USArray
A Continental-scale Seismic Observatory

Transportable Array Deployment to Alaska and Western Canada

The EarthScope Transportable Array (TA) is a dense network of state-of-the-art seismic stations that, from 2004-2015, migrated across the contiguous 48 states recording the high-quality data needed to map the structure of the earth beneath North America. The project sponsored by the National Science Foundation (NSF) and deployed by Incorporated Research Institutions for Seismology (IRIS) already has made possible a growing body of significant, peer reviewed science that furthers our understanding of the continent, its formation, and its hazards.

Deployment to Alaska

The Transportable Array has since moved north to Alaska and western Canada. A few test stations were installed in 2011-2013 before deployment began in earnest in 2014. In all, TA’s Alaska phase comprises 280 stations and will run to 2020 when removals will begin. All stations are now in the ground, including 72 cooperating stations from existing networks operated largely by the Alaska Earthquake Center but also including stations operated by Alaska Volcano ObservatoryNational Tsunami Warning Center, and Canadian Hazard Information Service. The array is a grid of stations spaced about 85km apart covering all of mainland Alaska and parts of the Yukon, British Columbia, and the Northwest Territories (Figure 1). An interactive map of active TA stations is available here.

The Transportable Array team planned to remove the remaining Alaska TA stations this summer during the 2020 field season. Due to local, state, and federal travel restrictions in response to the pandemic and with the support of the National Science Foundation (NSF), IRIS postponed removal of most of these stations to the 2021 field season. Data telemetry will continue until May 2021 and the Array Network Facility (ANF) will continue to support archival at the IRIS DMC along with processing onsite baler media as it is returned from removals.

The timeline of operations, transitions, and removals for the Alaska TA stations is being executed as follows:

  • In Fall 2019, 43 stations were transferred to the AEC under the AK network code, leaving 151 to be operated by IRIS.
  • By May 1 2020, 24 additional stations were transitioned to other operators.
  • During the 2020 field season, all remaining stations continued to be operated with data telemetry and archival at the IRIS DMC.
    • Limited station removals were done while adhering to all local, state, and federal travel restrictions as well as employing a limited contact strategy developed specifically for the Alaska TA project.
  • By September 30 2020, 45 stations will be transferred to the AEC under the AK network code as part of a funded award in response to the 19-048 NSF Dear Colleague Letter.
  • On May 1 2021, telemetry will be turned off of the remaining stations and real-time data collection will cease.
  • During the 2021 field season, all remaining stations will be removed. All baler media returned before September 1 2021 will be processed at ANF.

A subset of Alaska Transportable Array stations have been or are in the process of being transitioned to other network operators. Seismic data will still be archived and available via the IRIS DMC, with a change of network code and, in some cases, a change in sample rate or channel/location code. This might require adjusting data retrieval scripts. The full list of adopted or continuing Transportable Array stations is available under the virtual network _US-TA-ADOPTED. Note that this will be updated to include stations as their data acquisition is transferred.

Station hosts and the public can view data in webicorder or event views from stations or locate the nearest station with real-time data using the IRIS Station Monitor app

A paper on the Alaska Transportable Array will be published in a focus section of Seismological Research Letters in November and is already available online at: https://doi.org/10.1785/0220200154. A longer format final report is in preparation and will be made available on this website.

IRIS would like to thank the National Science Foundation for their continued support of the Alaska Transportable Array project through NSF Award EAR-1261681.

Figure 1: Current TA Footprint. "TA" sites (circles) are new seismic stations, and "Existing" sites are either upgraded (squares) or as-is (triangles) contributing seismic stations. Station locations are available in KMZ and CSV format (version 10/25/2018).

Scientific Motivations

There were strong scientific motivations for shifting the TA to Alaska. Alaska is the nation’s most seismically active state, with more large and moderate earthquakes than the rest of the country combined. Furthermore, that seismicity is varied in nature and spread across the entire state (Figure 2), including regions that have never been closely monitored. The pre-TA instrumentation simply was not adequate for investigating the forces at play in many of the state’s far-flung regions. New TA stations have already greatly increased earthquake detections in Southeast Alaska, Southwest Alaska, and the North Slope. As in the contiguous 48 states, this unprecedented station coverage makes possible new research into the structure of the earth beneath Alaska.

