留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

中层顶准单色重力波特性的钠荧光多普勒激光雷达观测分析

王博,  胡雄,  闫召爱,  肖存英,  郭商勇,  程永强,  郭文杰

downloadPDF
文章导航 > 红外与激光工程  > 2017 >  46(5): 506002-0506002(8)
王博, 胡雄, 闫召爱, 肖存英, 郭商勇, 程永强, 郭文杰. 中层顶准单色重力波特性的钠荧光多普勒激光雷达观测分析[J]. 红外与激光工程, 2017, 46(5): 506002-0506002(8). doi: 10.3788/IRLA201746.0506002
引用本文: 王博, 胡雄, 闫召爱, 肖存英, 郭商勇, 程永强, 郭文杰. 中层顶准单色重力波特性的钠荧光多普勒激光雷达观测分析[J]. 红外与激光工程, 2017, 46(5): 506002-0506002(8). doi: 10.3788/IRLA201746.0506002
shu
Wang Bo, Hu Xiong, Yan Zhaoai, Xiao Cunying, Guo Shangyong, Cheng Yongqiang, Guo Wenjie. Observational study of quasi-monochromatic gravity waves characteristics in mesopause region with sodium fluorescence Doppler lidar[J]. Infrared and Laser Engineering, 2017, 46(5): 506002-0506002(8). doi: 10.3788/IRLA201746.0506002
Citation: Wang Bo, Hu Xiong, Yan Zhaoai, Xiao Cunying, Guo Shangyong, Cheng Yongqiang, Guo Wenjie. Observational study of quasi-monochromatic gravity waves characteristics in mesopause region with sodium fluorescence Doppler lidar[J]. Infrared and Laser Engineering, 2017, 46(5): 506002-0506002(8). doi: 10.3788/IRLA201746.0506002
shu

中层顶准单色重力波特性的钠荧光多普勒激光雷达观测分析

doi: 10.3788/IRLA201746.0506002
  • 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: 

国家自然科学基金（41104099，41104100，41204137）

详细信息
    作者简介:

    王博(1987-),男,博士生,主要从事临近空间大气物理方面的研究。Email:wangbocas@163.com

    通讯作者: 胡雄(1967-),男,研究员,博士生导师,主要从事临近空间环境建模、预报、探测方面的研究。Email:xhu@nssc.ac.cn

  • 中图分类号: P356

Observational study of quasi-monochromatic gravity waves characteristics in mesopause region with sodium fluorescence Doppler lidar

  • 1.

    National Space Science Center,Chinese Academy of Sciences,Beijing 100190,China;

  • 2.

