Computer aided detection of transient inflation events at Alaskan volcanoes using GPS measurements from 2005–2015

Abstract

Analysis of transient deformation events in time series data observed via networks of continuous Global Positioning System (GPS) ground stations provide insight into the magmatic and tectonic processes that drive volcanic activity. Typical analyses of spatial positions originating from each station require careful tuning of algorithmic parameters and selection of time and spatial regions of interest to observe possible transient events. This iterative, manual process is tedious when attempting to make new discoveries and does not easily scale with the number of stations. Addressing this challenge, we introduce a novel approach based on a computer-aided discovery system that facilitates the discovery of such potential transient events. The advantages of this approach are demonstrated by actual detections of transient deformation events at volcanoes selected from the Alaska Volcano Observatory database using data recorded by GPS stations from the Plate Boundary Observatory network. Our technique successfully reproduces the analysis of a transient signal detected in the first half of 2008 at Akutan volcano and is also directly applicable to 3 additional volcanoes in Alaska, with the new detection of 2 previously unnoticed inflation events: in early 2011 at Westdahl and in early 2013 at Shishaldin. This study also discusses the benefits of our computer-aided discovery approach for volcanology in general. Advantages include the rapid analysis on multi-scale resolutions of transient deformation events at a large number of sites of interest and the capability to enhance reusability and reproducibility in volcano studies.

Episodic inflation events at Akutan Volcano, Alaska, during 2005–2017

“…In March 1996, an intense earthquake swarm was accompanied by uplift as much as 60 cm on the west flank of Akutan [Lu et al, 2000b[Lu et al, , 2005. Small inflation events occurred in 2008 [Ji and Herring, 2011;Li et al, 2016] and in 2011 [Walwer et al, 2016], identified with Global Positioning System (GPS) data. The 1996The , 2008, and 2011 events did not culminate in an eruption, and they may be episodes of magma accumulation in a shallow reservoir underneath Akutan.…”