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Heritage

More than a decade of Waves In Ice deployments, from the 2012 NIWA array and the 2014 Nature paper to the KOPRI fleet of 2024. The stories, the public data and the open source are on the WII5 site.
Six buoys labelled and lined up before going into the ice on a NIWA deployment.

Six buoys labelled and lined up before going into the ice on a NIWA deployment.

WII6 is the sixth design in a line that started in 2012. Earlier instruments used a Kistler single-axis accelerometer with a lower-cost inertial measurement unit (IMU). The Sparton motion sensor used in multiple WII5 deployments remains an option for WII6. The wave maths builds on the work across those generations.

Deployments

Year Deployment History
2012 NIWA, East Antarctica, the SIPEX II voyage: the first array, and the data behind the 2014 Nature paper NIWA 2012
2014 Scott Base testing Scott Base 2014
2016 Internal test deployment, and the first WII3 builds WII3 testing
2016 Japan Japan 2016
2016 NIWA test NIWA testing
2017 NIWA, Ross Sea, the PIPERS voyage: fourteen buoys through autumn ice growth PIPERS 2017
2017 NYU Abu Dhabi NYU 2017
2018 Japan Japan 2018
2018 University of Melbourne Melbourne 2018
2019 to 2022 Tasmania, the WII5 generation at sea Tasmania 2019 to 2022
2019 to 2021 TWK5, Canada Canada 2019 to 2021
2024 Korea Polar Research Institute, ten deployed buoys KOPRI 2024

The scientific figure in the gallery is Extended Data Figure 3 from Kohout et al. (2014), Storm-induced sea-ice breakup and the implications for ice extent. It compares wave power spectra during a storm-generated wave event and calm seas, at different distances from the ice edge.

On the WII5 site

The previous site remains the record of the earlier generations and stays online:

The science

The wave-motion mathematics and the field programmes were led by Dr Alison Kohout of NIWA. Her project pages cover the sensor design, data collection on each voyage, the analysis, and the publications: Waves in Ice.