    University of Chinese Academy of Sciences,Beijing 100049,China

  • 摘要: 利用2011~2013年期间60 h的钠荧光多普勒激光雷达温度和风场数据，采用矢端曲线法提取廊坊上空85~95 km中层顶区域准单色惯性重力波的所有参量，并统计准单色大气重力波的活动特性。获得的85次准单色重力波事件中，上传（下传）重力波64次（21次），占总数的75。29%（24。71%）。垂直波长（水平波长）和观测周期平均值分别为6。6 km（727。8 km）和7。4 h，分别集中在6~9 km（200~800 km）和2~7 h，固有周期平均值为7。76 h，主要集中在3~9 h，水平传播方向分布比较均匀，没有占主导的传播方向。对于上传重力波，水平背景风在大气重力波水平传播方向上的分量取正值和取负值的概率大致相等，但对于下传重力波，该风场分量取正值的概率大约是取负值的2倍，说明观测到的下传大气重力波在中层顶区域多为顺风传播。
    Abstract: The quasi-monochromatic gravity waves （QM GWs)parameters in the mesopause region over Langfang (39.4N, 116.6E) were studied based on the 60 h sodium fluorescence Doppler lidar data during 2011-2013 year. A total of 85 QM GWs were extracted from the simultaneously measured temperature and wind profiles between 85 km and 95 km using hodograph method. The result shows that vertical wavelengths (horizontal wavelengths) and observed periods are mainly distributed from 6 km to 9 km (200 km to 800 km) and 2 h to 7 h, with the mean values 6.6 km (727.8 km) and 7.4 h respectively. GWs propagating upward in the vertical direction are with an occurrence of 75.29%. The intrinsic periods are mainly distributed from 3 h to 9 h with a mean value 7.76 h. There is no dominant horizontal propagation direction. The probability of the horizontal background wind component along the horizontal propagate direction Up0 is about 50% for upward GWs, but for downward GWs the probability of Up0 is about 66.66%, which is about 2 times of the probability of Up0 (33.33%)，which suggests that the observed downward GWs are mainly propagating horizontally along the wind.
  • [1] Kaifler B, Lbken F J, Hffner J, et al. Lidar observations of gravity wave activity in the middle atmosphere over Davis (69S, 78E), Antarctica[J]. Journal of Geophysical Research:Atmospheres, 2015, 120(10):4506-4521.
    [2] Schirber S, Manzini E, Krismer T, et al. The quasi-biennial oscillation in a warmer climate:sensitivity to different gravity wave parameterizations[J]. Climate Dynamics, 2015, 45(3-4):825-836.
    [3] Li T, She C Y, Liu H L, et al. Sodium lidar-observed strong inertia-gravity wave activities in the mesopause region over Fort Collins, Colorado (41N, 105W)[J]. Journal of Geophysical Research:Atmospheres, 2007, 112(D22):104-1.
    [4] Zhang S D, Yi F, Huang C M, et al. Latitudinal and altitudinal variability of lower atmospheric inertial gravity waves revealed by US radiosonde data[J]. Journal of Geophysical Research:Atmospheres, 2013, 118(14):7750-7764.
    [5] Kramer R, Wst S, Schmidt C, et al. Gravity wave characteristics in the middle atmosphere during the CESAR campaign at Palma de Mallorca in 2011/2012:Impact of extratropical cyclones and cold fronts[J]. Journal of Atmospheric and Solar-Terrestrial Physics, 2015, 128(5):8-23.
    [6] Gong S, Zeng X, Xue X, et al. First time observation of sodium layer over Wuhan, China by sodium fluorescence lidar[J]. Science in China Series A:Mathematics, 1997, 40(11):1228-1232.
    [7] Yi F, Zhang S, Zeng H, et al. Lidar observations of sporadic Na layers over Wuhan (30.5N, 114.4E)[J]. Geophysical Research Letters, 2002, 29(9):59-1.
    [8] Dou X K, Xue X H, Chen T D, et al. A statistical study of sporadic sodium layer observed by sodium lidar at Hefei (31.8 N, 117.3 E)[J]. Annales Geophysicae, 2009, 27(6):2247-2257.
    [9] Xue X H, Dou X K, Lei J, et al. Lower thermospheric-enhanced sodium layers observed at low latitude and possible formation:Case studies[J]. Journal of Geophysical Research:Space Physics, 2013, 118(5):2409-2418.
