度.利用UKF和EKF两种不同非线性算法,对考虑各种摄动力后的导航定位精度进行全面的计算机仿真实验,并就仿真结果进行了误差分析,同时研究了各种有关参数对导航精度的影响.     

基于无线电掩星观测的火星高层大气研究

近年来,火星高层大气受到越来越多的关注和研究。由于缺乏磁场的阻挡,火星高层大气与星际空间环境关联密切;同时,低层大气中的活动(例如尘暴)也会对其造成影响。而耦合在火星高层大气中的电离层则使这些过程变得更加复杂。火星高层大气和电离层结构的变化会对火星探测和通信活动造成很大的影响。然而,目前人们对火星高层大气100～130 km高度长期、稳定的观测数据仍然相对较少。文章将首先介绍火星高层大气研究的历史和现状,然后分别介绍本研究组利用无线电掩星实验获取火星130 km中性大气密度的方法、主要成果及未来的工作。     

充气式返回舱气动热特性研究

文章针对航天器返回实时性和经济性的需求,以充气式返回舱为研究对象,研究该飞行器从空间站返回过程中的气动特性,重点分析气动热特性。文章通过引入分子运动论、Kemp-Riddell方法、Linear桥函数等计算方法,建立起该飞行器在自由分子流区、过渡流区和连续流区高超声速情况下的表面热平衡方程,得出了该飞行器返回过程中的驻点热流密度和驻点壁面温度。计算分析了该飞行器最大直径D1和半锥角α等几何尺寸对其气动热特性的影响,得到在一定范围内增大D1和α可以有效减小驻点热流密度和驻点壁面温度,并研究在峰值加热高度附近70km、80km处不同马赫数下的气动热特性。在此基础上,依据热防护系统材料和布局,将气动加热计算的表面热流分布作为外壁边界条件,分析了结构材料层的温度变化特性。     

地磁扰动期间低轨目标轨道预报的误差修正

针对地磁扰动期间大气密度变化造成的低轨目标较大的轨道预报误差,提出一种根据POES卫星观测的极光能量注入数据改进短期轨道预报的方法。分析表明CHAMP卫星的沿迹大气密度及轨道衰减与极光能量注入具有较好的相关性。通过线性回归方法,建立轨道半长轴衰减及阻力调制系数的修正公式,并使用修正后的阻力调制系数取代两行元(TLE)中的该系数带入SGP4模型进行位置预报。该方案考虑了外推过程中地磁扰动引起的大气密度响应,能更准确地反映外推过程中大气阻力对轨道的影响。将其应用到2008年CHAMP卫星和国际空间站的轨道预报中,结果表明,半长轴和位置的预报误差可分别降低50%和30%左右。进一步对不同年份、不同轨道高度的目标进行了预报误差修正的分析,验证了该方法的普适性。     

分布式卫星轨道构形的大气摄动分析及修正方法

在低轨道运行的分布式卫星受大气摄动的影响,其轨道构形很快遭到破坏,环绕卫星的相对运动轨迹中心不断发生漂移。本研究的目的在于建立一种降低大气摄动对分布式卫星轨道构形影响的补偿方法,以使分布式卫星的轨道构形能够更好地自然维持。研究基于考虑高度变化和太阳周日变化的大气密度模型,得出分布式卫星不同初始相位环绕卫星的长半轴摄动方程。并提出一种补偿大气摄动影响的长半轴修正方法。仿真结果显示,采用此大气摄动补偿方法能够在给定时间内大大降低大气摄动的影响,从而显著提高分布式卫星轨道构形的自然维持能力。     

地球边缘大气密度时空特性分析

分析了地球边缘大气密度的时变特性及空间分布特性。从物理原因出发并基于NRLMSISE-00和MET-99大气模型计算随不同时空变量变化的相对大气密度,以说明各时空因素对地球边缘大气密度的影响程度。分析结果表明地球边缘大气密度具有较强的时变特性,昼夜和季节均对大气密度产生一定影响。空间特性表现为纬度对大气密度的影响明显,而经度影响微弱。季节不同导致纬度的影响程度不同,纬度因素在夏季和冬季的影响强于春秋。随着纬度的增加,季节对地球边缘大气密度的影响逐渐增强,而当地时间的影响呈减弱趋势。相比较而言,低纬区的昼夜波动强于季节波动,高纬区的季节波动强于昼夜波动。     

