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Ruby Mckenzie Sheat

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Climate-induced sea-level rise: Implications for archaeological taonga at Te Pokohiwi ō Kupe | Wairau Bar, Aotearoa New Zealand

DOI
10.20507/MAIJournal.2025.14.1.1
Article type
Journal article
Keywords
climate change
coastal flooding
hazard risk
taonga
wāhi tapu
Wairau Bar
Author(s)
Shaun Williams
Peter Meihana
Cyprian Bosserelle
Corey Hebberd
Rebecca Welsh
Jay Hepi
Ruby Mckenzie Sheat
Start page
5
End page
15

Te Pokohiwi o Kupe | Wairau Bar in the Marlborough region is where one of Aotearoa New Zealand’s earliest archaeological heritage sites is located, dating back to the early 1300s. This article describes a baseline study to map the effects of present-day and future sea levels on archaeological heritage land at Te Pokohiwi ō Kupe. Results suggest that approximately 20% of the heritage land is susceptible to a 100-year storm-wave inundation under present climate and sea-level conditions. With 1 m of sea-level rise likely to be reached between 2070 and 2130, approximately 75% of heritage land will be compromised by a 100-year storm inundation event.

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Climate-induced sea-level rise: Implications for archaeological taonga at Te Pokohiwi ō Kupe | Wairau Bar, Aotearoa New Zealand

WHAT’S IN THE KETE? An inventory of Māori-centred resources for disaster preparedness in Aotearoa New Zealand

DOI
10.20507/MAIJournal.2024.13.1.11
Article type
Journal article
Keywords
disaster risk and resilience
disaster preparedness
DRR communication
education tools
Māori-centred
Author(s)
Ruby Mckenzie Sheat
Kristie-Lee Thomas

Māori collectives are drawing from mātauranga and asserting rangatiratanga over disaster preparedness for the wellbeing of their communities. However, long-standing impacts of colonisation have contributed to Māori being disproportionately impacted by disasters, and to a lack of knowledge concerning the existence and availability of Māori-centred disaster risk and resilience (DRR) tools that help whānau prepare. Two key findings were drawn from a desktop literature review and thematic analysis.

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WHAT’S IN THE KETE?
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