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北京上空下三角钾层的激光雷达观测与研究

王泽龙 杨国韬 王继红 焦菁 杜丽芳 荀宇畅

王泽龙, 杨国韬, 王继红, 焦菁, 杜丽芳, 荀宇畅. 北京上空下三角钾层的激光雷达观测与研究[J]. 空间科学学报, 2018, 38(1): 65-72. doi: 10.11728/cjss2018.01.065
引用本文: 王泽龙, 杨国韬, 王继红, 焦菁, 杜丽芳, 荀宇畅. 北京上空下三角钾层的激光雷达观测与研究[J]. 空间科学学报, 2018, 38(1): 65-72. doi: 10.11728/cjss2018.01.065
WANG Zelong, YANG Guotao, WANG Jihong, JIAO Jing, DU Lifang, XUN Yuchang. Lidar Observations and Studies of the Lower-triangle Potassium Layer over Beijing ormalsize[J]. Chinese Journal of Space Science, 2018, 38(1): 65-72. doi: 10.11728/cjss2018.01.065
Citation: WANG Zelong, YANG Guotao, WANG Jihong, JIAO Jing, DU Lifang, XUN Yuchang. Lidar Observations and Studies of the Lower-triangle Potassium Layer over Beijing ormalsize[J]. Chinese Journal of Space Science, 2018, 38(1): 65-72. doi: 10.11728/cjss2018.01.065

北京上空下三角钾层的激光雷达观测与研究

doi: 10.11728/cjss2018.01.065
基金项目: 

国家自然科学基金项目(NSFC41474130,41264006,41627804),青年科学基金项目(41604130),国家国际科技合作专项(2014DFA20770),中国科学院国家空间科学中心重点培育项目和国家重点实验室专项项目共同资助

详细信息
    作者简介:

    杨国韬,E-mail:gtyang@spaceweather.ac.cn

  • 中图分类号: P352

Lidar Observations and Studies of the Lower-triangle Potassium Layer over Beijing ormalsize

  • 摘要: 利用2010年11月至2011年10月和2013年5月至2014年4月两年的观测数据发现一种特殊的钾层,称其为下三角钾层.下三角钾层的峰值密度随时间逐渐增加,峰值密度所在高度不断降低,钾原子浓度随高度的升高先迅速增加,然后又缓慢减少.当下三角钾层出现时,90km以下的柱密度显著增加,而90km以上的柱密度变化不大,导致钾层总的柱密度明显增加.一月是下三角钾层出现时长最多且出现率最高的月份,这可能与大气半日潮汐的季节变化有关.下三角钾层的频繁出现使钾层一月份的柱密度和峰值密度分别增加15.7%和12.9%,而质心高度却降低0.18km.将下三角钾层与同时同地观测的钠层进行比较,结果显示当钾原子浓度增加时,钠原子浓度却变化不大.假设不存在特殊的源注入,结合钾层模型与钠层模型中的化学反应及其相应的化学反应速率,可以推测下三角钾层中增加的钾原子主要来自KO2,部分来自KOH.

     

