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The Potential of VSOP2

Oct 2007 | Comments Off on The Potential of VSOP2

WEI ERHU, LIU JINGNAN, YAN WEI

 
The feasibility of the latest SVLBI program—VSOP2 for geodetic applications is analyzed
   

SVLBI (Space Very Long Baseline Interferometry) is an extension of the ground-based VLBI into the space. It has some important potential applications in geodesy and geodynamics, including the definition, practical realization, and the interconnection of different reference frames, determining the geocentric positions of VLBI stations, estimation of the gravity field of the Earth, and satellite orbit determination using the delay and delay rate observables.

The idea of SVLBI was brought forward by N, S. Kardashev in 1970s. More deeper research had been done in 1970s and 1980s. With the launching of the first SVLBI satellite of the VLBI Space Observatory Programme (VSOP) of Japan, in February 1997, this technique has become a reality. An international team of scientists, working under the auspices of the FÖMI Satellite Geodesy Observatory, Hungary, has designed the Geodesy Demonstration Experiment (GEDEX), for the purpose of exploring the feasibility of the geodetic applications of SVLBI. However, several major problems also exist. It is not suitable for geodetic and geodynamic study, which requires precise tracking capabilities resulting in cm orbit accuracy. But the precision of orbit determination is within 10 meters. It is not suitable to frequently changing observing objects. So it cannot provide observations aiming at more radio sources, which are required for geodetic and geodynamical studies. On the other hand, the satellite stopped transmitting observation data after October 2003 and terminated its work on 02:28UT November 11th 2005.

Introduction of VSOP2

The Project

Following the success of the VSOP, a next generation space VLBI mission, currently called VSOP-2, is being planned in Japan with international collaboration for a launch as early as 2012.

Although there are some obvious defects in VSOP, it is more preponderant than ground-based VLBI. For example, it can provide radio observation with a baseline length longer than the diameter of the Earth to increase observation resolution; also, it can provide all-day VLBI imaging; It has the ability of quick-imaging by the fast movement of VSOP surrounding the Earth; Observation of microscale characteristic is provided by the reduction of u – v empty and so on (SHEN Zhiqiang, 1998). VSOP can achieve more difficult researches with these advantages, such as revealing the fine structures of active galactic nuclei (AGNs). VSOP has achieved its preconcerted mission requirement and has obtained some successes after several years, including: the quick-change of radio source in 1 day can be observed by quick-imaging; north-south resolution is increased obviously; increasing the dynamic range of image (WAN Tongshan, 1999). So VSOP has promoted the development of SVLBI.

Based on the successes of VSOP, the science goals for the VSOP-2 mission will place the emphasis on observations in the millimeter wave-band, enabling imaging on the scale of the accretion disk and jet acceleration region surrounding the supermassive black holes in the center of active galactic nuclei, and allow the structure of protostellar magnetospheres to be clarified. Because of the improvement of satellite orbit and structure, such as large deployable reflector (LDR), VSOP2 is more efficient than its precursor. These improvements include: ten times higher observing frequency; ten times better resolution; ten times higher sensitivity; astrometric capability and further sensitivity gains from phase referencing; Measurement of magnetic fields through dual polarization observations and so on.

figure12figure13

Satellite

Orbital parameters

VSOP

VSOP2

Apogee height ha km

21400

25000

Perigee height hp km

560

1000

Orbit period T h

6.3

7.45

Inclinatio i °

46.4 or 31

31

Arg.of perigee ω °

285 315 or alterable

questionably

Eccentricity ε

0.379

0.7

RAAN Ω

alterable

-0.46

Satellite orbit parameters

As the next generation of VSOP, VSOP2 makes progress in many aspects. According to VSOP-2 Proposal Abridged English Version, the satellite orbit parameters of VSOP2, such as apogee height and perigee height, are appropriately adjusted by studying the influence of high angular resolution and orbit period caused by high apogee height, the influence of atmospheric resistance near perigee and so on. The adjustment makes VSOP2 more suitable for science researches. The comparison of VSOP and VSOP2 parameters is listed in Table 1.

In the following, simulation analyses will be made.

