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  • Carbon cycle  (2)
  • 18DD20140819; 18DD20140819_P12; 18DD20140819_P16; 18DD20140819_P20; 18DD20140819_P26; 18DD20140819_P4; 18DD20150608; 18DD20150608_P12; 18DD20150608_P16; 18DD20150608_P20; 18DD20150608_P26; 18DD20150608_P4; 18DD20150818; 18DD20150818_P12; 18DD20150818_P16; 18DD20150818_P20; 18DD20150818_P26; 18DD20150818_P4; 18DD20160525; 18DD20160525_AT01; 18DD20160525_LC12; 18DD20160525_LD6.5; 18DD20160605; 18DD20160605_P12; 18DD20160605_P16; 18DD20160605_P20; 18DD20160605_P26; 18DD20160605_P4; 18DD20160816; 18DD20160816_P12; 18DD20160816_P16; 18DD20160816_P20; 18DD20160816_P26; 18DD20160816_P4; 18DD20170604; 18DD20170604_P12; 18DD20170604_P16; 18DD20170604_P20; 18DD20170604_P26; 18DD20170604_P4; Ammonium; Bottle number; Campaign; Carbon, inorganic, dissolved; Carbon, particulate; carbon export; Chlorophyll a; Date/time end; Date/Time of event; Date/time start; Density, sigma-theta (0); DEPTH, water; Event label; Gross primary production of carbon; Identification; John P. Tully; Latitude of event; Light intensity; Line P; Longitude of event; Mixed layer depth; MULT; Multiple investigations; Nitrate; Nitrogen, particulate; Northeast Pacific; Oxygen; Phosphate; Pressure, water; primary production; Primary production of carbon; Salinity; Silicate; Temperature, water; Temperature, water, potential; δ13C isotopic abundance; δ15N isotopic abundance; δ18O, gas  (1)
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  • 1
    Publication Date: 2023-07-19
    Keywords: 18DD20140819; 18DD20140819_P12; 18DD20140819_P16; 18DD20140819_P20; 18DD20140819_P26; 18DD20140819_P4; 18DD20150608; 18DD20150608_P12; 18DD20150608_P16; 18DD20150608_P20; 18DD20150608_P26; 18DD20150608_P4; 18DD20150818; 18DD20150818_P12; 18DD20150818_P16; 18DD20150818_P20; 18DD20150818_P26; 18DD20150818_P4; 18DD20160525; 18DD20160525_AT01; 18DD20160525_LC12; 18DD20160525_LD6.5; 18DD20160605; 18DD20160605_P12; 18DD20160605_P16; 18DD20160605_P20; 18DD20160605_P26; 18DD20160605_P4; 18DD20160816; 18DD20160816_P12; 18DD20160816_P16; 18DD20160816_P20; 18DD20160816_P26; 18DD20160816_P4; 18DD20170604; 18DD20170604_P12; 18DD20170604_P16; 18DD20170604_P20; 18DD20170604_P26; 18DD20170604_P4; Ammonium; Bottle number; Campaign; Carbon, inorganic, dissolved; Carbon, particulate; carbon export; Chlorophyll a; Date/time end; Date/Time of event; Date/time start; Density, sigma-theta (0); DEPTH, water; Event label; Gross primary production of carbon; Identification; John P. Tully; Latitude of event; Light intensity; Line P; Longitude of event; Mixed layer depth; MULT; Multiple investigations; Nitrate; Nitrogen, particulate; Northeast Pacific; Oxygen; Phosphate; Pressure, water; primary production; Primary production of carbon; Salinity; Silicate; Temperature, water; Temperature, water, potential; δ13C isotopic abundance; δ15N isotopic abundance; δ18O, gas
    Type: Dataset
    Format: text/tab-separated-values, 7326 data points
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2010. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 115 (2010): C11015, doi:10.1029/2010JC006152.
    Description: The concentration of inert gases and their isotopes in the deep ocean are useful as tracers of air-sea gas exchange during deepwater formation. ΔKr/Ar, ΔN2/Ar, and δ40Ar were measured in deep profiles of samples collected in the northwest Pacific, subtropical North Pacific and tropical Atlantic oceans. For the ocean below 2000 m, we determined a mean ΔKr/Ar composition of −0.96% ± 0.16%, a mean ΔN2/Ar of 1.29% ± 0.21% relative to equilibrium saturation, and for δ40Ar a value of 1.188‰ ± 0.055‰ relative to air. These data are used to constrain high-latitude ventilation processes in the framework of three-box and seven-box ocean models. For the three-box model tracer data, we constrain the appropriate surface area of the high-latitude region in both models to be 3.6% (+2.5%, −1.7%) of ocean surface area and the bubble air injection rate to be 22.7 (+8.8, −7.3) mol air m−2 yr−1. Results for the seven-box model were similar, with a high-latitude area of 3.3% (+2.2%, −1.3%). Our results provide geochemical support for suggestions that the effective area of high-latitude ventilation is much smaller than the region of elevated preformed nutrients and demonstrate that noble gases strongly constrain the ocean solubility pump. Reducing high-latitude surface area weakens the CO2 solubility pump in the box models and limits communication between the atmosphere and deep ocean. These tracers should be useful constraints on high-latitude ventilation and the strength of the solubility pump in more complex ocean general circulation models.
