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子午工程首次火箭探空数据准单色惯性重力波特性分析
引用本文:王博, 胡雄, 肖存英, 史东波, 韦峰, 王欣颖, 王连忠. 子午工程首次火箭探空数据准单色惯性重力波特性分析[J]. 空间科学学报, 2017, 37(5): 547-553. doi: 10.11728/cjss2017.05.547
作者姓名:王博  胡雄  肖存英  史东波  韦峰  王欣颖  王连忠
作者单位:1. 中国科学院国家空间科学中心 北京 100190;;;2. 中国科学院大学 北京 100049
基金项目:国家重点研发计划项目(2016YFB0501503)和国家自然科学基金项目(41104099,41104100,41204137)共同资助
摘    要:

利用2010年6月3日子午工程首次气象火箭探测的温度和风场数据,采用矢端曲线法分别从平流层(20~50km)和对流层(0~15km)廓线提取了海南火箭发射场上空准单色惯性重力波参数.火箭探测的平流层和对流层两个准单色惯性重力波分别向上和向下逆风传播,固有周期为20.1h和22.4h,垂直波长为9.5km和4.0km,水平波长为2900km和753km,垂直群速度cgz为0.0887m·-1和0.0298m·-1,水平群速度cgh为12.7m·-1和3.65m·-1λh/λz为305:1和188:1,cgh/cgz为143:1和122:1.



关 键 词:准单色惯性重力波   固有周期   传播方向   气象火箭
收稿时间:2016-05-12
修稿时间:2017-07-27

Characteristics of Quasi-monochromatic Inertia Gravity Waves Revealed by First Meteorological Rocket Data of the Meridian Space Weather Monitoring Projectormalsize
WANG Bo, HU Xiong, XIAO Cunying, SHI Dongbo, WEI Feng, WANG Xinying, WANG Lianzhong. Characteristics of Quasi-monochromatic Inertia Gravity Waves Revealed by First Meteorological Rocket Data of the Meridian Space Weather Monitoring Projectormalsize[J]. Chinese Journal of Space Science, 2017, 37(5): 547-553. doi: 10.11728/cjss2017.05.547
Authors:WANG Bo  HU Xiong  XIAO Cunying  SHI Dongbo  WEI Feng  WANG Xinying  WANG Lianzhong
Affiliation:1. National Space Science Center, Chinese Academy of Sciences, Beijing 100190;;;2. University of Chinese Academy of Sciences, Beijing 100049
Abstract:Wind and temperature data detected by the first meteorological rocket of the Meridian Space Weather Monitoring Project were used to study quasi-monochromatic inertia Gravity Waves (GW) over Hainan rocket launch site (19.5°N, 109°E). The GW extracted from the stratosphere (troposphere) revealed by rocket sonde data is upward (downward) GW, and propagates against the background wind. The intrinsic period, vertical wavelength λz, horizontal wavelength λh, vertical group velocity cgz, and horizontal group velocity cgh of Stratospheric (Tropospheric) GW are 20.1h (22.4h), 9.5km (4km), 2900km (753km), 0.0887 (0.0298)m·-1, and 12.7 (3.65)m·-1, respectively. There is a significant difference between cgh/cgz and λhz because of the background wind. The value of λhz and cgh/cgz is 305:1 (188:1) and 143:1 (122:1) for the stratospheric (tropospheric) GW. 
Keywords:Quasi-monochromatic inertia gravity waves  Intrinsic period  Propagation direction  Meteorological rocket
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