    [10] She C Y, Sherman J, Yuan T, et al. The first 80-hour continuous lidar campaign for simultaneous observation of mesopause region temperature and wind[J]. Geophysical Research Letters, 2003, 30(6):52.
    [11] Gardner C S, Voelz D G. Lidar studies of the nighttime sodium layer over Urbana, Illinois:2. Gravity waves[J]. Journal of Geophysical Research:Space Physics, 1987, 92(A5):4673-4694.
    [12] Beatty T J, Hostetler C A, Gardner C S. Lidar observations of gravity waves and their spectra near the mesopause and stratopause at Arecibo[J]. Journal of the Atmospheric Sciences, 1992, 49(6):477-496.
    [13] Collins R L, Hallinan T J, Smith R W, et al. Lidar observations of a large high-altitude sporadic Na layer during active aurora[J]. Geophysical Research Letters, 1996, 23(24):3655-3658.
    [14] Yang G, Clemesha B, Batista P, et al. Gravity wave parameters and their seasonal variations derived from Na lidar observations at 23 S[J]. Journal of Geophysical Research:Atmospheres, 2006, 111(D21):107-1.
    [15] Yang G, Clemesha B, Batista P, et al. Lidar study of the characteristics of gravity waves in the mesopause region at a southern low-latitude location[J]. Journal of Atmospheric and Solar-Terrestrial Physics, 2008, 70(7):991-1011.
    [16] Ai Yong, Lu Shu, Zhang Xunjie, et al. Lidar observations of gravity wave activity and spectra in the mesopause region at Wuhan, China[J]. Science in China Series A:Mathematics, 1998, 28(9):818-822
    [17] Song Juan, Cheng Xuewu, Yang Guotao, et al. The investigation of gravity wave activities on mesopause over Wuhan by sodium lidar[J]. Chin J Sapce Sci, 2005, 25(6):522-528. (in Chinese)宋娟, 程学武, 杨国韬, 等. 武汉上空中层顶大气重力波活动的钠层荧光激光雷达观测研究[J]. 空间科学学报, 2005, 25(6):522-528.
    [18] Gong S, Yang G, Xu J, et al. Statistical characteristics of atmospheric gravity wave in the mesopause region observed with a sodium lidar at Beijing, China[J]. Journal of Atmospheric and Solar-Terrestrial Physics, 2013, 97(5):143-151.
    [19] Gong Shaohua, Liu Zhengkuan, Guan Sai, et al. Lidar study on the parameter relations of gravity waves in themesopause region at Beijing[J]. Infrared and Laser Engineering, 2015, 44(4):1134-1140. (in Chinese)龚少华, 刘正宽, 关塞, 等. 北京上空中层顶区域重力波参数关系的激光雷达研究[J]. 红外与激光工程, 2015, 44(4):1134-1140.
    [20] Zou Xu, Yang Guotao, Wang Jihong, et al. Gravity wave parameters and their seasonal variatins derived from Na lidar observations at Hainan,China[J]. Chinese J Geophys, 2015, 58(7):2274-2282. (in Chinese)邹旭, 杨国韬, 王继红, 等. 基于激光雷达手段的海南地区重力波与其波谱的季节分布特性研究[J]. 地球物理学报, 2015, 58(7):2274-2282.
    [21] Hu X, Yan Z A, Guo S Y, et al. Sodium fluorescence Doppler lidar to measure atmospheric temperature in the mesopause region[J]. Chinese Science Bulletin, 2011, 56(4-5):417-423.
    [22] Yan Zhaoai. Research on sodium fluorescence Doppler lidar system[D]. Beijing:Graduate School of Chinese Academy of Sciences, 2010. (in Chinese)闫召爱. 钠荧光多普勒激光雷达系统的研究[D]. 北京:中国科学院研究生院, 2010.
    [23] Fang Xin. Sodium temperature and wind lidar development and gravity wave momentum flux observation[D]. Hefei:University of Science and Technology of China, 2012. (in Chinese)方欣. 钠测温测风激光雷达的研制及重力波动量通量的探测[D]. 合肥:中国科学技术大学, 2012.
    [24] Li T, Fang X, Liu W, et al. Narrowband sodium lidar for the measurements of mesopause region temperature and wind[J]. Applied Optics, 2012, 51(22):5401-5411.
    [25] Yang W M. Gravity wave studies of the mesopause region using a Na wind/temperature lidar[D]. Illinois:University of Illinois,1998.
    [26] Hu X, Liu A Z, Gardner C S, et al. Characteristics of quasi-monochromatic gravity waves observed with Na lidar in the mesopause region at Starfire Optical Range, NM[J]. Geophysical Research Letters, 2002, 29(24):22-1-22-4.
