| Summary: | Analyses of the Western Canadian Arctic coastline have revealed substantial increases (up to 110%) in coastal erosion over the last two decades, following a sustained period of relatively consistent retreat since the first aerial surveys in the 1950s. Arctic permafrost cliffs comprise over 34% of the Earth’s coastlines, yet understanding of the sensitivities and impacts of accelerating coastal erosion in these regions remains extremely limited. Accelerated rates of retreat have been accompanied by higher frequencies and magnitudes of collapse, threatening coastal communities, nearshore and back barrier ecosystems, and critical infrastructure across the Arctic. The NERC (Natural Environment Research Council) UK-Canada bursary program has enabled the addition of UK expertise to enhance and complement a wider comprehensive assessment of the state of the Beaufort Sea coast, currently being undertaken by Natural Resources Canada. The bursary support has facilitated the development of new ideas that combine in-depth local knowledge and long-term datasets developed by Natural Resources Canada, with novel approaches to detail the thermodynamic behaviour and thaw processes at key sites. Multi-platform and multi-resolution survey approaches have been combined with novel in situ monitoring and targeted geochemical sampling to add new dimensions to the understanding of permafrost cliff erosion processes and their impact within the coastal zone. Here we present a summary of the NERC UK-Canada Bursary funded research into the drivers, responses, and wider impacts of permafrost coast erosion. It is important to set the long-term erosion trends in context and re-evaluate previous rates and inferences of the resultant contribution of material into the coastal zone. Peninsula Point within the Pingo Canadian Landmark (~10 km west of Tuktoyaktuk) proved to be an excellent study site with clear and variable exposures of massive ground ice. We set the long-term erosion trends in context with photogrammetric analysis of historic ...
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