Twentieth century constraints on sea level change and earthquake deformation at Macquarie island

• Published in: Geophysical Journal International
• Main Authors: Watson, CS, Burgette, RJ, Tregoning, P, White, P, Hunter, JR, Coleman, R, Handsworth, R, Brolsma, H
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley-Blackwell 2010
• Subjects: Earth Sciences; Physical geography and environmental geoscience; Physical geography and environmental geoscience not elsewhere classified; Antarctic; Antarc*; Macquarie Island
• Online Access: https://doi.org/10.1111/j.1365-246X.2010.04640.x; http://ecite.utas.edu.au/64046

Through the combination of rare historical sea level observations collected during Sir Douglas Mawson's 1911-1914 Australasian Antarctic Expedition (AAE), together with modern sea level data, space geodetic estimates of crustal displacement and modelling of coseismic and post-seismic earthquake deformation, we present a contemporary analysis to constrain sea level and land level change over the twentieth century at Macquarie Island (54degree 30S, 158degree 57E).We combine 9 months of 1912-1913 sea level data with intermediate observations in 1969-1971, 1982 and 1998-2007 to estimate sea level rise relative to the land at +4.8 +/- 0.6 mm yr-1. Combined with estimates of global mean sea level rise, this value supports the geologically surprising notion of land subsidence, conflicting with longer term geological evidence that suggests uplift at ~0.8 mm yr-1 over the last 400-300 Kyr. We investigate the current tectonic evolution of the Island through analysis of Global Positioning System (GPS) solutions that utilize data over the period 2000-2009. Importantly, this provides an opportunity to refine the source parameters of the Mw ~8.0 great earthquake of 2004 December 23 using estimates of coseismic displacements at regional GPS sites. We use the estimated earthquake source and GPS observations of four years of post-seismic deformation at Macquarie Island to infer the rheology of the oceanic upper mantle. We find that an asthenosphere bounded by stronger material above and below is required to produce the observed post-seismic deformation, particularly in the vertical component. Assuming a Maxwell rheology, the best fit is given by an asthenospheric viscosity of 3x1019 Pa s. The inferred rheology determined from the 2004 earthquake is used to model long period post-seismic deformation from Mw ~8.0 earthquakes of 1989 and 1924. The 1924 earthquake is the closest of the three great earthquakes to Macquarie Island, and our modelling suggests that the majority of the vertical deformation at the tide gauge over the ...