    Description: Funding was provided by NSF‐OCE‐0647979.
    Keywords: Noble gases ; Ventilation ; Carbon cycle ; Solubility pump ; Gas exchange
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 3
    Publication Date: 2022-05-27
    Description: © The Author(s), 2021. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Siegel, D. A., Cetinic, I., Graff, J. R., Lee, C. M., Nelson, N., Perry, M. J., Ramos, I. S., Steinberg, D. K., Buesseler, K., Hamme, R., Fassbender, A. J., Nicholson, D., Omand, M. M., Robert, M., Thompson, A., Amaral, V., Behrenfeld, M., Benitez-Nelson, C., Bisson, K., Boss, E., Boyd, P. W., Brzezinski, M., Buck, K., Burd, A., Burns, S., Caprara, S., Carlson, C., Cassar, N., Close, H. H., D’Asaro, E., Durkin, C., Erickson, Z., Estapa, M. L., Fields, E., Fox, J., Freeman, S., Gifford, S., Gong, W., Gray, D., Guidi, L., Haëntjens, N., Halsey, K., Huot, Y., Hansell, D., Jenkins, B., Karp-Boss, L., Kramer, S., Lam, P., Lee, J-M., Maas, A., Marchal, O., Marchetti, A., McDonnell, A., McNair, H., Menden-Deuer, S., Morison, F., Niebergall, A. K., Passow, U., Popp, B., Potvin, G., Resplandy, L., Roca-Martí, M., Roesler, C., Rynearson, T., Traylor, S., Santoro, A., Seraphin, K. D., Sosik, H. M., Stamieszkin, K., Stephens, B., Tang, W., Van Mooy, B., Xiong, Y., Zhang, X. An operational overview of the EXport Processes in the Ocean from RemoTe Sensing (EXPORTS) Northeast Pacific field deployment. Elementa: Science of the Anthropocene, 9(1), (2021): 1, https://doi.org/10.1525/elementa.2020.00107.
    Description: The goal of the EXport Processes in the Ocean from RemoTe Sensing (EXPORTS) field campaign is to develop a predictive understanding of the export, fate, and carbon cycle impacts of global ocean net primary production. To accomplish this goal, observations of export flux pathways, plankton community composition, food web processes, and optical, physical, and biogeochemical (BGC) properties are needed over a range of ecosystem states. Here we introduce the first EXPORTS field deployment to Ocean Station Papa in the Northeast Pacific Ocean during summer of 2018, providing context for other papers in this special collection. The experiment was conducted with two ships: a Process Ship, focused on ecological rates, BGC fluxes, temporal changes in food web, and BGC and optical properties, that followed an instrumented Lagrangian float; and a Survey Ship that sampled BGC and optical properties in spatial patterns around the Process Ship. An array of autonomous underwater assets provided measurements over a range of spatial and temporal scales, and partnering programs and remote sensing observations provided additional observational context. The oceanographic setting was typical of late-summer conditions at Ocean Station Papa: a shallow mixed layer, strong vertical and weak horizontal gradients in hydrographic properties, sluggish sub-inertial currents, elevated macronutrient concentrations and low phytoplankton abundances. Although nutrient concentrations were consistent with previous observations, mixed layer chlorophyll was lower than typically observed, resulting in a deeper euphotic zone. Analyses of surface layer temperature and salinity found three distinct surface water types, allowing for diagnosis of whether observed changes were spatial or temporal. The 2018 EXPORTS field deployment is among the most comprehensive biological pump studies ever conducted. A second deployment to the North Atlantic Ocean occurred in spring 2021, which will be followed by focused work on data synthesis and modeling using the entire EXPORTS data set.
    Description: DAS, NN, KB, EF, SK, AB, AM, UP: NASA 80NSSC17K0692. MJB, EB, JG, LG, KH, LKB, JF, NH: NASA 80NSSC17K0568. KB, CBN, LR, MRM: NASA 80NSSC17K0555. CC, DH, BS: NASA 80NSSC18K0437. HC: NSF 1830016. BP, KDS: NSF 1829425. ME, KB, CD, MO: NASA 80NSSC17K0662. AF: NSF 1756932. BJ, KB, MB, SB, SC: NSF 1756442. PH, OM, JML: NSF 1829614. CL, ED, DN, MO, MJP, AT, ZN, ST: NASA 80NSSC17K0663. AM, NC, SG, WT, AN, WG: NASA 80NSSC17K0552. SMD, TR, HM, FM: NASA 80NSSC17K0716. CR, HS: NASA 80NSSC17K0700. AS, PB: NASA 80NSSC18K1431. DS, AM, KS NASA 80NSSC17K0654. BVM: NSF 1756254. XZ, DG, LG, YH: NASA 80NSSC17K0656 and 80NSSC20K0350.
    Keywords: Biological pump ; NASA field campaign ; NPP fates ; Carbon cycle ; Organic carbon export ; Export pathways
    Repository Name: Woods Hole Open Access Server
    Type: Article
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