For the Californian network
glorg is used to estimate daily translations of the network with
the orienataion constrained to the IERS Bulletin A values. Over the
125 km extent of this network, 1 mas error in Earth orientation
should change the relative coordinates by <1 mm.
The California globk command file and
glorg command file can be viewed
with these hyper-links. globk.usesite contains
the name of the sites used in the globk solution (used to eliminate
un-wanted sites). glorg.cali.usesite
and glorg.cont.usesite contain
the names of the sites used for the origin constraint in the California
and Central Asia glorg runs.
The current California RMS scatters
are updated daily.
For the Central Asia network
which spans 1800 km we estimate only
translation in glorg (same as the smaller California network).
The Central Asia globk command file and
glorg command file can be viewed
with these hyper-links. The same rotational constraints are applied
as California. (These constraints were previously 10-times larger).
The current Central Asia RMS scatters
are updated daily. These summary files include both the orginal larger
Central Asia network (with translation and rotation) and the
smaller network (with only translation).
In both analyses, the SIO orbits are constrained to +-100 mm in position and 0.01 mm/sec in velocity. Radiation parameter adjustments are constrained to 1% of the direct radiation pressure.
The data from Central Asia is collected in collaboration with the Russian Academy of Sceinces Institute for High Temperature Physics (IVTAN). The IVTAN web page contains more information about the continuous sites and the GPS campaigns that have been carried out in the region.
The results shown on these pages were made possible by support
from the National Science Foundation
(NSF), the National Aeronautics and
Space Administration
(NASA), the Southern California Earthquake Center
(SCEC),
and the University Navstar Consortium
(UNAVCO).
|
|
Introduced site-dependent data noise computed from postfit residuals with an elevation angle dependent model. |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
The atmospheric delay plots for these sites show the 6-hourly estimates from the NCEP analysis field (in red; other sites show the daily mean value). We save the statistics of the RMS scatter of the phase residuals and the number of phase measurements as a function of elevation angle. RMS phase residuals by date and elevation angles Number of phase residuals by date and elevation angles (Multiply fractional part of year by 365 to get day-of-year) |
|
|