Requirements for Orbit Determination

The simulation of VSOP2 in this paper includes: Orbit Determination (OD) of VSOP2 satellite by GNSS, the tracking status of the satellite and the feasibility of connecting observation between the satellite and the observation stations on the ground.
During the stimulation, the orbit period is 447.43 minutes and other parameters are invariable. The orbits of simulant satellites are shown in Fig 1, in which VSOP orbit is yellow and VSOP2 orbit is purple. The simulant time is from 2008 1 1 12:00:00 UTC to 2008 1 2 12:00:00 UTC (almost three orbit periods). Sampling interval is 60 seconds.

 
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WEI ERHU, LIU JINGNAN, YAN WEI

Orbit determination accuracy requirements

In the report prepared by the RADIOASTRON Navigation Astrometry and Geodesy (NAG) Working Group about the precise navigation of the SVLBI satellite, the following orbit determination accuracy requirements have been specified (NAG, 1989):
1) Standard Orbit: Required accuracy better than 1000 m for satellite control, orbit prediction, tracking and data communication.
2) Precise Orbit: Required accuracy better than 50m for processing ground-to-space VLBI data, and most astrometric applications.
3) Highly Precise Orbit: Required accuracy better than 1 m for geodetic and some astrometric.

Required accuracy better than 0.1m for geodynamic applications.
The accuracy of standard orbit and precise orbit has been achieved with the development of tracking technology. Even the OD accuracy of VSOP can be achieved 3-10 m which satisfies the requirement of above two accuracies. But It is not suitable for geodetic and geodynamic studies because it can’t achieve the accuracy of highly precise orbit, better than 1 m, because of its irregular shape, big ratio of area/mass, the limit of the accuracy obtainable using Doppler data only and so on. VSOP2 makes some improvements in its structure. Its higher science goals request higher accuracy of OD. Some studies indicate that OD accuracy can achieve cm level which is suitable for geodetic applications by using GPS and accelerometer (ISAS, 2003).

As reported (ISAS, 2003), the satellite in relatively low Earth orbit can achieve 5 cm level OD with GPS and accelerometer. But there is no signal from GPS near VSOP apogee. Using GALILEO system as a supplement of GPS is a best way to improve OD. Pre-literature has been discussed the coverage instance of SVLBI satellite by GPS and GALILEO system (WEI Erhu, 2006). As some papers (IAIN/GNSS 2006) have studied, it will be possible to use GPS and GALILEO as one system. In this paper, the OD accuracy of VSOP2 by above situation is discussed.

Simulation Study

Simulation Condition

GALILEO constellation in simulation is composed of 27 satellites. They spread equably in 3 orbits whose inclination is 56°. The satellite’s altitude is 23062 km and orbit period is 14.0 hs. The ratio of coverage of VSOP2 near apogee, which is advantaged for OD, will be improved because of higher altitude of GALILEO. The parameters of GPS are from NASA website (ftp://cddis.gsfc.nasa.gov/gps/data/daily/2005/). There are 24 satellites in the simulation.

On the other hand, considering the antenna is not globose to receive signal from all directions, and the influence of ionosphere and troposphere, the antenna is designed to point to space. It is designed as a cone with an apex angle of 80° to let the satellite to receive as more signals as possible. The coverage instance of VSOP2 by GPS and GALILEO system and its DOPs (PDOP which will be chose the best 6 satellites to calculate is mainly considered) is analyzed to achieve high accuracy OD. VSOP’s Simulant conclusion in the same time is compared.

Results of Simulation

There is not enough number of satellites to calculate the coverage time and PDOP during the simulation because of the design of the antenna. For example, the coverage near the apogee is too bad for OD. The coverage instance of VSOP and VSOP2 by GPS and GALILEO system is shown in Table 2.

According to the Table above, VSOP2’s coverage time by GNSS is shorter than VSOP in the simulation because its apogee height is higher. But during the natural tracking time, VSOP2’s mean PDOP is appreciably smaller than VSOP. And VSOP2’s PDOP is steadier than VSOP by analyzing their max and min PDOPs. That means the geometric structure of VSOP2 and GNSS system is better. It ascribes to the superiority of VSOP2’s orbit design.

As reported (ISAS, 2003), because of the combination of GPS and GALILEO system, the mean square error of OD accuracy can achieve 3 cm, so the actual OD accuracy can achieve 0.073 m by calculating with the mean PDOP—2.454. During the simulation, the time which OD accuracy under 1 m accounts for total time 100%, excluding the epoch which doesn’t satisfy the OD requirement. The OD accuracy of VSOP2 and VSOP by GNSS is shown in Fig 2. This conclusion is suitable for geodetic and geodynamic studies.

