2001 Vol. 21, No. 2

Display Method:
PROPAGATION OF ALFVÉN WAVES IN MULTI-LAYER SOLAR ATMOSPHERE MODEL
LI Bo, WANG Shui
2001, 21(2): 97-104. doi: 10.11728/cjss2001.02.20010201
Abstract(2407) PDF 523KB(967)
Abstract:
In this paper, the actual solar atmoshpere is idealized as a multi-isothermal-layer system so as to obtain the energy transmittance of the linear Alfven wave that propagates through such a system in presence of a uniform oblique magnetic field. The result indicates that two-layer models are essentially different to three-layer models. In two-layer models, the temperature jump act as a high pass-filter, while in three-layer models, resonant transfer will take place, the transmittance shows a. vibration. The result reveals that the lower parts of the solar atmopshere are more suitable for those Alfven waves with period of a few seconds to transfer their energy.
NUMERICAL RESEARCH ABOUT WHITE LIGHT CORONAGRAPH FIGURE OBSERVED AT MAY 2 1998
YE Zhanyin, WEI Fengsi, FENG Xueshang, SHI Yong, YAO Jiusheng
2001, 21(2): 105-113. doi: 10.11728/cjss2001.02.20010202
Abstract(2322) PDF 862KB(834)
Abstract:
A new model of 2-D ideal magnetohydrodynamic equations, which sets spherical coordinates (γ, φ) on the plane of sky to avoid singular geometry at solar poles, is employed to simulate white light coronagraph figure. Numerical white light figure of the final self-consistent steady state, calculated with initial magnetic field constructed from a magnetic hexapole and several dipoles and with projected characteristic inner boundary condition, agrees basically with the observed coronagraph figure. The simulation also shows that magnetic structure dominates the solar wind flow field.
THE EVOLUTION OF MULTIPLE CURRENT SHEET IN ANISOTROPIC PLASMA
MA Yingjuan, JIA Yingdong, WANG Shui
2001, 21(2): 114-123. doi: 10.11728/cjss2001.02.20010203
Abstract(2431) PDF 849KB(1018)
Abstract:
The evolution of periodic multiple current sheets in the presence of a pressure anisotropy is numerically simulated based on a two-dimensional three component magnetohydrodynamic method. It is found out that when the plasma parameter β<<1, a slight anisotropy can only expedite the magnetic reconnection process. When the plasma parameter β≈1 (means that the thermal pressure is comparable with the magnetic pressure), slight perpendicular anisotropy can not only expedite the magnetic reconnection process, but also change the position of X line in reconnection. The magnetic filed changes gradually from an anti-symmetric configuration to a symmetric shape, which will further evolve into an anti-symmetric configuration in opposite phase with initial configuration. Large perpendicular anisotropy or parallel anisotropy will enhance the growth rate dramatically. But the magnetic field configuration does not have fundamental change in parallel anisotropy. There are only some irregular disturbs in the center of the current sheet. The magnetic islands that formed in the anisotropy plasma with periodical current sheets are smaller than those formed in isotropic periodical current sheets with same parameters.
SHEARED ION FLOW INSTABLITY IN MAGNETOPAUSE BOUNDARV LAYER AT THE HIGH-LATITUDE MAGNETOTALL
LU Li, LIU Zhenxing, LI Zhongyuan
2001, 21(2): 124-130. doi: 10.11728/cjss2001.02.20010204
Abstract(2202) PDF 593KB(822)
Abstract:
The sheared ion flow instability is studied in an inhomogeneous plasma background of magnetopause boundary layer at the high latitude magnetotail. By considering tail-aligned currents, we find that the instability excitation strongly depend on the disturbed wavelength. The quasi-critical wave number for the instability is obtained. For relative long wavelength perturbation the instability tend to be excited at the inner edge of the boundary layer. The stable surface wave at magnetopause and the K-H instability at the inner edge of the boundary layer can exist at the same time, and that may help to transfer the momentum toward magnetosphere continuously.
