Goddard VLBI global solution 2007a
Goddard global solution 2007a used all available dual band VLBI observations
(except VLBA Calibrator Survey) at 8.4 GHz and 2.2 GHz from 1979.08.03 to
2006.12.14, 4232 diurnal sessions,
5,330,408 measurements of group delays.
Single combined least square solution was done.
Technical description provides additional
details.
Source positions
Positions of 710 sources were estimated as global parameters.
The sources that A) were observed in two or more sessions and had 40 or
more good observations or B) were observed only in one session and had 25
or more good observations were included in the group of sources whose
positions were estimated as global parameters. Positions of these sources
are presented in catalogue 2007a.sou . The sources which had only
one good observation as well as two gravitational lenses,
0218+35A/0218+35B and 1830-21A/1830-21B, were excluded from the dataset.
Position of other 204 sources were estimated in each session individually.
Time series of their positions are presented in 2007a.lso file. Mean
values of their position are presented in catalogue 2007a_lso.sou .
Station positions and velocities
Positions of 153 stations and their velocities were estimated as global
parameters. Station positions are given on epoch 1997.01.01
Earth orientation parameters
Pole coordinates X, Y, UT1 angle, and their rate, daily correction to the
nutation in longitude and nutation in obliquity were estimated for each
session separately.
Assessment of accuracy of EOP series
Comparison of EOP parameters determined from 80 simultaneous 24 hours
VLBI experiments at networks CORE-A and NEOS-A.
- Plot of differences in
X pole coordinates;
- Plot of differences in
Y pole coordinates;
- Plot of differences in
UT1 angles;
- Plot of differences in
nutation in longitude;
- Plot of differences in
nutation in obliquity;
- Plot of differences in
X pole rates;
- Plot of differences in
Y pole rates;
- Plot of differences in
UT1 rates;
- Table of statistics of the
differences.
Statistics
Comparison of EOP series
Comparison with
IERS C04
series shows random noise with slight linear trend with scatter comparable
with the accuracy of VLBI EOP series, except UT1 where the noise of IERS C04
series is dominating.
- Plot of the differences with IERS C04 in
X pole coordinates;
- Plot of the differences with IERS C04 in
Y pole coordinates;
- Plot of the differences with IERS C04 in
UT1 angles;
- Plot of the differences with IERS C04 in
nutation in longitude;
- Plot of the differences with IERS C04 in
nutation in obliquity;
- Table of statistics of the
differences.
Miscellaneous
| Listing of the Solve solution.
|
in spool format.
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solution page.
Web page was prepared by Leonid Petrov
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Last update 27-DEC-2006 17:27:59