Items \ Satellite

Coverage time percentage

Mean PDOP

Max PDOP

Min PDOP

VSOP

61.4903%

4.406

1000

1.573

VSOP2

48.0663%

2.454

22.766

1.61

Improvement

Although PDOP for VSOP2 is better in the simulation, coverage time is an important factor in OD. So if the pointing of GNSS antenna can be set to more directions, the OD accuracy will be better. For example, if another GNSS antenna points to the Earth and its apex angle is also 80°, the percentage of coverage time will increase to 100%. Its mean PDOP is 4.196. But the influence of atmosphere in this kind of situation should be considered. The details are shown in Table 3 and Fig 3

The simulation above shows that VSOP2’s OD accuracy is suitable for geodetic applications by using GNSS system.

 
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WEI ERHU, LIU JINGNAN, YAN WEI

figure14

SVLBI
Satellite

Coverage
time

Mean
PDOP

OD
accuracy

OD
accuracy

VSOP2

100%

4.196

0.126

100%

Coverage of the tracking network

Tracking station

The ground tracking station is to receive and record observation data from satellite, to measure the position, movement velocity and orbit parameters of the satellite. And it is an important factor to guarantee the successful observation, so it is necessary to establish tracking stations and use advisable technique to complete these tasks. Mainly, VSOP2 system use K waveband to track and observe the satellite.

There is no material about the tracking stations for VSOP2, so tracking stations for VSOP will be used in the simulation, which are Usuda in Japan (10 m caliber), Green Bank in USA (14 m caliber) and other three DSN (Deep Space Network) stations of NASA (Goldstone in USA, Tidbinbilla in Australia and Madrid in Spain, all 11 m caliver).

Results and analyses

The simulation gives the dynamic and real-time coverage result of satellite and shows the report of coverage time. According to the simulate results, the total coverage time of VSOP2 satellite by tracking stations is 151875.737 seconds. The shortest coverage time is 2944.578 seconds in Usuda and the longest one is 22135.337 seconds in Green Bank. The percentage of coverage time of each tracking station is shown in Fig4. These results are improved by comparing with VSOP (VSOP’s coverage instance in the same time is shown in Fig 5.The total coverage time is 130764.923 seconds). These improvements are attributed to the new design of satellite structure and orbit.

figure15

Percentage of VSOP and VSOP2 by tracking network is respectively 85.37% and 86.39%, excluding the overlapped parts of coverage. For VSOP2, the coverage time of satellite by tracking station can be improved obviously from the example of Tidbinbilla and Madrid. But the coverage time of some stations, such as Green Bank, is shorter than VSOP. VSOP2 is designed to observe radio source in the south sky, so the coverage time of high latitude station is shorter.

If more tracking stations all over the world are added, the situation will be improved. In a word, the ability of coverage time of VSOP2 by tracking station is improved.

figure16

The baseline formed by observation station and VSOP2 satellite

Simulation condition

The formula of radio telescope angular resolution is θ′′= λ/D.ρ′′ (1) in which θ is angular resolution, λ is the wavelength of radio wave received by telescope, D is the length of baseline.

According to the formula (1), the length of baseline is a crucial factor to influence SVLBI angular resolution when the wavelength of radio source is invariable. High angular resolution caused by long baseline will be useful for geodetic applications.

Although the length of SVLBI baseline of VSOP2 is extended, actual baseline formed by observation station and VSOP2 satellite is the guarantee of interferometry. To consider its applications in China, several Chinese radio telescopes will be selected in the simulation. There is a radio source in the simulation too. The observing time and the number of baselines formed by observation station and VSOP2 satellite will be analyzed.

The selected radio telescopes are located in Beijing, Shanghai, Kunming, Urumqi and Guizhou. The diameter of telescope in Beijing Shanghai and Urumqi is 25 m, in Kunming is 40 m and in Guizhou is 500 m. The latter two are being established now. The selected radio source’s code is HR-7745, its right ascension is 20h18m56s and declination is -47°42´39˝, located in the south sky.

