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临近空间大气密度扰动对高超声速飞行器气动热环境的影响

程旋 肖存英 杜涛 胡雄 杨钧烽

程旋, 肖存英, 杜涛, 等 . 临近空间大气密度扰动对高超声速飞行器气动热环境的影响[J]. 北京航空航天大学学报, 2021, 47(4): 754-764. doi: 10.13700/j.bh.1001-5965.2020.0044
引用本文: 程旋, 肖存英, 杜涛, 等 . 临近空间大气密度扰动对高超声速飞行器气动热环境的影响[J]. 北京航空航天大学学报, 2021, 47(4): 754-764. doi: 10.13700/j.bh.1001-5965.2020.0044
CHENG Xuan, XIAO Cunying, DU Tao, et al. Influence of atmospheric density disturbance on aerothermodynamic environment of hypersonic vehicles in near space[J]. Journal of Beijing University of Aeronautics and Astronautics, 2021, 47(4): 754-764. doi: 10.13700/j.bh.1001-5965.2020.0044(in Chinese)
Citation: CHENG Xuan, XIAO Cunying, DU Tao, et al. Influence of atmospheric density disturbance on aerothermodynamic environment of hypersonic vehicles in near space[J]. Journal of Beijing University of Aeronautics and Astronautics, 2021, 47(4): 754-764. doi: 10.13700/j.bh.1001-5965.2020.0044(in Chinese)

临近空间大气密度扰动对高超声速飞行器气动热环境的影响

doi: 10.13700/j.bh.1001-5965.2020.0044
基金项目: 

中国科学院A类战略性先导科技专项 XDA17010301

国家自然科学基金 11872128

国家自然科学基金 91952111

国家空间科学中心“青年科技创新”课题 Y9211FAF3S

详细信息
    作者简介:

    程旋  男, 博士研究生。主要研究方向: 临近空间大气建模及应用

    肖存英  女, 博士, 教授, 博士生导师。主要研究方向: 临近空间大气环境

    通讯作者:

    肖存英, E-mail: xiaocunying@bnu.edu.cn

  • 中图分类号: V419;V219;P351;P421

Influence of atmospheric density disturbance on aerothermodynamic environment of hypersonic vehicles in near space

Funds: 

Strategic Priority Research Program of the Chinese Academy of Sciences XDA17010301

National Natural Science Foundation of China 11872128

National Natural Science Foundation of China 91952111

Youth Science and Technology Innovation Foundation of NSSC Y9211FAF3S

More Information
  • 摘要:

    基于TIMED/SABER 2002—2018年大气密度观测数据,统计分析了20~80 km大气密度扰动对高超声速飞行器飞行热环境的影响。根据驻点热流估算方法给出的大气密度变化量与热流变化量之间的关系,定性和定量分析了不同月份大气密度相对变化量引起的热流变化量在垂直和水平方向的分布特征。研究表明:SABER大气密度月年均值计算的热流相对USSA76在夏季半球中高纬度地区偏高,在冬季半球偏低。在夏季半球高纬度地区约80 km附近存在热流增量的极大值,南半球夏季的极大值高于北半球夏季,尤其在南半球1月份,热流偏高可达32.2%。在经度方向,热流分布在夏季半球差异较小,冬季半球差异较大;考虑真实大气中存在的扰动时,在南半球和北半球夏季80 km附近,SABER大气密度预测的热流分别比USSA76偏高可达40.7%和36.6%。在经度方向,大气扰动引起的热流经向分布差异显著。在飞行器设计时,大气扰动的影响不能忽略;高超声速飞行器飞行应避免在夏季穿越南半球和北半球,规避热流增加带来的风险。

     

  • 图 1  大气密度相对偏差与热流变化量的关系

    Figure 1.  Relationship between atmospheric density error and heating transfer variation

    图 2  不同月份大气密度纬圈平均值相对USSA76的偏差引起的热流变化量随纬度和高度的分布

    Figure 2.  Latitude-altitude distribution of heating transfer variations caused by error between zonal monthly mean atmospheric density and USSA76

    图 3  80 km高度大气密度月平均值相对USSA76的偏差引起的热流变化量随经度和纬度的分布

    Figure 3.  Latitude-longitude distribution of heating transfer variations caused by error between monthly mean atmospheric density at 80 km and USSA76

    图 4  大气密度扰动引起的最小热流变化量和最大热流变化量在不同月份随纬度和高度的分布

    Figure 4.  Latitude-altitude distribution of minimum and maximum heating transfer variations caused by atmospheric density disturbances in different months

    图 5  80 km高度大气密度扰动引起的最小热流变化量和最大热流变化量在不同月份随纬度和经度的分布

    Figure 5.  Latitude-longitude distribution of minimum and maximum heating transfer variations caused by atmospheric density disturbances at 80 km in different months

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出版历程
  • 收稿日期:  2020-02-21
  • 录用日期:  2020-03-27
  • 网络出版日期:  2021-04-20

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