2022
DOI: 10.1175/jpo-d-22-0076.1
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Development of a sea-sediment coupled model incorporating ocean bottom heat flux

Abstract: Previous in-situ observations have suggested that bottom water temperature variations in shelf seas can drive significant ocean bottom heat flux (BHF) by heat conduction. The BHF-driven bottom water temperature variations, however, have been overlooked in ocean general circulation models. In this study, we established a sea-sediment fully coupled model through incorporating the BHF. The coupled model included a sediment temperature module/model, and the BHF was calculated based on the sediment heat content var… Show more

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