ITRF2000 post-fit residuals at colocation sites: positions The scaled standard errors result from the application of the multiplicative factor derived for each analysis center in the ITRF combination algorithm. ============================================================================== ============================================================================== 40439 OWENS VALLEY Residuals (mm) Scaled Std. Err.(mm) Epoch Ties SSC East North Up East North Up ------------------------------------------------------------------------------ M001 TIE40439 .3 -.1 .0 3.7 3.5 .4 1997.00 S002 TIE40439 1.1 -6.4 22.5 6.4 8.8 8.6 1997.00 ============================================================================== 40439 OWENS VALLEY Residuals (mm) Scaled Std. Err.(mm) Epoch VLBI SSC East North Up East North Up ------------------------------------------------------------------------------ M004 R GSFC -4.1 -.6 -2.8 14.9 19.0 18.2 1987.84 M004 R SHA -2.6 2.3 1.3 16.3 18.4 19.2 1987.84 S002 R GIUB 3.2 3.2 -7.2 9.6 11.9 11.9 1987.29 S002 R GSFC -1.8 -1.3 -29.5 5.7 7.6 7.8 1986.88 S002 R SHA -1.4 -1.6 -28.0 8.9 10.8 11.1 1991.46 S006 R GIUB 1.4 2.1 -2.4 2.1 2.8 2.6 1995.41 S006 R GSFC .5 .6 3.0 1.1 1.4 1.4 1995.42 S006 R SHA .7 .3 3.7 2.3 2.6 2.6 1996.23 ============================================================================== 40439 OWENS VALLEY Residuals (mm) Scaled Std. Err.(mm) Epoch SLR SSC East North Up East North Up ------------------------------------------------------------------------------ M001 L4 CSR -31.2 9.3 -2.7 70.4 92.4 92.2 1980.75 M003 L4 CSR -280.6 -84.1 -1261.5 648.6 885.3 885.8 1978.19 M004 L CGS -84.2 1.5 40.6 23.9 20.0 22.4 1997.00 M004 L4 CSR 9.1 -28.5 -14.0 47.3 61.9 62.8 1989.05 M004 L DEOS 16.1 15.1 96.0 104.5 127.3 115.4 1991.74 ============================================================================== 40439 OWENS VALLEY Residuals (mm) Scaled Std. Err.(mm) Epoch Multi SSC East North Up East North Up ------------------------------------------------------------------------------ M004 C GRIM 16.0 -19.1 -32.7 20.1 22.5 22.5 1988.90