The Southwest Pacific GPS Project: Geodetic results from Burst 1 of the 1990 Field Campaign |
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| Authors: | B Schutz M Bevis F Taylor D Kuang P Abusali M Watkins J Recy B Perin O Peyroux |
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| Institution: | (1) Center for Space Research, The University of Texas at Austin, USA;(2) Marine, Earth and Atmospheric Sciences, North Carolina State University, USA;(3) Institute for Geophysics, The University of Texas at Austin, USA;(4) Institut Français de Recherche Scientifique Pour le Developpement en Cooperation (ORSTOM), France;(5) University Navstar Consortium (UNAVCO), USA;(6) Cook Islands Survey Department, UK |
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| Abstract: | The Southwest Pacific GPS Project (SWP) is using the Global Positioning System (GPS) to monitor crustal motion across and within a plate boundary complex between the Australian and Pacific plates. GPS field campaigns were conducted in 1988, 1989 and 1990, to observe networks of increasing size and complexity. The 1990 campaign consisted of two periods, or  Bursts , and this paper focuses on the analysis of data collected during the nine day Burst 1 in July, 1990, a period in which GPS Selective Availability was activated. During Burst 1, baselines that spanned the Tonga Trench and the Lau Basin were observed, and only one station (Espiritu Santo, Vanuatu) was located west of Fiji in the network. The lengths of the baselines observed fall mainly between 300 km and 1600 km, but some lines are as long as 3500 km. A total of 78 station-days of field site data and approximately 150 station-days of global fiducial data were processed from predominantly codeless receivers. A global fiducial network of 20 sites was used to provide orbit control and accuracy assessment for the 13 available satellites. The daily solutions for 45 baselines between 10 SWP sites have an RMS scatter in the length of 24 mm plus 6 parts per billion. This scatter provides an estimate of baseline precision for the Burst 1 nominal solution. Experiments were conducted to investigate a variety of possible effects on the SWP Network baseline estimates, including the influence of a reduced global fiducial network for the purpose of assessing the quality of results obtained in 1988 and 1989 in which the fiducial network was smaller than in 1990. These experiments produced results that agreed with the nominal solution at the level of the precision estimate. Furthermore, estimates for selected baselines in Australia, the Central Pacific, North America and Europe, also measured by VLBI and SLR, were used for an external accuracy evaluation. The GPS and VLBI or SLR determinations of length agreed at a level consistent with the nominal solution precision estimate. |
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