 
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WEI ERHU, LIU JINGNAN, YAN WEI

Results and analyses

Observing time is the guarantee of baseline observation. In the simulation, the observing time of HR-7745 by VSOP2 satellite is 79501.476 seconds, accounts for 92.02% of the simulation time. The observing time and proportion of each telescope is: Beijing, 11148.078 seconds,12.90% Shanghai, 23077.354 seconds, 26.71% Guizhou, 27132.087 seconds, 31.42% Kunming, 28297.055 seconds, 32.75% Urumqi, 0 seconds, 0%. The observing time of radio telescopes in China is decreased by the increasing latitude and longitude. Especially for Urumqi radio telescope, it can’t undertake the mission of tacking radio source in south sky.

According to the observing time, there are the most 4 baselines can be formed from 1 Jun 2008 18:18:27.371 to1 Jun 2008 19:55:06.457. The observing time is 5771 seconds and accounts for 6.68% of the simulation time. The observing time and proportion of different number of baselines is listed in Table 4.

figure18

Item Number of baseline

Observing time (seconds)

proportion

1

27000

31.25%

2

19920

23.06%

3

14760

17.08%

4

5771

6.68%

According to the results above, three observation stations’ observing time which can form baselines with the satellite is more than an orbit period in the simulation, excluding radio telescopes in Beijing and Urumqi. The observing time is long enough for observation. In the simulation, Kunming and Guizhou can form baseline with VSOP2 satellite when it is in the apogee (it is shown in Fig 6 in which VSOP2 and HR-7745 are both projection of Sub-satellite point). So the length of baseline can be longer than 31000 km. The angular resolution can achieve 0.086 seconds by calculating with a radio wave length of 13 cm. The conclusion is considerable.

The simulant results of VSOP in the same time are listed in Table 5. According to the results, the VSOP2’s ability of observing radio sources in the south sky is improved.

In the simulation, only radio telescopes in China are considered. The observing results will be better if there are more radio telescopes all over the world. According to the observing time of simulant radio source, the observing ability of radio source in the south sky is one designing purpose of VSOP2. The observation of radio sources in this area is a weakness of Chinese radio telescopes. The use of VSOP2 is hopeful to improve it.

SVLBI Satellite

Observing
time

Proportion

4 baselines

Time

Proportion

VSOP

74918.6s

86.7%

1090s

1.2%

Conclusion

According to the three simulations above, an elementary conclusion can be made that the ability of VSOP2 in the applications of geodetic research has been improved obviously. First, the average accuracy of OD is less than 0.5 m by GNSS system. It is achieved the requirement of applications for geodetic studies. Second, the proportion of tracking time of satellite by observation station is over 85%. It ensures the transmission of observing data and controling command. Finally, the observing ability of radio sources in the south sky is improved.

It is just considered the improvement of VSOP2’s orbit design in this paper. The improvement of satellite structure is ignored. Considering the scarcity of data and information, we believe that more successful results can be achieved in further studying.

Acknowledgement

This research is funded by the national ‘973 Project’ of China (No. 2006CB701301), and the project of university education and research of Hubei province (20053039). And most of all, this paper is to my Indian friend Prof. Madhav N.Kulkarni who, in his life time,has made tremendous contributions in the researchment on geodesy, geodynamics, and GNSS applications.

Reference

SHEN Zhiqiang. Progress in Space VLBI Science [J]. Progress In Astronomy, 1998, 6: 117-134 WAN Tongshan. The Present and Future of Space VLBI [J]. Progress In Astronomy, 1999, 6: 136-147 ISAS.VSOP-2 Proposal Abridged English Version.http://www.vsop.isas.jaxa.jp/vsop2/ NAG (1989). Precise Orbit Determination of RADIOASTRON, Report of the RADIOASTRON NAG Group to the Eighth RADIOASTRON Meeting, Greenbank, WV, May 1-5 WEI Erhu. Research on the Designment of Chinese Space VLBI System and Computation Simulation[D]. Wuhan University. 2006.

YANG Ying, WANG Qi. STK in computer simulation application [M]. National defence industry press. 2002

 

WEI Erhu

Associate professor,
Ph. D, School of Geodesy and
Geomatics, Wuhan University, China.
ehwei@sgg. whu. edu. cn
   

LIU Jingnan

President,
Wuhan University, Academician of CAE,
China
jnliu@whu.edu.cn
   

YAN Wei

Master candidate,
Croatia,
School of Geodesy and Geomatics,
Wuhan University, China.
2201feihong@163.com
   
     
 
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