Message-ID: <39527C15.38E1A869@geod.nrcan.gc.ca> Date: Thu, 22 Jun 2000 16:50:29 -0400 From: Remi Ferland To: igsmail@igscb.jpl.nasa.gov Subject: [IGSMAIL-2899]: Original / New realization of ITRF97 Sender: owner-igsmail Precedence: bulk ****************************************************************************** IGS Electronic Mail 23 Jun 11:22:02 PDT 2000 Message Number 2899 ****************************************************************************** Author: Remi Ferland Dear Colleagues, As you are well aware, starting with GPS week 1065 we have switched to a new realization of ITRF97 (IGS00P04_RS51.SNX). The new realization is a subset of the cumulative solution IGS00P04.snx, containing weekly solutions from the last 4 years (1996-1999). It can be found in: ftp igscb.jpl.nasa.gov cd /pub/station/coord get IGS00P04_RS51.SNX.Z It replaces the original realization of ITRF97 (ITRF97_IGS_RS51.SNX) extracted by Zuheir from the ITRF97 solution, and available at the same location. The objective of the change was to ensure a better internal consistency of the IGS products. The new realization has been aligned to the original realization to minimize potential discontinuities. The magnitude of discontinuity was checked by transforming the weekly combinations (1060-1064) using the new IGS realization "IGS00P04_RS51.snx". This week solution (1065) was transformed using "ITRF97_IGS_RS51.snx". All transformations were unweighted. The statistics of the 6 weekly transformation are : Parameter Average Std. Normalized --------- ------- ---- ---------- R X (mas) 0.0152 (+-0.0081) 1.8 R Y (mas) 0.0063 (+-0.0041) 1.5 R Z (mas) -0.0022 (+-0.0073) -0.3 T X (m) -0.0007 (+-0.0003) -2.1 T Y (m) 0.0005 (+-0.0002) 2.0 T Z (m) 0.0002 (+-0.0002) 0.9 SCL (ppb) -0.0807 (+-0.0294) -2.7 Note: Signs of GPS 1065 transformations have been reversed to ensure consistency. Based on the small sample containing the 6 most recent weeks, there is no significant difference (at 3 sigmas) between the two realizations of ITRF, when applied to the weekly combination. The transformation parameters uncertainty derived from the propagation of the covariance information from the weekly solutions and the ITRF realization is about 0.04mas in rotation, 1.0mm and 1.5mm in XY and Z translation and 0.2ppb in scale. This also indicates that the average transformation parameters are not significant! The discontinuity on the cumulative solution (IGS00P23.snx) expressed in terms of the transformation parameters is: R X (mas) -0.00010 R Y (mas) -0.00004 R Z (mas) -0.00026 T X (m) 0.00000 T Y (m) 0.00001 T Z (m) 0.00000 SCL (ppb) -0.00055 d R X (mas/y) -0.00015 d R Y (mas/y) -0.00003 d R Z (mas/y) -0.00033 d T X (m/y) 0.00000 d T Y (m/y) 0.00001 d T Z (m/y) 0.00000 d SCL (ppb/y) -0.00107 The discontinuity on the cumulative solution for GPS weeks 1060-1064 is (as expected) almost identical to the transformation given above. The magnitude of transformations are very small … they are well within the noise level! Please feel free to do your own comparison, Best Regards, Remi, --------------4DE546B51CD206EAA1CE4177 Content-Type: text/x-vcard; charset=us-ascii; name="ferland.vcf" Content-Transfer-Encoding: 7bit Content-Description: Card for Remi Ferland Content-Disposition: attachment; filename="ferland.vcf" begin:vcard n:Ferland;Remi tel;fax:(613) 995-3215 tel;work:(613) 995-4002 x-mozilla-html:FALSE org:Geodetic Surveys;Natural Resources Canada adr:;;456 - 615 Booth Street;Ottawa;Ontario;K1A 0E9;Canada version:2.1 email;internet:ferland@geod.nrcan.gc.ca title:Research Officer fn:Remi Ferland end:vcard --------------4DE546B51CD206EAA1CE4177--