{"database":"biostudies-literature","file_versions":[],"scores":null,"additional":{"submitter":["Spiro Jaeger G"],"funding":["Indian Ministry of Earth Science","Office of Naval Research"],"pagination":["e1701504"],"full_dataset_link":["https://www.ebi.ac.uk/biostudies/studies/S-EPMC5834007"],"repository":["biostudies-literature"],"omics_type":["Unknown"],"volume":["4(2)"],"pubmed_abstract":["Salinity, rather than temperature, is the leading influence on density in some regions of the world's upper oceans. In the Bay of Bengal, heavy monsoonal rains and runoff generate strong salinity gradients that define density fronts and stratification in the upper ~50 m. Ship-based observations made in winter reveal that fronts exist over a wide range of length scales, but at O(1)-km scales, horizontal salinity gradients are compensated by temperature to alleviate about half the cross-front density gradient. Using a process study ocean model, we show that scale-selective compensation occurs because of surface cooling. Submesoscale instabilities cause density fronts to slump, enhancing stratification along-front. Specifically for salinity fronts, the surface mixed layer (SML) shoals on the "],"journal":["Science advances"],"pubmed_title":["Submesoscale-selective compensation of fronts in a salinity-stratified ocean."],"pmcid":["PMC5834007"],"funding_grant_id":["N000141612470, N000141310451"],"pubmed_authors":["Mahadevan A","Spiro Jaeger G"],"additional_accession":[]},"is_claimable":false,"name":"Submesoscale-selective compensation of fronts in a salinity-stratified ocean.","description":"Salinity, rather than temperature, is the leading influence on density in some regions of the world's upper oceans. In the Bay of Bengal, heavy monsoonal rains and runoff generate strong salinity gradients that define density fronts and stratification in the upper ~50 m. Ship-based observations made in winter reveal that fronts exist over a wide range of length scales, but at O(1)-km scales, horizontal salinity gradients are compensated by temperature to alleviate about half the cross-front density gradient. Using a process study ocean model, we show that scale-selective compensation occurs because of surface cooling. Submesoscale instabilities cause density fronts to slump, enhancing stratification along-front. Specifically for salinity fronts, the surface mixed layer (SML) shoals on the ","dates":{"release":"2018-01-01T00:00:00Z","publication":"2018 Feb","modification":"2025-04-19T15:19:29.779Z","creation":"2019-03-26T23:05:52Z"},"accession":"S-EPMC5834007","cross_references":{"pubmed":["29507874"],"doi":["10.1126/sciadv.1701504"]}}