Abstract
This study provides an integrated analysis of exchanges of water, salt and heat between the north-western Black
Sea shelf and the deep basin. Three contributing physical mechanisms are quantified, namely: Ekman drift,
transport by mesoscale eddies at the edge of the NW Black Sea shelf and non-local cascading assisted by the rim current and mesoscale eddies.
Original language | English |
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Publication status | Published - Apr 2017 |
Event | EGU General Assembly 2017 - European Geosciences Union General Assembly, 23–28 April 2017, Vienna, Austria Duration: 23 Apr 2017 → 28 Apr 2017 |
Conference
Conference | EGU General Assembly 2017 |
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Period | 23/04/17 → 28/04/17 |