平流层飞艇艇务管理任务分析

针对平流层飞艇的特点，文章分析艇务管理的主要任务，并对艇务管理的任务特点探讨了艇务管理系统在设计时可采用的各种技术，为开展平流层飞艇的研制提供设计思路。     

平流层飞艇艇务管理任务分析

针对平流层飞艇的特点,文章分析艇务管理的主要任务,并对艇务管理的任务特点探讨了艇务管理系统在设计时可采用的各种技术,为开展平流层飞艇的研制提供设计思路。     

飞艇的信息战应用研究

飞艇广泛应用于预警、侦察、通讯、干扰等信息对抗领域,具有传统航空器无法取代的优势.分析了飞艇的信息化作战应用和国外的技术现状,并在此基础上,讨论了飞艇信息战应用的发展趋势和所涉及的一系列关键技术.     

平流层飞艇控制与推进技术

飞艇作为平流层平台可以实现无线通信、空间观测、大气测量以及军事侦察等目的。本文主要结合平流层的环境特点对平流层飞艇动力推进系统的组成和概念进行初步分析,并对飞艇在升空、浮空、回收过程中的飞行控制策略进行探讨,同时简要分析了控制系统的组成、控制难点和飞艇应急控制问题。     

平流层飞艇的结构健康监测系统初探

文章从介绍平流层飞艇的结构健康监测定义入手,说明了该系统研究的作用和意义以及工作原理。在分析平流层飞艇运行环境和结构可能的损伤模式的基础上,从工程应用角度出发,对结构健康监测系统方案展开了研究,探讨了平流层飞艇结构健康监测系统中的一些关键因素,为今后结构健康监测系统设计提供参考。     

基于阻力气动特性计算的飞艇艇身外形研究

采用SIMPLE算法、S-A湍流模型求解了三维不可压雷诺平均N-S方程,数值模拟了绕飞艇的低速不可压粘性流动,计算了不同艇身外形的阻力特性.本文方法计算结果与实验结果或其他文献的计算结果符合良好,可以用于飞艇的气动特性计算.通过对6个不同外形的相同体积飞艇阻力特性计算,得到了最佳艇身外形,表明本文方法可以用于艇身外形的选型设计.     

A Possible Transfer Mechanism for the 11-Year Solar Cycle to the Lower Stratosphere

Observational evidence of the 11-year solar cycle (SC) modulation of stratosphere temperatures and winds from the ERA-40 dataset is reviewed, with emphasis on the Northern winter hemisphere. A frequency modulation of sudden warming events is noted, with warmings occurring earlier in solar minimum periods than in solar maximum periods. The observed interaction between the influence of the SC and the quasi biennial oscillation (QBO) on the frequency of sudden warmings is noted as a possible clue for understanding their mechanism of influence. A possible transfer route for the 11-year solar cycle from the equatorial stratopause region to the lowest part of the stratosphere is proposed, via an influence on sudden warming events and the associated induced meridional circulation. SC and QBO composites of zonal wind anomalies show anomalous wind distributions in the subtropical upper stratosphere in early winter. Mechanistic model experiments are reviewed that demonstrate a sensitivity of sudden warmings to small wind anomalies in this region. Various diagnostics from these experiments are shown, including EP fluxes and their divergence and also the synoptic evolution of the polar vortex, in order to understand the mechanism of the influence. Some recent GCM experiments to investigate the SC/QBO interaction are also described. They simulate reasonably well the observed SC/QBO interaction of sudden warming events and appear to support the hypothesis that tropical/subtropical upper stratospheric wind anomalies are an important influence on the timing of sudden warmings.     

平流层长航时气球轨迹控制系统研究

首先介绍了平流层气球的应用意义及进行轨迹控制的必要性,然后描述了一种基于不同海拔风速差的轨迹控制方法,简要说明了平流层风速随海拔的变化规律,在此基础上研究了包括超压气球和轨迹控制系统在内的气球飞行系统各部分特点,最后简单分析了整个飞行系统的建模与仿真中的要点问题。结果表明,这种轨迹控制方法是一种几乎不需要消耗能源的有效轨迹控制方法,具有较高的应用价值和推广价值。     

A general calculation method to specify center-of-buoyancy for the stratospheric airship with multiple gas cells

As the lighter-than-air (LTA) flight vehicle, the stratospheric airship is a desirable platform to provide communication and surveillance services. During the ascent from sea-level to the mission altitude, the volume of the lifting gas may change significantly, which will result in the change of the center-of-buoyancy (CB). A general calculation method is developed to specify CB for the stratospheric airship with a double-ellipsoid hull and an arbitrary number of the gas cells. The cross-section-integral (CSI) method is used as a basic calculation scenario to specify CB. Considering the complexity in determining the boundary between the helium and air in the gas cell, a searching algorithm is put forward and the specification of CB can be conducted by the iterative calculation. As an important application, the stable condition of the pitch angle is analyzed when the change of CB is involved. Under different initial configurations, the stable pitch angle of the stratospheric airship during the ascent is specified and compared, which shows the advantages of the multi-gas-cell configuration. The results of this paper may provide an important reference for the engineering application of the stratospheric airship.     

Simulating planetary wave propagation to the upper atmosphere during stratospheric warming events at different mountain wave scenarios

Parameterization schemes of atmospheric normal modes (NMs) and orographic gravity waves (OGWs) have been implemented into the mechanistic Middle and Upper Atmosphere Model (MUAM) simulating atmospheric general circulation. Based on the 12-members ensemble of runs with the MUAM, a composite of the stratospheric warming (SW) has been constructed using the UK Met Office data as the lower boundary conditions. The simulation results show that OGW amplitudes increase at altitudes above 30 km in the Northern Hemisphere after the SW event. At altitudes of about 50 km, OGWs have largest amplitudes over North American and European mountain systems before and during the composite SW, and over Himalayas after the SW. Simulations demonstrate substantial (up to 50–70%) variations of amplitudes of stationary planetary waves (PWs) during and after the SW in the mesosphere-lower thermosphere of the Northern Hemisphere. Westward travelling NMs have amplitude maxima not only in the Northern, but also in the Southern Hemisphere, where these modes have waveguides in the middle and upper atmosphere. Simulated variations of PW and NM amplitudes correspond to changes in the mean zonal wind, EP-fluxes and wave refractive index at different phases of the composite SW events. Inclusion of the parameterization of OGW effects leads to decreases in amplitudes (up to 15%) of almost all SPWs before and after the SW event and their increase (up to 40–60%) after the SW in the stratosphere and mesosphere at middle and high northern latitudes. It is suggested that observed changes in NM amplitudes in the Southern Hemisphere during SW could be caused by divergence of increased southward EP-flux. This EP-flux increases due to OGW drag before SW and extends into the Southern Hemisphere.