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  • 2020-2024  (2)
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  • 1
    Publication Date: 2024-02-22
    Description: Formalised knowledge systems, including universities and research institutes, are important for contemporary societies. They are, however, also arguably failing humanity when their impact is measured against the level of progress being made in stimulating the societal changes needed to address challenges like climate change. In this research we used a novel futures-oriented and participatory approach that asked what future envisioned knowledge systems might need to look like and how we might get there. Findings suggest that envisioned future systems will need to be much more collaborative, open, diverse, egalitarian, and able to work with values and systemic issues. They will also need to go beyond producing knowledge about our world to generating wisdom about how to act within it. To get to envisioned systems we will need to rapidly scale methodological innovations, connect innovators, and creatively accelerate learning about working with intractable challenges. We will also need to create new funding schemes, a global knowledge commons, and challenge deeply held assumptions. To genuinely be a creative force in supporting longevity of human and non-human life on our planet, the shift in knowledge systems will probably need to be at the scale of the enlightenment and speed of the scientific and technological revolution accompanying the second World War. This will require bold and strategic action from governments, scientists, civic society and sustained transformational intent.
    Language: English
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 2
    Publication Date: 2023-06-28
    Description: A magnitude 5.6 earthquake occurred under Lake Taupo in New Zealand at 11:47pm (local time) on the 30〈sup〉th〈/sup〉 November 2022. Subsequent to this earthquake evidence of tsunami waves was discovered around the lake shore, and also recorded on three water-level gauges. Surveys were made to record inundation heights and extents around the lake. Interpretation of the collected data suggests that there were at least two tsunami sources: 1) a largely sub-lacustrine landslide occurring in Wharewaka Bay near Taupo township, and 2) a tsunami generated by movement of the lake bed associated with the earthquake. The observed impacts of the landslide-caused tsunami appear to mainly affect an area of the lake within a few hundred metres of the landslide source, while those generated by the co-seismic lake-bed movement are more widely distributed around the lake, particularly on the eastern side. Tsunami observations have been interpreted alongside seismic and geodetic data to better understand the source processes that generated the tsunami waves. Modelling and further work to quantify both tsunami sources are ongoing and latest results will be presented. We will describe the installation of new water-level instruments to better monitor lake water disturbances, e.g., caused by volcanic activities, and discuss the implications of this event for our understanding of the hazard and risk in the Taupo region.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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