亚毫米波大气传输计算及分析

主要研究了在近亚毫米波段的大气传输特性，通过分析红外区和毫米波区的大气２模型，给出了亚毫米波段的大气传输模型参及加权项的表达形式。在吸收模型的理论的基础上，推导了以宏观气象条件为参变量的解析表达式，并由实验数据加权后的模型进行了验证分析，加权模型与实验数据基本吻合。在散射模型中，提出了以粒子的统计分布均值代替一般的密度分布，从而提高了计算精度。分别推导了Ｍｉｅ和Ｒａｙｌｅｉｇｈ散射系数求解的数学表     

地球扰动大气模型

本文介绍了地球扰动大气模型和建立该模型的方法。文中详细描述了该模型中，密度变化的各单个分量和风场变化的各单个分量，并给出了它们各自的计算公式。本大气扰动模型中包含了１３７个大气扰动状态方案，可供返回轨道计算、救生轨道计算和返回控制设计计算分别选用。     

variations of the atmospheric chemical composition in the earths’s polar regions after solar proton flare on July 14, 2000 (photochemical simulation)

Altitude—temporal cross-sections q(z, t) of atmospheric ionization rates by solar protons above the polar regions were calculated using the GOES-10 satellite data on solar proton fluxes for the period of solar proton flare (SPF) on July 14, 2000. The values of q(z, t) were used further in calculations of variations of the atmospheric chemical composition during the flare in the northern and southern polar regions (70°N and 70°S) by two different 1D photochemical models of the atmosphere (neutral and charged components). The calculation results have shown considerable variation of the ozone content after SPF: a decrease of [O3] was about 80% at altitudes of 65–75 km above northern and 25% in the layer of 55–65 km above the southern polar region. Such decrease of the ozone content is a result of reactions with [NO] and [OH] whose concentrations have grown substantially during SPF. According to calculations, the increase of electron concentration during SPF has reached 3–4 orders of magnitude at altitudes of 50–80 km. A comparison of the calculation results with the observational data on [NO], [NO2], and [O3] from the UARS and HALOE satellites for 70°N have shown a good qualitative correspondence, however, for variations of nitric oxides there are quantitative discrepancies.     

Coronal mass ejection (CME) activity of low mass M stars as an important factor for the habitability of terrestrial exoplanets. II. CME-induced ion pick up of Earth-like exoplanets in close-in habitable zones

Atmospheric erosion of CO2-rich Earth-size exoplanets due to coronal mass ejection (CME)-induced ion pick up within close-in habitable zones of active M-type dwarf stars is investigated. Since M stars are active at the X-ray and extreme ultraviolet radiation (XUV) wave-lengths over long periods of time, we have applied a thermal balance model at various XUV flux input values for simulating the thermospheric heating by photodissociation and ionization processes due to exothermic chemical reactions and cooling by the CO2 infrared radiation in the 15 microm band. Our study shows that intense XUV radiation of active M stars results in atmospheric expansion and extended exospheres. Using thermospheric neutral and ion densities calculated for various XUV fluxes, we applied a numerical test particle model for simulation of atmospheric ion pick up loss from an extended exosphere arising from its interaction with expected minimum and maximum CME plasma flows. Our results indicate that the Earth-like exoplanets that have no, or weak, magnetic moments may lose tens to hundreds of bars of atmospheric pressure, or even their whole atmospheres due to the CME-induced O ion pick up at orbital distances 相似文献   

