G41A-0994
Integration Of Low-Cost Single-Frequency GPS Stations Using 'Spider' Technology Within Existing Dual-Frequency GPS Network at Soufrière Hills Volcano, Montserrat (West Indies): Processing And Results

Thursday, 17 December 2015
Poster Hall (Moscone South)
Karen Pascal1,2, Kirill Palamartchouk3, Richard G Lahusen4, Kirby Young4,5 and Barry Voight6, (1)Montserrat Volcano Observatory, Flemmings, Montserrat, (2)Seismic Research Centre, University of the West Indies, St Augustine, Trinidad and Tobago, (3)Newcastle University, School of Civil Engineering and Geosciences, Newcastle, United Kingdom, (4)Pennsylvannia State University, University Park, PA, United States, (5)Northeastern University, Boston, MA, United States, (6)Pennsylvania State Univ, University Park, PA, United States
Abstract:
Twenty years ago, began the eruption of the explosive Soufrière Hills Volcano, dominating the southern part of the island of Montserrat, West Indies. Five phases of effusive activity have now occurred, characterized by dome building and collapse, causing numerous evacuations and the emigration of half of the population.

Over the years, the volcano monitoring network has greatly expanded. The GPS network, started from few geodetic markers, now consists of 14 continuous dual frequency GPS stations, distributed on and around the edifice, where topography and vegetation allow. The continuous GPS time series have given invaluable insight into the volcano behavior, notably revealing deflation/inflation cycles corresponding to phases and pauses of effusive activity, respectively.

In 2014, collaboration of the CALIPSO Project (Penn State; NSF) with the Montserrat Volcano Observatory enriched the GPS and seismic monitoring networks with six ‘spider’ stations. The ‘spiders’, developed by R. Lahusen at Cascades Volcano Observatory, are designed to be deployed easily in rough areas and combine a low cost seismic station and a L1-only GPS station. To date, three ‘spiders’ have been deployed on Soufrière Hills Volcano, the closest at ~1 km from the volcanic conduit, adjacent to a lava lobe on the dome.

Here we present the details of GPS data processing in a network consisting of both dual and single frequency receivers (‘spiders’) using GAMIT/GLOBK software. Processing together single and dual frequency data allowed their representation in a common reference frame, and a meaningful geophysical interpretation of all the available data. We also present the ‘spiders’ time series along with the results from the rest of the network and examine if any significant deformation, correlating with other manifestations of volcanic activity, has been recorded by the ‘spiders’ since deployment. Our results demonstrate that low cost GNSS equipment can serve as valuable components in volcano deformation monitoring networks.