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dc.contributor.authorNicholson, David P.  Concept link
dc.contributor.authorWilson, Samuel T.  Concept link
dc.contributor.authorDoney, Scott C.  Concept link
dc.contributor.authorKarl, David M.  Concept link
dc.date.accessioned2015-07-31T16:40:35Z
dc.date.available2015-07-31T16:40:35Z
dc.date.issued2015-05-22
dc.identifier.citationGeophysical Research Letters 42 (2015): 4032–4039en_US
dc.identifier.urihttps://hdl.handle.net/1912/7435
dc.description© The Author(s), 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Geophysical Research Letters 42 (2015): 4032–4039, doi:10.1002/2015GL063065.en_US
dc.description.abstractUsing autonomous underwater gliders, we quantified diurnal periodicity in dissolved oxygen, chlorophyll, and temperature in the subtropical North Pacific near the Hawaii Ocean Time-series (HOT) Station ALOHA during summer 2012. Oxygen optodes provided sufficient stability and precision to quantify diel cycles of average amplitude of 0.6 µmol kg−1. A theoretical diel curve was fit to daily observations to infer an average mixed layer gross primary productivity (GPP) of 1.8 mmol O2 m−3 d−1. Cumulative net community production (NCP) over 110 days was 500 mmol O2 m−2 for the mixed layer, which averaged 57 m in depth. Both GPP and NCP estimates indicated a significant period of below-average productivity at Station ALOHA in 2012, an observation confirmed by 14C productivity incubations and O2/Ar ratios. Given our success in an oligotrophic gyre where biological signals are small, our diel GPP approach holds promise for remote characterization of productivity across the spectrum of marine environments.en_US
dc.description.sponsorshipThe authors acknowledge support from the National Science Foundation (NSF) through an NSF Science and Technology Center, the Center for Microbial Oceanography Research and Education (C-MORE; NSF EF-0424599). D.N. also was supported by NSF (OCE-1129644) and an Independent Study Award from the Woods Hole Oceanographic Institution (WHOI). D.M.K. was also supported by the Gordon and Betty Moore Foundation. WHOI Summer Student Fellow Cole Stites-Clayton, Stanford University, contributed to early stages of Seaglider data analysis and was supported by an NSF REU grant to WHOI (OCE-1156952).en_US
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen_US
dc.publisherJohn Wiley & Sonsen_US
dc.relation.urihttps://doi.org/10.1002/2015GL063065
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subjectPrimary productivityen_US
dc.subjectGlideren_US
dc.subjectDielen_US
dc.subjectOxygenen_US
dc.subjectNet community productionen_US
dc.subjectHawaiien_US
dc.titleQuantifying subtropical North Pacific gyre mixed layer primary productivity from Seaglider observations of diel oxygen cyclesen_US
dc.typeArticleen_US
dc.identifier.doi10.1002/2015GL063065


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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