Downward flux of particles in the western Southern Adriatic margin is reported.
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Shallow vs. deep DSW cascading exerts 1st order control on particle flux export.
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Observations and numerical modelling support occasional storm-driven sediment transport.
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A very short transfer time of NAdDW from formation area to cascading sites is documented.
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Near-bottom currents by DSW cascading are compatible with bedform activity in the basin
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