Radiation dose and shielding for the Space Station

Significant differences in dose prediction for Space Station arise depending on whether or not the magnetic field model is extrapolated into the future. The basis for these calculations is examined in detail, and the importance of the residual atmospheric layer at altitudes below 1000 km, with respect to radiation attenuation is emphasized. Dosimetry results from Shuttle flights are presented and compared with the computed results. It is recommended that, at this stage, no extrapolation of the magnetic field into the future be included in the calculations. A model adjustment, to replace this arbitrary procedure is presented. Dose predictions indicate that, at altitudes below 500 km and at low inclination, and with nominal module wall thickness (0.125 in. aluminum), orbit stay times of 90 days in Space Station would result in quarterly radiation doses to the crew, which are well within present limits both for males and females. Countermeasures would be required for stay times of a year or more and the measure of increasing shielding is examined.     

Aerobraking at Venus: A science and technology enabler

Venus remains one of the great unexplored planets in our solar system, with key questions remaining on the evolution of its atmosphere and climate, its volatile cycles, and the thermal and magmatic evolution of its surface. One potential approach toward answering these questions is to fly a reconnaissance mission that uses a multi-mode radar in a near-circular, low-altitude orbit of ∼400 km and 60–70° inclination. This type of mission profile results in a total mission delta-V of ∼4.4 km/s. Aerobraking could provide a significant portion, potentially up to half, of this energy transfer, thereby permitting more mass to be allocated to the spacecraft and science payload or facilitating the use of smaller, cheaper launch vehicles.Aerobraking at Venus also provides additional science benefits through the measurement of upper atmospheric density (recovered from accelerometer data) and temperature values, especially near the terminator where temperature changes are abrupt and constant pressure levels drop dramatically in altitude from day to night.Scientifically rich, Venus is also an ideal location for implementing aerobraking techniques. Its thick lower atmosphere and slow planet rotation result in relatively more predictable atmospheric densities than Mars. The upper atmosphere (aerobraking altitudes) of Venus has a density variation of 8% compared to Mars' 30% variability. In general, most aerobraking missions try to minimize the duration of the aerobraking phase to keep costs down. These short phases have limited margin to account for contingencies. It is the stable and predictive nature of Venus' atmosphere that provides safer aerobraking opportunities.The nature of aerobraking at Venus provides ideal opportunities to demonstrate aerobraking enhancements and techniques yet to be used at Mars, such as flying a temperature corridor (versus a heat-rate corridor) and using a thermal-response surface algorithm and autonomous aerobraking, shifting many daily ground activities to onboard the spacecraft. A defined aerobraking temperature corridor, based on spacecraft component maximum temperatures, can be employed on a spacecraft specifically designed for aerobraking, and will predict subsequent aerobraking orbits and prescribe apoapsis propulsive maneuvers to maintain the spacecraft within its specified temperature limits. A spacecraft specifically designed for aerobraking in the Venus environment can provide a cost-effective platform for achieving these expanded science and technology goals.This paper discusses the scientific merits of a low-altitude, near-circular orbit at Venus, highlights the differences in aerobraking at Venus versus Mars, and presents design data using a flight system specifically designed for an aerobraking mission at Venus. Using aerobraking to achieve a low altitude orbit at Venus may pave the way for various technology demonstrations, such as autonomous aerobraking techniques and/or new science measurements like a multi-mode, synthetic aperture radar capable of altimetry and radiometry with performance that is significantly more capable than Magellan.     

Estimation of potential abilities of middle atmosphere density measurements from a near-Earth orbit within the UV wavelength range

Analysis of errors in atmospheric density measurements by lidar on board the ISS is performed. It is shown that using as the lidar transmitter a Nd:YAG laser with moderate parameters of emission at a wavelength of 353 nm and a receiving mirror diameter of 0.4 m, it is possible to cover with a 10% measurement error a height range, on average, from 40–60 km and 30–40 km in the nighttime and daytime, respectively, down to the troposphere. Working with emission at 266 nm with a 10% error, it is possible to move to the heights of the mesosphere (70 km) and penetrate the atmosphere down to a height of 40 km. Thus, the use of two harmonics makes it possible to assimilate the height range of atmospheric density measurements from on board the ISS beginning from 70 km and down to the troposphere.     

