Show simple item record

dc.contributor.authorBianucci, Laura  Concept link
dc.contributor.authorBalaguru, Karthik  Concept link
dc.contributor.authorSmith, Richard W.  Concept link
dc.contributor.authorLeung, L. Ruby  Concept link
dc.contributor.authorMoriarty, Julia M.  Concept link
dc.date.accessioned2018-11-08T19:46:30Z
dc.date.available2018-11-08T19:46:30Z
dc.date.issued2018-10-24
dc.identifier.citationScientific Reports 8 (2018): 15740en_US
dc.identifier.urihttps://hdl.handle.net/1912/10700
dc.description© The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Scientific Reports 8 (2018): 15740, doi:10.1038/s41598-018-33640-3.en_US
dc.description.abstractHurricanes passing over the ocean can mix the water column down to great depths and resuspend massive volumes of sediments on the continental shelves. Consequently, organic carbon and reduced inorganic compounds associated with these sediments can be resuspended from anaerobic portions of the seabed and re-exposed to dissolved oxygen (DO) in the water column. This process can drive DO consumption as sediments become oxidized. Previous studies have investigated the effect of hurricanes on DO in different coastal regions of the world, highlighting the alleviation of hypoxic conditions by extreme winds, which drive vertical mixing and re-aeration of the water column. However, the effect of hurricane-induced resuspended sediments on DO has been neglected. Here, using a diverse suite of datasets for the northern Gulf of Mexico, we find that in the few days after a hurricane passage, decomposition of resuspended shelf sediments consumes up to a fifth of the DO added to the bottom of the water column during vertical mixing. Despite uncertainty in this value, we highlight the potential significance of this mechanism for DO dynamics. Overall, sediment resuspension likely occurs over all continental shelves affected by tropical cyclones, potentially impacting global cycles of marine DO and carbon.en_US
dc.description.sponsorshipSupport for J. Moriarty was provided by the USGS Mendenhall Program.en_US
dc.language.isoen_USen_US
dc.publisherNature Publishing Groupen_US
dc.relation.urihttps://doi.org/10.1038/s41598-018-33640-3
dc.rightsAttribution 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.titleContribution of hurricane-induced sediment resuspension to coastal oxygen dynamicsen_US
dc.typeArticleen_US
dc.identifier.doi10.1038/s41598-018-33640-3


Files in this item

Thumbnail
Thumbnail
Thumbnail

This item appears in the following Collection(s)

Show simple item record

Attribution 4.0 International
Except where otherwise noted, this item's license is described as Attribution 4.0 International