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dc.contributor.authorLanerolle, 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.contributor.authorLanerolle, Lyon W. J.  Concept link
dc.date.accessioned2014-01-23T16:14:37Z
dc.date.available2014-01-23T16:14:37Z
dc.date.issued2013-10-03
dc.identifier.citationJournal of Geophysical Research: Oceans 118 (2013): 4924–4944en_US
dc.identifier.urihttps://hdl.handle.net/1912/6381
dc.description© The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Journal of Geophysical Research: Oceans 118 (2013): 4924–4944, doi:10.1002/jgrc.20331.en_US
dc.description.abstractThe overall size of the “dead zone” within the main stem of the Chesapeake Bay and its tidal tributaries is quantified by the hypoxic volume (HV), the volume of water with dissolved oxygen (DO) less than 2 mg/L. To improve estimates of HV, DO was subsampled from the output of 3-D model hindcasts at times/locations matching the set of 2004–2005 stations monitored by the Chesapeake Bay Program. The resulting station profiles were interpolated to produce bay-wide estimates of HV in a manner consistent with nonsynoptic, cruise-based estimates. Interpolations of the same stations sampled synoptically, as well as multiple other combinations of station profiles, were examined in order to quantify uncertainties associated with interpolating HV from observed profiles. The potential uncertainty in summer HV estimates resulting from profiles being collected over 2 weeks rather than synoptically averaged ∼5 km3. This is larger than that due to sampling at discrete stations and interpolating/extrapolating to the entire Chesapeake Bay (2.4 km3). As a result, sampling fewer, selected stations over a shorter time period is likely to reduce uncertainties associated with interpolating HV from observed profiles. A function was derived that when applied to a subset of 13 stations, significantly improved estimates of HV. Finally, multiple metrics for quantifying bay-wide hypoxia were examined, and cumulative hypoxic volume was determined to be particularly useful, as a result of its insensitivity to temporal errors and climate change. A final product of this analysis is a nearly three-decade time series of improved estimates of HV for Chesapeake Bay.en_US
dc.description.sponsorshipFunding for this study was provided by the IOOS COMT Program through NOAA grants NA10NOS0120063 and NA11NOS0120141. Additional funding was provided by NSF grant OCE-1061564.en_US
dc.format.mimetypeapplication/pdf
dc.format.mimetypeapplication/msword
dc.format.mimetypetext/plain
dc.language.isoen_USen_US
dc.publisherJohn Wiley & Sonsen_US
dc.relation.urihttps://doi.org/10.1002/jgrc.20331
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Unported*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/*
dc.subjectHypoxiaen_US
dc.subjectHypoxic volumeen_US
dc.subjectChesapeake Bayen_US
dc.subjectDead zoneen_US
dc.subjectWater qualityen_US
dc.subjectDissolved oxygenen_US
dc.titleCombining observations and numerical model results to improve estimates of hypoxic volume within the Chesapeake Bay, USAen_US
dc.typeArticleen_US
dc.identifier.doi10.1002/jgrc.20331


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