    [27] Xu Li, Hu Xiong, Yan Zhaoai, et al. Retrieval method of atmospheric parameters for a Sodium Doppler lidar[J]. Infrared and Laser Engineering, 2009, 38(1):140-143. (in Chinese)徐丽, 胡雄, 闫召爱, 等. 钠多普勒激光雷达大气参数反演方法[J]. 红外与激光工程, 2009, 38(1):140-143.
    [28] Xu Li, Hu Xiong, Cheng Yongqiang, et al. Simulation of echo-photon counts of a Sodium Doppler lidar and retrievals of atmospheric parameters[J]. Chinese J Geophys, 2010, 53(7):1520-1528. (in Chinese)徐丽, 胡雄, 程永强, 等. 钠多普勒激光雷达回波光子数仿真及大气参数反演[J]. 地球物理学报, 2010, 53(7):1520-1528.
    [29] Zhang S D, Yi F. A statistical study of gravity waves from radiosonde observations at Wuhan (30 N, 114 E) China[J]. Annales Geophysicae, 2005, 23(3):665-673.
    [30] Allen S J, Vincent R A. Gravity wave activity in the lower atmosphere:Seasonal and latitudinal variations[J]. Journal of Geophysical Research:Atmospheres, 1995, 100(D1):1327-1350.
    [31] Gardner C S, Taylor M J. Observational limits for lidar, radar and airglow imager measurements of gravity wave parameters[J]. Journal of Geophysical Research, 1998, 103(D6):6427-6437.
  • [1] 李乘, 吴德成, 刘爽, 邓迁, 秘国江, 王邦新, 王珍珠, 刘东, 王英俭.  铁共振荧光多普勒激光雷达光源的频率稳定性研究 . 红外与激光工程, 2023, 52(10): 20230025-1-20230025-8. doi: 10.3788/IRLA20230025
    [2] 闫召爱, 胡雄, 郭文杰, 郭商勇, 程永强, 张炳炎, 陈志芳, 赵尉博.  临近空间多普勒激光雷达技术及其应用（特邀） . 红外与激光工程, 2021, 50(3): 20210100-1-20210100-10. doi: 10.3788/IRLA20210100
    [3] 张玮钒, 颜昌翔, 高志良, 王思宇, 申箫, 袁静, 董有志.  二自由度快速控制反射镜系统固有频率优化设计 . 红外与激光工程, 2021, 50(6): 20200450-1-20200450-12. doi: 10.3788/IRLA20200450
    [4] 魏天问, 夏海云.  基于相干多普勒激光雷达的风雨同时探测 . 红外与激光工程, 2020, 49(S2): 20200406-20200406. doi: 10.3788/IRLA20200406
    [5] 王元祖, 韩於利, 孙东松, 韩飞, 周安然, 张楠楠, 唐磊.  我国中纬度地区多普勒激光雷达准零风层多季节观测与分析 . 红外与激光工程, 2020, 49(3): 0305004-0305004-8. doi: 10.3788/IRLA202049.0305004
    [6] 张楠楠, 赵若灿, 孙东松, 韩淤利, 陈冲.  基于瑞利多普勒激光雷达的惯性重力波长期观测研究 . 红外与激光工程, 2020, 49(S2): 20200351-20200351. doi: 10.3788/IRLA20200351
    [7] 李明, 张晓光, 李璞.  惯性稳定平台固有特性参数辨识 . 红外与激光工程, 2019, 48(S1): 89-96. doi: 10.3788/IRLA201948.S117004
    [8] 陈冲, 孙东松, 陈廷娣, 韩於利, 赵若灿, 周安然, 王国成, 唐磊.  基于瑞利多普勒激光雷达数据的重力波测量与分析 . 红外与激光工程, 2018, 47(9): 930002-0930002(5). doi: 10.3788/IRLA201847.0930002
    [9] 冯帅, 蒋立辉, 熊兴隆, 马愈昭.  含有突变信号的激光雷达能见度反演 . 红外与激光工程, 2017, 46(3): 330001-0330001(7). doi: 10.3788/IRLA201746.0330001
    [10] 邓潘, 张天舒, 陈卫, 刘洋.  合肥上空中层大气密度和温度的激光雷达探测 . 红外与激光工程, 2017, 46(7): 730003-0730003(6). doi: 10.3788/IRLA201746.0730003
    [11] 谭巧, 徐启峰, 谢楠, 邱鑫茂, 谢榕芳.  BGO晶体固有线性双折射及其温度特性的定量研究 . 红外与激光工程, 2016, 45(6): 622004-0622004(6). doi: 10.3788/IRLA201645.0622004
    [12] 邓潘, 张天舒, 刘建国, 刘洋, 董云升, 范广强.  532 nm和355 nm瑞利激光雷达观测中层大气的数据对比分析 . 红外与激光工程, 2016, 45(S2): 19-25. doi: 10.3788/IRLA201645.S230001
    [13] 程永强, 胡雄, 闫召爱, 郭商勇, 孙逸桥, 张旭.  可重部署钠激光雷达接收系统减震设计 . 红外与激光工程, 2016, 45(S1): 92-97. doi: 10.3788/IRLA201645.S130005
    [14] 程永强, 胡雄, 闫召爱, 郭商勇, 王博.  大气重力波引起的偶发钠层研究 . 红外与激光工程, 2016, 45(10): 1030004-1030004(6). doi: 10.3788/IRLA201645.1030004
    [15] 田媛, 韩一平, 牛化恒, 雷园.  弱电离高超声速流场对太赫兹波传播影响 . 红外与激光工程, 2015, 44(12): 3690-3695.
    [16] 龚少华, 刘正宽, 关塞, 焦菁, 沈振江, 羊大力, 孙书娟, 陈春霞.  北京上空中层顶区域重力波参数关系的激光雷达研究 . 红外与激光工程, 2015, 44(4): 1134-1140.
    [17] 姜成昊, 杨进华, 张丽娟, 李祥.  新型多普勒成像激光雷达原理设计与仿真 . 红外与激光工程, 2014, 43(2): 411-416.
    [18] 刘华松, 余俊宏, 冷健, 庄克文, 季一勤.  毫米波在SiO2基底材料中的传播特性 . 红外与激光工程, 2014, 43(4): 1145-1149.
    [19] 谭东杰, 张安.  方向相关与互信息加权组合多模图像配准方法 . 红外与激光工程, 2013, 42(3): 836-841.
    [20] 刘志明, 陈坤峰, 高业胜, 史学舜, 简水生.  阵列波导光栅中自由传播区模式的有效折射率 . 红外与激光工程, 2013, 42(8): 2146-2149.
  • 加载中
WeChat 点击查看大图
计量
  • 文章访问数:  389
  • HTML全文浏览量:  85
  • PDF下载量:  87
  • 被引次数: 0
出版历程
  • 收稿日期:  2016-04-23
  • 修回日期:  2016-05-18
  • 刊出日期:  2017-05-25