THE GLOBAL IONOSPHERIC RESPONSE TO THE GEOMAGNETIC STORM EVENT DURING MAY 1998
ZHANG Manlian, SHANG Sheping, GUO Jianshan, LUO Xigui
2001, 21(2): 131-140. doi: 10.11728/cjss2001.02.20010205
Abstract(2577) PDF 935KB(885)
Abstract:
Using the ionospheric characteristic parameter f0F2 observed in more than 40 ionosonde stations distributed over the world, the response of the ionosphere to the geomagnetic storm event during May 1998 is studied by calculating the percentage deviation of the daily f0F2 value from its monthly median value for these stations which are divided into 5 regions according to their longitudinal distribution. The results showed that the characteristics of the ionospheric disturbance during the active phase of the storm can be explained by the storm circulation theory, but it seems that the positive disturbance appearing in the European region during the late recovery phase could not be attributed to this explanation.
A NUMERICAL STUDY OF NONLINEAR PROPAGATION OF A GRAVITY-WAVE MCKET IN 3-DIMENSIONAL GLOBAL COORDINATION
ZHANG Shaodong, YI Fan, XIONG Donghui
2001, 21(2): 141-147. doi: 10.11728/cjss2001.02.20010206
Abstract(2263) PDF 603KB(825)
Abstract:
By using full-implicit-continuous-Eulerian (FICE) scheme, and taking the atmospheric basic motion equations in 3-dimensional global coordination as the governing equations, a numerical simulation of nonlinear propagation of a gravity-wave packet in mesosphere is presented. The numerical results perfectly show the nonlinear propagation of a gravity-wave packet in mesosphere. A comparison of the numerical results with the linear gravity-wave theories is also presented.
A STUDY OF NONLINEAR PROPAGATION OF 3D GRAVITY-WAVE MCKETS IN A COMPRESSIBLE ATMOSPHERE BY USING ADI SCHEME
YUE Xianchang, YI Fan
2001, 21(2): 148-158. doi: 10.11728/cjss2001.02.20010207
Abstract(2125) PDF 899KB(1001)
Abstract:
By using an Alternative-Direction-Implicit (ADI) scheme, a numerical model for nonlinear propagation of gravity-wave packets in a three-dimensional compressible atmosphere is solved. Results of numerical simulation show that after several periods, the gravity-wave packets propagate steadily upward and keep its shape well. The interior points and boundaries of the calculating region are stable. During the propagation the amplitude of wave-associated perturbation velocities increase with the increasing height. This shows that ADI scheme is reliable for simulating the nonlinear propagation of gravity-wave packets in a three-dimensional compressible atmosphere. From the results, It’s also found that under nonlinear condition, a gravity wave packet is still able to keep some characterizations as under linear propagation. The nonlinear effect mainly impacts the propagation velocity of gravity-wave packets.
THE GEOMAGNETIC RESPONSE OF MAY 1998 EVENT
WANG Danwen, FENG Xueshang
2001, 21(2): 159-164. doi: 10.11728/cjss2001.02.20010208
Abstract(2565) PDF 429KB(854)
Abstract:
During the May 1998 great event time, there was a strong storm. This storm commenced on about 2200 UT of Mad 1. The initial phase was from 2200 of May 1 to 0300 of May 2, with a sudden commencement. The main phase was from 0300 of May 2 to 0600 of May 4. The recovery phase lasted quite a few days. Observations show that there are Pc2-Pc5 geomagnetic pulsations after sudden commencement of initial phase, and these pulsations, perhaps are due to the large scale lessening or expanding of the magnetosphere. The Beijing Obs. 1 Hz Data of horizontal component H during this storm on 1-5 May 1998 are analysed. It is found that there are a lot of Pc2-Pc3 pulsations on the first 4 hours in the main phase. The power spectrum firstly, then use the band pass filter are calculated. There are some Pc5 in the recovery phase, although in China latitudes are low: L =1-2. There are some Pc5-Pc6 in the storm day time in the India. In Beijing, the Pc5 magnitude is about 5nT. It is at 18 hourLT. The band of frequencies of Pc2 pulsation is 0.1-0.15 Hz, the band of Pc3 is 0.02-0.1 Hz, and the band of pc5 is 2.0-4.0 mHz. The storm recovery phase begins when the IMF turns less southward, with delays of about 2 hours. As Fig.2 shows, the Bz. component of IMF is turning to southward when the main phase of the storm begins, and the southward IMFs (Bz< 0) decrease to the minimum on 0400 of May 4, two hours later the storm recovery phase begins. The solar wind electrical field vBz is also calculated, where v is the SW speed, the Bz is the north-south component of IMF. Some results: vBz change suddenly when the initial phase is beginning; the main phase of the storm begins at 0300 of May 2, vBz is decreasing; the recovery phase begins when vBz turns to the minimum, with delays of about 2 hours are got.
