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dc.contributor.authorBever, Aaron J.  Concept link
dc.contributor.authorFriedrichs, Marjorie A. M.  Concept link
dc.contributor.authorFriedrichs, Carl T.  Concept link
dc.contributor.authorScully, Malcolm E.  Concept link
dc.date.accessioned2018-11-01T17:58:42Z
dc.date.available2018-11-01T17:58:42Z
dc.date.issued2018-09-12
dc.identifier.citationJournal of Geophysical Research: Oceans 123 (2018): 6392-6407en_US
dc.identifier.urihttps://hdl.handle.net/1912/10682
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 Journal of Geophysical Research: Oceans 123 (2018): 6392-6407, doi:10.1029/2018JC014129.en_US
dc.description.abstractLow levels of dissolved oxygen (DO) occur in many embayments throughout the world and have numerous detrimental effects on biota. Although measurement of in situ DO is straightforward with modern instrumentation, quantifying the volume of water in a given embayment that is hypoxic (hypoxic volume (HV)) is a more difficult task; however, this information is critical for determining whether management efforts to increase DO are having an overall impact. This paper uses output from a three‐dimensional numerical model to demonstrate that HV in Chesapeake Bay can be estimated well with as few as two vertical profiles. In addition, the cumulative hypoxic volume (HVC; the total amount of hypoxia in a given year) can be calculated with relatively low uncertainty (<10%) if continuous DO data are available from two strategically positioned vertical profiles. This is because HV in the Chesapeake Bay is strongly constrained by the geometry of the embayment. A simple Geometric HV calculation method is presented and numerical model results are used to illustrate that for calculating HVC, the results using two daily‐averaged profiles are typically more accurate than those of the standard method that interpolates bimonthly cruise data. Bimonthly data produce less accurate estimates of HVC because high‐frequency changes in oxygen concentration, for example, due to regional‐weather‐ or storm‐induced changes in wind direction and magnitude, are not resolved. The advantages of supplementing cruise‐based sampling with continuous vertical profiles to estimate HVC should be applicable to other systems where hypoxic water is constrained to a specific area by bathymetry.en_US
dc.description.sponsorshipNOAA Grant Number: NA13NOS0120139en_US
dc.language.isoen_USen_US
dc.publisherJohn Wiley & Sonsen_US
dc.relation.urihttps://doi.org/10.1029/2018JC014129
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectChesapeake Bayen_US
dc.subjectOxygenen_US
dc.subjectDead zoneen_US
dc.subjectHypoxiaen_US
dc.subjectObserving systemsen_US
dc.subjectEstuaryen_US
dc.titleEstimating hypoxic volume in the Chesapeake Bay using two continuously sampled oxygen profilesen_US
dc.typeArticleen_US
dc.identifier.doi10.1029/2018JC014129


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