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substantial intensification of the ocean heat transport, highlighting their climatic influence. However, the dynamics of submesoscale flows, and hence their representation in climate models, have not been
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revealed that blowing snow over sea ice can generate fine sea-salt aerosols, which warm the surface by modifying cloud properties. We propose that other impurities deposited in Arctic snow, e.g. black carbon
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al., pre-print). Although their direct sea level contribution is small, they can indicate which trajectory we are on. By modelling these regions under contrasting scenarios and searching for tipping
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communities may have ecosystem level impacts that must be considered as part of sustainable management of the deep ocean, and in light of the new High Seas Treaty. This studentship will ask: how are deep-water
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sediment–water column model we have been developing in Exeter. With a well calibrated and tested sediment/water-column model, we will then perform idealised experiments focused on a range of proposed blue