Abstract
Oceanographic processes at coastal scales require much higher horizontal resolution from both ocean models and
observations as compared to deep water oceanography. Aside from a few exceptions such as land-locked seas, the
hydrodynamics of coastal shallow waters is strongly influenced by the tides, which in turn control the mixing,
formation of temperature fronts and other phenomena.
Original language | English |
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Publication status | Published - Apr 2017 |
Event | EGU General Assembly - European Geosciences Union General Assembly, 23–28 April 2017, Vienna, Austria Duration: 23 Apr 2017 → 28 Apr 2017 |
Conference
Conference | EGU General Assembly |
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Period | 23/04/17 → 28/04/17 |