spu2015a.eops.txt Technical description of solution spu2015a 1. Purpose of solution: Session EOP 2. Analysis Center: Saint-Petersburg University (SPU) 3. Short narrative description of solution: Observational VLBI groupe delays (IRIS-A and NEOS-A since 2-Jan-1989 and R1, R4 since 1-Jan-2002) have been analyzed for this solution. Reductional model is realised in accordance with the IERS Conventions 2003. Relativistic corrections are calculated in accordance with the IERS consensus model. Celestial reference frame was fixed to the ICRF Extension catalogue. A priori terrestrial reference frame was the VTRF2005 catalogue, but daily station coordinates have been estimated under NNR and NNT constraints. VTRF2005 velocity field is used for station coordinates calculation. All parameters under estimation have been adjusted using Kalman filter technique. Troposphere wet delay is modeled as a stochastic process like random walk with spectral density equal to 0.1 picosec**2/sec. Clock offset is considered as a random walk stochastic process with spectral density equal to 1.0 picosec**2/sec. Clock rate is considered as a constant parameter. Troposphere gradients are modeled as a constant parameters. 4. Estimated parameters: a. celestial frame: No b. terrestrial frame: Yes c. Earth orientation: X, Y, UT1-UTC, dpsi, deps d. zenith troposphere: Random walk process e. troposphere gradient: constant parameters f. station clocks: Offset as a random walk process, rate as a constant g. baseline clocks: No h. other: No 5. Celestial reference frame: a. priori source positions: ICRF Ext.2 b. source positions adjusted in solution: No c. solution identification or reference: ICRF Ext.2 6 - Terrestrial reference frame: a. priori station positions: VTRF2005 b. priori station velocities: VTRF2005 velocity field c. reference epoch: 1997.0 d. station positions/velocities adjusted in solution: station positions adjusted on daily basis l. solution identification or reference: VTRF2005 7. Earth orientation: a. a priori precession model: IAU2000A b. a priori nutation model: IAU2000A c. a priori short-period tidal variations in x, y, UT1: Model (IERS Conventions 2003) d. EOP estimation: X, Y, UT1-UTC, dpsi, deps every session 8. A priori geophysical models: a. troposphere: VMF1 mapping function for dry and wet delays b. solid Earth tide: IERS Conventions 2003. c. ocean loading: IERS Conventions 2003. d. atmosphere loading: information about local pressure for separate VLBI sites has been used from server of Onsala Space Observatory 9. Data type: delays 10. Data editing: Only data with zero quality flag in NGS format are used 11. Data weighting: Observations with elevation less than 5 degrees to be divided by sin(elevation). Observations with elevation more than 5 degrees are not weighted as a rule, but Kalman filter approach checks a quality of every observation and downweights it in case of bad result. 12. Standard errors reported: Formal errors are derived from Kalman filter adjustment 13 Software: OCCAM v. 6.2 14. Other information: ------------------------------------------------------------------------------ Dmitriy Trofimov senior lecturer of Astronomy department Tel: +7-(812)-428-41-99 Fax: +7-(812)-428-71-29 Sobolev Astronomical Institute of Saint-Peterburg University Universitetskii pr., 28, Petrodvorets, Saint-Petersburg, Russia, 198504 d.trofimov@spbu.ru