EGU2020-11411, updated on 12 Jun 2020
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Improving tsunami forecast with data assimilation on dense pressure gauge arrays: the 2009 Dusky Sound, New Zealand, tsunami

Aditya Gusman1, Anne Sheehan2, and Kenji Satake3
Aditya Gusman et al.
  • 1GNS Science, Earth Structure and Processes, New Zealand (
  • 2Department of Geological Sciences, University of Colorado Boulder, Boulder, United States (
  • 3Earthquake Research Institute, The University of Tokyo, Tokyo, Japan (

Tsunami warnings in New Zealand rely on first locating and determining size of a large earthquake and then using precomputed simulation results to forecast the threat level and timing of the resulting tsunami. The number of offshore pressure gauges for tsunami monitoring around the world is increasing and it provides the opportunity to develope new methods to forecast tsunamis. In cases where a dense array of offshore pressure gauges is available, a data assimilation method can be applied to estimate the tsunami using the observations of pressure changes. Here we apply the data assimilation method to the tsunami generated from the 2009 Dusky Sound, New Zealand, magnitude 7.8 earthquake and determine a rapid and accurate estimate of the tsunami wave arrival time and size along the west coast of New Zealand.  The tsunami was recorded by the Marine Observations of Anisotropy near Aotearoa (MOANA) OBS network which consists of a total of 30 differential pressure gauges.

We use tsunami waveform inversion applied to Deep‐ocean Assessment and Reporting of Tsunamis (DART) offshore pressure gauge and coastal tide gauge data to estimate the fault slip distribution of the Dusky Sound earthquake. The tsunami from this fault slip estimate is then used as a reference to measure the forecast accuracy from different methods to forecast the tsunami threat in New Zealand’s tsunami warning zones. Methods that are evaluated here include the currently operational tsunami warning procedure in New Zealand, tsunami data assimilation that relies only on the dense pressure gauge array data, and tsunami data assimilation with an initial condition model from W-Phase inversion result.

A good match was found between the forecast from the data assimilation method and observed tsunami waveforms at the Charleston tide gauge station on the west coast of New Zealand's South Island. However, this method gives an accurate forecast only along the west coast of New Zealand because the offshore pressure gauge network is located off the west coast of the South Island. While an advantage of the data assimilation is that no initial condition is needed, we find that our forecast is improved especially along the south and east coasts of the South Island by merging tsunami forward modelling from a rapid W‐phase earthquake source solution with the data assimilation method.

How to cite: Gusman, A., Sheehan, A., and Satake, K.: Improving tsunami forecast with data assimilation on dense pressure gauge arrays: the 2009 Dusky Sound, New Zealand, tsunami, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11411,, 2020

Comments on the presentation

AC: Author Comment | CC: Community Comment | Report abuse

Presentation version 1 – uploaded on 05 May 2020
  • CC1: Comment on EGU2020-11411, Rachel Hunt, 06 May 2020

    Thank you so much for sharing your work Aditya, Anne, and Kenji. You mentioned in your paper that studies like these are important for testing and further developing rapid and accurate tsunami warning systems. Could research like this also be useful in educating the New Zealand public about the tsunami risks they face and how best to respond when they receive a tsunami warning?

    Rachel Hunt, PhD Student, UCL

    • AC1: Reply to CC1, Anne Sheehan, 07 May 2020

      Hi Rachel, Thanks for your interest! This kind of work could definitely be useful in educating the New Zealand public about tsunami risks  and how best to respond to tsunami warnings. Aditya is at GNS Science in New Zealand and perhaps can comment about ongoing efforts in New Zealand. Anne

    • AC2: Reply to CC1, Aditya Gusman, 07 May 2020

      Hi Rachel,

      Thank you for your question. This particular study could be useful for the public to understand how we (GNS Science) obtain a tsunami threat level map for tsunami warning purposes during an event, and shows that we are exploring other approaches. People are encouraged to evacuate to safe places upon receiving a tsunami warning. To determine the safe places, we at GNS are currently working on making tsunami evacuation zones in coastal communities along the New Zealand coast using tsunami inundation modeling (not presented here). 



  • CC2: Comment on EGU2020-11411, Rachel Hunt, 08 May 2020

    Hi Anne and Aditya, thank you so much for your helpful responses. I am currently designing my PhD project and will hopefully be carrying out fieldwork in New Zealand in the future. I hope to focus on the integration of traditional knowledge and deliver this through a novel communication method to improve the way people respond to tsunami early warnings. However, I am still in the early stages of research design and will have a more fixed idea of the project over the next couple of months. Aditya, your work on determining evacuation zones through tsunami inundation modelling sounds very interesting and I would be keen to hear more about it. Thank you both for your time!

    • AC3: Reply to CC2, Anne Sheehan, 08 May 2020

      Rachel, Good luck with your research! It sounds very valuable. Anne