  • [1] GARDNER C S. Performance capabilities of middle-atmosphere temperature lidars: comparison of Na, Fe, K, Ca, Ca+, and Rayleigh systems[J]. Appl. Opt., 2004, 43(25):4941-4956
    [2] PLANE J M C. The chemistry of meteoric metals in the Earth's upper atmosphere[J]. Int. Rev. Phys. Chem., 1991, 10(1):55-106
    [3] GARDNER C S, VOELZ D G, SECHRIST C F Jr, et al. Lidar studies of the nighttime sodium layer over Urbana, Illinois: 1. Seasonal and nocturnal variations[J]. J. Geophys. Res., 1986, 91(A12):13659-13673
    [4] ESKA V, VON ZAHN U, PLANE J M C. The terrestrial potassium layer (75~110km) between 71°S and 54°N: observations and modeling[J]. J. Geophys. Res., 1999, 104(A8):17173-17186
    [5] GARDNER C S, CHU Xianzhao, ESPY P J, et al. Seasonal variations of the mesospheric Fe layer at Rothera, Antarctica (67.5°S, 68.0°W)[J]. J. Geophys. Res., 2011, 116(D2):D02304
    [6] GERDING M, ALPERS M, VON ZAHN U, et al. Atmospheric Ca and Ca+ layers: Midlatitude observations and modeling[J]. J. Geophys. Res., 2000, 105(A12):27131-27146
    [7] SULLIVAN H M, HUNTEN D M. Lithium, sodium, and potassium in the twilight airglow[J]. Can. J. Phys., 1964, 42(5):937-956
    [8] FELIX F, KEENLISIDE W, KENT G, et al. Laser radar observations of atmospheric potassium[J]. Nature, 1973, 246(5432):345-346
    [9] MEGIE G, BOS F, BLAMONT J E, et al. Simultaneous nighttime lidar measurements of atmospheric sodium and potassium[J]. Planet. Space Sci., 1978, 26(1):27-35
    [10] VON ZAHN U, HÖFFNER J. Mesopause temperature profiling by potassium lidar[J]. Geophys. Res. Lett., 1996, 23(2):141-144
    [11] ESKA V, HÖFFNER J, VON ZAHN U. Upper atmosphere potassium layer and its seasonal variations at 54°N[J]. J. Geophys. Res., 1998, 103(A12):29207-29214
    [12] FRIEDMAN J S, COLLINS S C, DELGADO R, et al. Mesospheric potassium layer over the Arecibo Observatory, 18.3°N, 66.75°W[J]. Geophys. Res. Lett., 2002, 29(5):1071
    [13] WANG Zelong, YANG Guotao, WANG Jihong, et al. Seasonal variations of meteoric potassium layer over Beijing (40.41°N, 116.01°E)[J]. J. Geophys. Res., 2017, 122(2):2106-2118
    [14] FRIEDMAN J S, CHU Xinzhao, BRUM C G M, et al. Observation of a thermospheric descending layer of neutral K over Arecibo[J]. J. Atmos. Solar-Terr. Phys., 2013, 104:253-259
    [15] JIAO Jing, YANG Guotao, WANG Jihong, et al. Occurrence and characteristics of sporadic K layer observed by lidar over Beijing, China[J]. Sci. China Earth Sci., 2016, 59(3):540-547
    [16] JIAO Jing, YANG Guotao, WANG Jihong, et al. First report of sporadic K layers and comparison with sporadic Na layers at Beijing, China (40.6°N, 116.2°E)[J]. J. Geophys. Res., 2015, 120(6):5214-5225
    [17] CLEMESHA B R, BATISTA P P, SIMONICH D M. Tide-induced oscillations in the atmospheric sodium layer[J]. J. Atmos. Solar-Terr. Phys., 2002, 64(12/13/14):1321-1325
    [18] YUE Jia, XU Jiyao, CHANG L C, et al. Global structure and seasonal variability of the migrating terdiurnal tide in the mesosphere and lower thermosphere[J]. J. Atmos. Solar-Terr. Phys., 2013, 105-106:191-198
    [19] GONG Shaohua, YANG Guotao, DOU Xiankang, et al. Statistical study of atmospheric gravity waves in the mesopause region observed by a lidar chain in eastern China[J]. J. Geophys. Res., 2015, 120(15):7619-7634
    [20] PLANE J M C, FENG W, DAWKINS E, et al. Resolving the strange behavior of extraterrestrial potassium in the upper atmosphere[J]. Geophys. Res. Lett., 2014, 41(13):4753-4760
    [21] PLANE J M C. A time-resolved model of the mesospheric Na layer: constraints on the meteor input function[J]. Atmos. Chem.-Phys., 2004, 4(3):627-638
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出版历程
  • 收稿日期:  2017-04-06
  • 修回日期:  2017-09-12
  • 刊出日期:  2018-01-15

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