大气探测激光雷达组网观测一致性研究

通过激光遥感获取气溶胶、云垂直分布情况，对研究气溶胶、云微物理特性、辐射强迫效应以及污染物传输等具有重大意义。在实际应用中激光雷达受激光器能量、发散角以及透过率等影响，会导致各雷达面对同一目标物探测数据不一致。随着地基大气探测激光雷达逐步规模化、标准化，对雷达组网观测一致性开展研究具有重要意义。为保证组网激光雷达数据高质量和高可靠性，在雷达系统自标定基础上，利用太阳光度计、大气分子模型获取激光雷达系统常数，确保各激光雷达回波信号定量可比。通过激光雷达组网观测进行探测目标一致性比对试验，以验证激光雷达系统探测一致性精度。结果表明：标定后，532 nm距离修正信号在1~2 km区间相对偏差从64.89%降低到22.16%，在2~5 km区间相对偏差从49.26%降低到8.90%，在9.5~11.5 km相对偏差从46.83%降低到10.91%；532 nm退偏比在1~2 km区间相对偏差从69.68%降低到20.68%，在2~5 km区间相对偏差从71.24%降低到6.69%，在9.5~11.5 km相对偏差从140.24%降低到9.02%；532 nm后向散射系数在1~2 km区间相对偏差从37.45%降低到23.63%，在2~5 km区间相对偏差从29.15%降低到21.45%，在9.5~11.5 km相对偏差从76.02%降低到24.16%。组网激光雷达数据结果一致性较好，可在多站点进行高精度探测，在气候变化研究、碳排放监测和环境研究等领域发挥重要作用，为大规模大气变化规律研究提供高质量、有效数据。     

Characteristics of thermal ion outflows in the polar cap according to data of the <Emphasis Type="Italic">Interball-2</Emphasis> satellite

Characteristics of polar wind fluxes at a height of ∼20000 km measured by the Hyperboloid mass-spectrometer installed onboard the Interball-2 satellite are presented in the paper. The characteristics are presented for the upwelling flows of ionospheric ions H⁺, He⁺, and O⁺ from the sunlit polar cap in the period of solar activity minimum. Orbit segments with minimal precipitation of magnetospheric ions and electrons were preliminarily selected, and the measurements where the fluxes of ions coming from the cusp/cleft were excluded as carefully as possible. Thus, the densities, field-aligned velocities, and temperatures of ions in the regions where fluxes of polar wind could be detected with the maximal probability degree are presented in the paper. It is found that cases when only H⁺ ions are reaching the detector are with high probability the polar wind outflows. Their characteristics agree well with the Tube-7 hydrodynamic model and are as follows: n ≈ 1.5 cm⁻³, V _∥ ∼ 21 km/s; T _∥ = 3500 K, and T _⊥ = 2000 K. In cases when He⁺ and O⁺ ions are also detected, the temperatures are substantially higher than the model ones, and the measured field-aligned velocities of O⁺ fluxes are several times higher than the model ones. Moreover, it was revealed that the polar wind outflows are predominantly observed in the polar cap regions where the polar rain fluxes are very small.     

激光雷达系统仿真软件

从激光雷达约束条件入手 ,研究了通用激光雷达仿真模型 (GL M) ,其中包括大气传输模型、探测器噪声模型、发射与接收模型、目标反射数据库。着重分析、讨论了各种天气和系统条件下 ,对激光雷达性能的影响。根据模型 ,研制了通用仿真软件 ,最后给出了计算机仿真结果。     

Drying as one of the extreme factors for the microflora of the atmosphere

An investigation of the effects of drying and drying-rewetting cycles under vacuum conditions of 10(-2) torr at -30 degrees C on conidia of the atmospheric strain Penicillium chrysogenum from 48-77 km heights, collected by meteorological rockets found that survival and restoration of the initial physiological properties were possible through some very efficient protective cellular mechanisms. Such adaptive possibilities explain the widespread diffusion of microbial cells throughout the biosphere of our planet.