Technical description of solution bkgint08 Intensives 1. Purpose of solution: Intensive EOP 2. Analysis center: Federal Agency for Cartography and Geodesy (BKG Leipzig) 3. Short narrative description of solution: All available Intensive sessions since 1999 were analysed for this solution (including the TSUKUBA-WETTZELL experiments since 2002). Celestial reference frame was fixed to bkg00011 global solution except for the 212 defining sources with values taken from the ICRF.Ext1 catalogue. Terrestrial reference frame VTRF2008a and the associated velocity field are used for station coordinates, reference epoche is 2000.0. Only clock parameters, tropospheric zenith parameters and UT1 were adjusted using least squares technique. The UTC epoch is the middle epoch for each session. The values of the official list of VLBI antenna axis offsets issued by the IVS Analysis Coordinator (http://vlbi.geod.uni-bonn.de/IVS-AC/Conventions/antenna-info.txt, update 2009-03-16) were used. Mean pole coordinates used for computation of pole tide deformation were applied according to IERS Conventions 2003 (eq. 23a, 23b). The Vienna mapping function (VMF1) is applied for troposphere correction modelling. A priori short-period tidal variations in EOP were taken into account in accordance with IERS Conventions 2003. Ocean loading model FES2004 computed by H. G. Scherneck was used. Thermal expansion modelling developed by A. Nothnagel was used (http://vlbi.geod.uni-bonn.de/IVS-AC/Conventions/antenna-info.txt). The values of station eccentricities were taken from the official IVS-table ECCDAT.ecc. 4. Estimated parameters: a. Celestial frame: No b. Terrestrial frame: No c. Earth orientation: UT1-TAI d. Zenith troposphere: Generally offsets for each session e. Troposphere gradient: No f. Station clocks: 3h piece-wise linear functions, rate constraint 5*10E-14 g. Baseline clocks: Not generally used as most are single baseline h. Other: No 5. Celestial reference frame: a. A priori source positions: bkg00011 global solution b. Source positions adjusted in solution: No 6 - Terrestrial reference frame: a. a priori station positions: VTRF2008a b. a priori station velocities: VTRF2008a c. Reference epoch: 2000.0 7. Earth orientation: a. A priori precession model: IERS 2003 b. A priori nutation model: MHB2000 c. A priori short-period tidal variations in x, y, UT1: a priori short-period tidal variations in x, y, UT1 were taken into account in accordance with IERS Conventions 2003 d. EOP estimation: UT1-TAI for each session. 8. A priori geophysical models: a. Troposphere: hydrostatic component with VMF1 mapping function b. Solid Earth tide: IERS Conventions c. Ocean loading: FES2004 model d. pole tides: IERS Conventions e. Atmosphere loading: none 9. Data type: Group delays 10. Data editing: 5 deg elevation cutoff, editing of outliers during adjustment when necessary 11. Data weighting: Observations are weighted using std reported in observational files; re-weighting iteration for each session to achieve the chi-square unity. 12. Standard errors reported: Reported formal errors are derived from least-squares estimation propagated from data uncertainties and weighted as discussed in #11. 13. Software: Calc 10, SOLVE release: 2008.12.05 14. Other information: Field 18 contains the session code Field 19 contains the duration of experiments