Figure 2: Seismicity from 1970-2012 for Alaska and vicinity from the Alaska Earthquake Center and USGS PDE catalogs, click for pdf. Figure courtesy of Natalia Ruppert (AEC).

Meteorological and Soil Temperature Data

Transportable Array stations are equipped with atmospheric sensors, including barometers and infrasound microphones (Figure 3). Because of the density of the TA network, this atmospheric data is proving valuable for studying weather and atmospheric events in remote, sparsely monitored regions, as well as for wildlfire response.

Figure 3: Locations of Meteorological (MET) sensors in the TA. Priority for co-located MET and seismic sensors was given to stations in remote areas that have not had meteorological sensor coverage before.

78 of the TA sites are instrumented with soil temperature profilers, the majority provided by the NASA ABoVE program but also by the Yukon Geological Survey. These stations complement an existing temperature monitoring network, allowing for better characterization of ground temperatures and permafrost conditions in northern and western Alaska. Subsurface temperatures depend on many variables, including snow cover, vegetation, terrain, and soil properties. Mean temperatures for a study region may not account for “hot spots” of change, which can significantly contribute to thaw and associated carbon emissions. A solution is to record temperature regimes within different ecotypes in order to build a portfolio of subsurface thermal regimes across various ground conditions. The TA sites are valuable for calibration and validation efforts and for informing thermal regime modeling. More information about this permafrost project can be found here.

Data Management

Transportable Array data is publicly available via the IRIS Data Management Center and is utilized by the USGS National Earthquake Information Center and NOAA Tsunami Warning Center for real-time hazard monitoring. Additionally, many TA stations in the contiguous 48 states were retained as part of the separately funded project, Central and Eastern United States Network (CEUSN). Data from these stations is available from the IRIS Data Management Center with network code N4.

Station Design

Alaska’s climate and geography demanded extensive station redesign to achieve the data return rates required for this project (Figure 4). Installing the sensors far enough underground for optimal data quality required designing a lightweight drill rig that could be flown to the sites by helicopter. Clusters of lithium iron phosphate batteries power the equipment through the long winter and are recharged by solar power systems during the summer. Most of the stations are located in wilderness, far from any telecommunications infrastructure. Near-real-time telemetry is provided by InMarSat BGAN, Iridium, cellular, or direct radio links.  With datalogger capacities of up to 64 GB storage, stations can maintain a complete record from 8+ years of deployment.

Figure 4: Schematic for an Alaska TA station, click to enlarge.

Each TA station’s seismograph system consists of a Quanterra Q330 datalogger connected to a three-component broadband seismometer (T120PH or STS-4B/5A) installed in a 6-inch diameter shallow borehole at a depth of about 2.8 meters. The standard TA atmospheric sensor package includes a MEMS state-of-health barometer, NCPA infrasound sensor, and SETRA microbarograph. Some stations also include a soil temperature profiler.

As an example of a typcial Alaska TA station, M29M was constructed and installed in just two days on July 26-27, 2016 along Somme Creek in the Yukon (Figure 5). The seismometer was installed using a down-the-hole hammer to drill a 2.7 meter steel cased hole into an igneous bedrock ridge line. For more photos of installation, see this mid-2017 field season report.

     

Figure 5. M29M construction (top left), weather sensor (top right), and final station exterior (bottom). Photo credit: Jeremy Miner

After 2019

Alaska’s TA stations are scheduled to be removed beginning in 2020. Because the Alaska phase has brought stations to active regions of Alaska that were previously unmonitored, efforts are underway to secure funds for incorporating some of these into Alaska’s permanent seismic network. With funding from USGS, 43 stations primarily in the south central region of Alaska will be transitioned to be operated by the Alaska Earthquake Center starting in September 2019. The NSF Dear Colleague Letter: "Repurposing the Alaska Transportable Array to Support Observations of Arctic Environmental Change" outlines another possible path forward for continuing observations using these stations. As with the inter-agency-funded CEUSN in the contiguous 48 states, there is broad agreement that TA stations in Alaska represent an important new capability for answering basic geologic questions and evaluating risks to life and infrastructure. Presentations and recommendations from the USArray Sustainability Workshop in 2016 are available at the ARCUS website.

