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    Rising sea levels and increased storminess are expected to accelerate the erosion of soft-cliff coastlines, threatening coastal infrastructure and livelihoods. To develop predictive models of future coastal change we need fundamentally to know how rapidly coasts have been eroding in the past, and to understand the driving mechanisms of coastal change. Direct observations of cliff retreat rarely extend beyond y, during which humans have significantly modified the coastal system. Cliff retreat rates are unknown in prior centuries and millennia. In this study, we derived retreat rates of chalk cliffs on the south coast of Great Britain over millennial time scales by coupling high-precision cosmogenic radionuclide geochronology and rigorous numerical modeling.
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    Publications - Dr Dylan Rood

    Thank you for visiting nature. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser or turn off compatibility mode in Internet Explorer. In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript. Knowledge about the Holocene evolution of the Greenland ice sheet GrIS is important to put the recent observations of ice loss into a longer-term perspective. In this study, we use six new threshold lake records supplemented with two existing lake records to reconstruct the Holocene ice marginal fluctuations of the Qassimiut lobe QL — one of the most dynamic parts of the GrIS in South Greenland.
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    Holocene ice marginal fluctuations of the Qassimiut lobe in South Greenland

    Mittarfeqarfiit annually purchases goods for millions of kroner, distributed on many different categories. This is for the benefit of not only our colleagues, but also our suppliers. We handle all procurement areas and thereby help to promote our strategy and strengthen our key performance indicators. We work to optimise our cooperation with suppliers and minimise complexity and annual costs.
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