COMPARISON OF DENSITY AND TEMPERATURE PROFILE OBSERVED BY LIDAR AND OCCULTATION TECHNIQUE
ZENG Zhen, HU Xiong, ZHANG Xunxie, Makoto Abo
2001, 21(2): 165-171. doi: 10.11728/cjss2001.02.20010209
Abstract(2737) PDF 606KB(1131)
Abstract:
Comparisons of profiles of the atmospheric density and the temperature at heights from 30-55 km measured by a Rayleigh with Na lidar and occultation technique have been made preliminarily. The lidar situated in Hochioji Tokyo (35.37°N, 139.23°E) operated routinely, and the data of occultation are available at almost the same place and at the same time (Oct.14, 1996), which allow to do comparisons of these results obtained by different techniques. The limits of these two techniques are discussed respectively. Results illustrate a good agreement in density profiles and temperature profiles.
IN-PLANAR MOTION AND REGULAR DYNAMICS OF MASS-LESS TETHER SATELLITE SYSTEM
YU Shaohua, LIU Qiang
2001, 21(2): 172-180. doi: 10.11728/cjss2001.02.20010210
Abstract(2148) PDF 697KB(879)
Abstract:
The motion of tether satellite system inner the orbital plane is described by the relative position vector between the subsatellite and base-satellite. As soon as the range rate control algorithm is established, the motion of the system is determined by the direction angle of the position vector, which has a stationary state. The stationary state is a limit point if the orbit is circular, and a limit cycle if the orbit is elliptical. An iterative algorithm is introduced to compute the limit cycle, and a method for stability analysis of the stationary state is also discussed. Computer simulations are carried out for both the limit point and limit cycle.
ORIGINAL NEPHOGRAM DEMODULATOR OF FY-B SATELLITE
ZHANG Wei, PAN Zhangyong, GUO Xingbo, YANG Zhixing
2001, 21(2): 181-186. doi: 10.11728/cjss2001.02.20010211
Abstract(2320) PDF 508KB(992)
Abstract:
Theory and realization of FY-2 B satellite original nephogram demodulator is introduced in this paper. By using Decision-feedback loop and programmable bit synchronizer, the demodulator has the advantage of quick lock, wide lock band and low bit error rate. This device has already been field tested and now using in CDAS Satellite station.
ANALYSIS OF HIGH QUALITY MICROGRAVITY ABOUT BALLOON-RELEASED TEST PLATFORM
GAO Yunfeng, WANG Linghua
2001, 21(2): 187-192. doi: 10.11728/cjss2001.02.20010212
Abstract(2271) PDF 485KB(861)
Abstract:
Some dynamic characters of a new balloon-released test platform in capsule with high quality microgravity are studied in this paper. The dynamics equations are obtained by considering the effect of the rarefied gas and the free molecular flow in vacuum chamber. The relationship between microgravity and control precision, detach time of platform from capsule, and pressure of the vacuum chamber are obtained by simulation.