Figure 6. Typical Alaska TA station installs were constructed in a single day with a four-person crew plus pilots. The drill and station hut are helicopter portable so that stations can be constructed in very remote regions.

Funding and Partners

The USArray Transportable Array is sponsored by the National Science Foundation. The successful funding of the IRIS SAGE proposal made possible the TA’s redeployment as a single, static footprint in Alaska and northwestern Canada through to 2020. The Transportable Array Advisory Committee (TAAC) advises on the operation and technical performance of the TA in the context of EarthScope's science goals and changes in annual budgets. 

The Alaska deployment of the USArray Transportable Array has cooperation and support from the Alaska Earthquake Center at the Geophysical Institute, University of Alaska Fairbanks. The AEC handles the telemetry and data acquisition for 54 stations in the Alaska TA network. Cooperation with the Canadian Hazards Information Service, Yukon Geological Survey, and Natural Resources Canada has also been vital to extending TA stations across the border.

The investment of EarthScope directly benefits other seismic network operators in Alaska, many of which are focused on characterizing seismic, volcanic, and tsunami hazards. IRIS also works with the Alaska Earthquake Center, Alaska Volcano Observatory, and the Alaska Tsunami Warning Center to upgrade and leverage existing seismic infrastructure and permitting wherever possible.  IRIS is keen to collaborate with members of the Arctic science community during the development and implementation of USArray in Alaska.

Additional Resources

Publications related to the Transportable Array in Alaska, including development plans and regional fact sheets, are available online here.

Staff

The collection of high-quality, telemetered data in remote regions of Alaska is a daunting task only made possible through the collaboration and hard work of many individuals. A list of the staff at the Anchorage Operations Center can be found here.

Contacts

Robert Woodward, President, 1-202-682-2220

Bob Busby, Transportable Array Manager, 1-800-504-0357

Further Reading

Busby, R. W., and K. Aderhold (2020), The Alaska Transportable Array: As Built, Seismological Research Letters, doi: https://doi.org/10.1785/0220200154.

Alaska TA: Capabilities and Interdisciplinary Instrumentation, Presentation Slides at 2017 AGU Fall Meeting

Benefits of Enhanced Earthquake Monitoring and Potential Earthquake Early Warning - A Stakeholder Survey (2016), Alaska Seismic Hazards Safety Commission

USArray-Alaska Extension into Northwestern Canada Workshop Report (2013)

Autonomous Polar Observing Systems Workshop Report (2011)

Opportunities for EarthScope Science in Alaska in Anticipation of USArray Report (2011)

Plafker, G. and Berg, H.C. (1994) An overview of the geology and tectonic evolution of Alaska, in Plafker, G. and Berg, H.C. (Eds.), The geology of Alaska: Boulder, Colorado, Geol. Soc. of Am., The Geology of North America, v. G1, p. 989-1021.

Freymueller, J.T., P.J. Haeussler, R.L. Wesson, and G. Ekstrom (Eds.) (2008), Active Tectonics and Seismic Potential of Alaska, Geophys. Monogr. Ser., vol. 179, 431 pp., doi:10.1029/GM179, AGU, Washington, D. C.

Wilson, F.H., Hults, C.P., Mull, C.G, and Karl, S.M, comps. (2015) Geologic map of Alaska: U.S. Geological Survey Scientific Investigations Map 3340, pamphlet 196 p., 2 sheets, scale 1:1,584,000.

 

Alaska TA equipment installed at the Knik Glacier Alaska Earthquake Center station (5/12/2015)