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2023年西北地区临近空间火箭探测数据分析评估

何阳 陈泰龙 黄江平

何阳, 陈泰龙, 黄江平. 2023年西北地区临近空间火箭探测数据分析评估[J]. 空间科学学报. doi: 10.11728/cjss2025.04.2024-0074
引用本文: 何阳, 陈泰龙, 黄江平. 2023年西北地区临近空间火箭探测数据分析评估[J]. 空间科学学报. doi: 10.11728/cjss2025.04.2024-0074
HE Yang, Chen Tailong, HUANG Jiangping. Analysis and Evaluation of Data from Near Space Meteorological Rocket Detection in Northwest Area (in Chinese). Chinese Journal of Space Science, 2025, 45(4): 1-10 doi: 10.11728/cjss2025.04.2024-0074
Citation: HE Yang, Chen Tailong, HUANG Jiangping. Analysis and Evaluation of Data from Near Space Meteorological Rocket Detection in Northwest Area (in Chinese). Chinese Journal of Space Science, 2025, 45(4): 1-10 doi: 10.11728/cjss2025.04.2024-0074

2023年西北地区临近空间火箭探测数据分析评估

doi: 10.11728/cjss2025.04.2024-0074 cstr: 32142.14.cjss.2024-0074
基金项目: 国家自然科学基金项目资助(42405065, 42275060)
详细信息
    作者简介:
    • 何阳 男, 1996年生, 四川成都人, 北京航空气象研究所工程师, 主要研究方向为临近空间和电离层大气环境. E-mail: heyang12357@sina.com
  • 中图分类号: P356

Analysis and Evaluation of Data from Near Space Meteorological Rocket Detection in Northwest Area

  • 摘要: 气象火箭是一种获取临近空间大气环境垂直分布精细结构的重要原位探测手段, 其探测结果具有比地基和天基遥感探测更高的精度, 客观评估其数据质量是各部门有效使用该探测数据的重要前提. 本文利用2023年冬季在西北地区进行的一次气象火箭探测, 获取了20~60 km高度区间内的气温、风场、密度和气压数据, 对热敏电阻测得的温度进行了偏差修正, 并将探测结果与遥感探测、经验预报模式以及再分析资料等数据进行了比对评估. 结果表明: 火箭探测风场结果与再分析数据吻合得较好, 并且能够更加准确地描述对应区域的精细大气环境; 火箭实测气温偏差在40 km以上逐渐凸显, 主要偏差项为电流加热项、温度滞后项以及气动加热项, 修正后的气温与参考数据吻合性较好, 不同来源的气温数据主要差异是平流层顶气温拐点出现的高度不同; 气压和密度结果的偏差随着高度的上升而增加. 分析认为, 本次火箭的探测数据质量较好, 精度较高, 通过对数据的分析评估验证了大气要素反演数学模型有效可靠.

     

  • 图  1  火箭探测轨迹的时间-高度曲线

    Figure  1.  Time-altitude curve of the rocket's detection trajectory

    图  2  火箭发上升(红色)和下降(蓝色)过程的水平运动轨迹

    Figure  2.  Horizontal movement trajectory of the rocket during its ascent (red) and descent (blue) process

    图  3  火箭下落过程中探空仪的速度-高度分布

    Figure  3.  Velocity-altitude distribution of the radiosonde during the rocket's descent

    图  4  火箭、HWM07和MERRA2数据风速风向的垂直分布

    Figure  4.  Vertical distribution of wind speed and direction in rocket, HWM07, and MERRA2 data

    图  5  火箭和MERRA2数据纬向风、经向风的垂直分布以及速度分量之差

    Figure  5.  Vertical distribution of zonal and meridional winds from the rocket and MERRA2 data, and the difference in velocity components between the two

    图  6  温度修正前后的垂直分布及各修正子项

    Figure  6.  Vertical distribution of temperature before and after correction, and each correction sub-item

    图  7  火箭、MERRA2、NRLMSISE-00、SABER数据的温度垂直分布以及温度偏差

    Figure  7.  Vertical distribution of temperature from rocket, MERRA2, NRLMSISE-00, and SABER, and the deviation between the rocket and the other three types of data

    图  8  火箭和MERRA2, NRLMSISE-00, SABER数据的密度垂直分布以及密度偏差分布

    Figure  8.  Vertical distribution of density from rocket, MERRA2, NRLMSISE-00, and SABER, and the deviation between the rocket and the other three types of data

    图  9  火箭和MERRA2, NRLMSISE-00, SABER数据的气压垂直分布以及气压偏差分布

    Figure  9.  Vertical distribution of pressure from rocket, MERRA2, NRLMSISE-00, and SABER, and the deviation between the rocket and the other three types of data

    表  1  原始探测数据不同高度区间的获取率

    Table  1.   Acquisition rate of the original detection data in different height intervals

    探测区段/km60~5050~4040~3030~20
    数据获取率/(%)99.599.699.699.6
    下载: 导出CSV
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出版历程
  • 收稿日期:  2024-06-06
  • 录用日期:  2025-06-30
  • 修回日期:  2024-11-29
  • 网络出版日期:  2024-12-02

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