中层顶准单色重力波特性的钠荧光多普勒激光雷达观测分析

doi: 10.3788/IRLA201746.0506002
  • 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
    • 作者简介:

    王博(1987-),男,博士生,主要从事临近空间大气物理方面的研究。Email:wangbocas@163.com

    通讯作者: 胡雄(1967-),男,研究员,博士生导师,主要从事临近空间环境建模、预报、探测方面的研究。Email:xhu@nssc.ac.cn
  • 收稿日期: 2016-04-23
  • 修回日期: 2016-05-18
  • 刊出日期: 2017-05-25
基金项目:

国家自然科学基金（41104099，41104100，41204137）

  • 中图分类号: P356

摘要: 利用2011~2013年期间60 h的钠荧光多普勒激光雷达温度和风场数据，采用矢端曲线法提取廊坊上空85~95 km中层顶区域准单色惯性重力波的所有参量，并统计准单色大气重力波的活动特性。获得的85次准单色重力波事件中，上传（下传）重力波64次（21次），占总数的75。29%（24。71%）。垂直波长（水平波长）和观测周期平均值分别为6。6 km（727。8 km）和7。4 h，分别集中在6~9 km（200~800 km）和2~7 h，固有周期平均值为7。76 h，主要集中在3~9 h，水平传播方向分布比较均匀，没有占主导的传播方向。对于上传重力波，水平背景风在大气重力波水平传播方向上的分量取正值和取负值的概率大致相等，但对于下传重力波，该风场分量取正值的概率大约是取负值的2倍，说明观测到的下传大气重力波在中层顶区域多为顺风传播。

English Abstract

    全文HTML

参考文献 (31)

目录

    /

    返回文章
    返回

    版权所有 © 2019 《红外与激光工程》编辑部｜ 地址: 天津市空港经济区中环西路58号｜ 邮政编码: 300308

    津ICP备19007885号-1

    本系统由 北京仁和汇智信息技术有限公司 开发    百度统计