不同初始扰动对电离层扩展F影响的数值模拟
Numerical simulation about the influence of different initial disturbance on the ionosphere spread-F
查看参考文献21篇
文摘
|
重力波、中性风场、电场是激发电离层扩展F的主要影响因子,本文基于中低纬电离层扩展F发展的物理模型,通过电场强度、背景风场对扩展F影响作用的分析和经验对比,首先验证了模型的有效性,后借助该模型数值模拟了给定背景环境下三种尺度初始电子密度扰动条件下扩展F的发展情况,同时研究了利用化学物质释放实现一定尺度扰动,进而激发扩展F的过程.结果表明,较强的背景电场、东向风场有利于扩展F的形成和抬升,与经验结论相吻合;电离层从被作用初始扰动到激发扩展F的过程中存在拐点效应,拐点之后扩展F被激发形成并且抬升迅速,同时短波长扰动相对于长波长扰动更有利于扩展F的激发和发展;化学物质H_2O释放通过耗散电子密度,形成了一定尺度扰动并诱发了扩展F的形成,该方法可作为一种人工激发扩展F的探索手段. |
其他语种文摘
|
The triggering role of different factors like gravity wave,neutral wind,and electric field in the formation of ionosphere spread-F is a hot issue. Based on a physical model which is developed to present the development of ionosphere spread-F, the reliability of this model is firstly proved by analysis of the effects of eastward electric field and background wind field on spread-F and comparison with experience. Then, on a given background, the spread-F triggered by three disturbances of the initial electron density of different scale is simulated in this paper. The possibility of causing a certain scale perturbation and triggering spread-F by chemical release is also demonstrated. The results show that strong electric-field intensity and eastward neutral wind are beneficial to the development of spread-F, proving that the physical model is reliable; there is an inflection point of the uplift rate of spread-F in the development process, after which spread-F is triggered and developed, and the electron density disturbances with short wavelength are much more beneficial to the triggering and development of spread-F than that of long wavelength; chemical H_2O can produce localized electron density depletion effectively, and it can form a certain scale initial disturbance of electron density for triggering spread-F in the ionosphere, indicating that chemical release could be used as a way to trigger spread-F artificially. |
来源
|
地球物理学报
,2017,60(2):470-479 【核心库】
|
DOI
|
10.6038/cjg20170202
|
关键词
|
电子密度扰动
;
扩展F
;
数值模拟
|
地址
|
1.
解放军理工大学气象海洋学院, 空间天气学国家重点实验室, 南京, 211101
2.
解放军理工大学气象海洋学院, 南京, 211101
|
语种
|
中文 |
文献类型
|
研究性论文 |
ISSN
|
0001-5733 |
学科
|
地球物理学 |
基金
|
国家自然科学基金项目
;
国家重点实验室专项基金资助
|
文献收藏号
|
CSCD:5908606
|
参考文献 共
21
共2页
|
1.
Basu S. Evolution of subkilometer scale ionospheric irregularities generated by high-power HF waves.
J. Geophys. Res,1997,102(A4):7469-7475
|
被引
2
次
|
|
|
|
2.
Bernhardt P A.
The response of the ionosphere to the injection of chemically reactive vapors [Ph. D. thesis],1976
|
被引
1
次
|
|
|
|
3.
Bernhardt P A. Three-dimensional, time-dependent modeling of neutral gas diffusion in a nonuniform, chemically reactive atmosphere.
J. Geophys. Res,1979,84(A3):793-802
|
被引
13
次
|
|
|
|
4.
Booker H G. Scattering of radio waves by the Fregion of the ionosphere.
Journal of Geophysical Research,1938,43(3):249-256
|
被引
15
次
|
|
|
|
5.
Cai H T. Simultaneous observations of large-scale traveling ionospheric disturbances on the nightside and dayside middle latitude.
Ann. Geophys,2012,30(12):1709-1717
|
被引
3
次
|
|
|
|
6.
Chou S Y. A numerical study of the wind field effect on the growth and observability of equatorial spread F.
J. Geophys. Res,1996,101(A8):17137-17149
|
被引
1
次
|
|
|
|
7.
Frissell N A. Climatology of medium-scale traveling ionospheric disturbances observed by the midlatitude Blackstone SuperDARN radar.
J. Geophys. Res. Space Physics,2014,119(9):7679-7697
|
被引
2
次
|
|
|
|
8.
Gurevich A. Large scale structuring of plasma density perturbations in ionospheric modifications.
Physics Letters A,2002,301(3/4):307-314
|
被引
2
次
|
|
|
|
9.
Hu Y G. Ionospheric disturbances produced by chemical releases and the resultant effects on short-wave ionospheric propagation.
J. Geophys. Res,2011,116:A07307
|
被引
5
次
|
|
|
|
10.
Huang C S. Nonlinear evolution of equatorial spread F: 1. On the role of plasma instabilities and spatial resonance associated with gravity wave seeding.
J. Geophys. Res,1996,101(A1):283-292
|
被引
4
次
|
|
|
|
11.
Huba J D. Impact of meridional winds on equatorial spread F: Revisited.
Geophys. Res. Lett,2013,40(7):1268-1272
|
被引
4
次
|
|
|
|
12.
Kolomiitsev O P. Ionosphere plasma holes-modeling and diagnostic.
Physics and Chemistry of the Earth, Part C: Solar, Terrestrial & Planetary Science,1999,24(4):393-399
|
被引
6
次
|
|
|
|
13.
Mendillo M. Finite element simulation (FES): a computer modeling technique for studies of chemical modification of the ionosphere.
Adv. Space Res,1993,13(10):55-64
|
被引
13
次
|
|
|
|
14.
Ossakow S L. Nonlinear equatorial spread F: Dependence on altitude of the F peak and bottomside background electron density gradient scale length.
J. Geophys. Res,1979,84(A1):17-29
|
被引
7
次
|
|
|
|
15.
Rappaport H L. Localized modes with zonal neutral wind, diffusion, and shear in equatorial spread F.
J. Geophys. Res,1998,103(A12):29137-19154
|
被引
1
次
|
|
|
|
16.
Sekar R. Effects of vertical winds and electric fields in the nonlinear evolution of equatorial spread F.
J. Geophys. Res,1994,99(A2):2205-2213
|
被引
4
次
|
|
|
|
17.
Sultan P J.
Chemical release experiments to induce F region ionospheric plasma irregularities at the magnetic equator [Ph. D. thesis],1994
|
被引
1
次
|
|
|
|
18.
Tsunoda R T. On equatorial spread F: Establishing a seeding hypothesis.
J. Geophys. Res,2010,115:12303
|
被引
1
次
|
|
|
|
19.
罗伟华. 赤道电离层R-T不稳定性发展的控制因素分析.
地球物理学报,2009,52(4):849-858
|
被引
11
次
|
|
|
|
20.
汪四成. 化学物质释放激发中低纬扩展F的数值模拟.
地球物理学报,2013,56(9):2906-2911
|
被引
5
次
|
|
|
|
|