Technical description of dgf2018a.snx ------------------------------------- 1. Purpose: Datum-free VLBI session normal equation files in SINEX 2.02 format, including station/source coordinates and EOP. 2. Analysis Center: Deutsches Geodaetisches Forschungsinstitut (DGFI-TUM), Technische Universitaet Muenchen, Munich, Germany 3. Estimated parameters: a. Celestial frame: Yes b. Terrestrial frame: Yes c. Earth orientation: Pole coordinates and their first derivatives, UT1-UTC and LOD, dX, dY, each valid for the duration of the session (normally 24 h), reference epoch is mid of session d. Zenith troposphere (per station): continuous piece-wise linear function (1 hour) rate constraint 66.0 ps/h e. Troposphere gradient (per station): discontinuous piece-wise linear function (24 hours) offset constraint 2.5 ps rate constraint 5.0 ps/h f. Station clocks (per station): Quadratic function per session plus a continuous piece-wise linear function (1 hour) offset constraint 66.0 ps rate constraint 135.0 ps/h (clock jumps estimated additionally) 4. Celestial reference frame: a. A priori source positions: ICRF2 b. Source positions adjusted in solution: Yes (>3 observations) 5 Terrestrial reference frame: a. A priori station positions: ITRF2014 b. A priori station velocities: ITRF2014 c. Axis offsets: taken from official IVS-table http://vlbi.geod.uni-bonn.de/Analysis/Thermal/antenna-info.txt d. Reference epoch: session epoch 6. Earth orientation: a. A priori precession/nutation model: IAU2006A b. A priori x and y pole coordinates and rates, UT1-UTC and rate: IERS EOP 14 C04, cubic window interpolation c. A priori short period (~daily and subdaily) tidal variations in x, y, dUT1: IERS Conventions 2010 d. EOP estimation: Pole coordinates and rates, UT1-UTC and rate (UT1dot), dX, dY, each valid for the duration of the session (normally 24 h), reference epoch is mid of session (see the SOLUTION/APRIORI block) 7. A priori geophysical models: a. Troposphere: hydrostatic component from surface pressure (in general as reported in the NGS files) mapped with the VMF1 dry mapping function, wet delay is estimated with the VMF1 wet mapping function. A priori values for the gradients are from TU Wien (Boehm & Schuh, 2007) since 2005.0 and from GSFC (MacMillan, 1995, and MacMillan & Ma, 1997) before 2005. b. Solid Earth tide: IERS Conventions 2010 c. Tidal ocean loading: FES2004 d. Pole Tide: IERS Conventions 2010 e. Atmosphere loading: Petrov & Boy (2003) https://lacerta.gsfc.nasa.gov/aplo_eph/ f. Thermal deformation: according to IVS conventions http://vlbi.geod.uni-bonn.de/Analysis/Thermal/antenna-info.txt 8. Data type: Group delays 9. Data editing: 5-degree elevation cut-off 10. Data weighting: Only observations with a zero quality flag in NGS cards are used. All observations are subject to an outlier test (data snooping). 11. Software: DOGS-RI 1.0 12. Further information: The SINEX 2.02 files include datum-free normal equations only, no solution. None of the station/source position parameters or EOP reported in this file are subject to any constraints.