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  • 1
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    PANGAEA
    In:  Supplement to: Fay, Amanda R; McKinley, Galen A (2014): Global open-ocean biomes: mean and temporal variability. Earth System Science Data, 6(2), 273-284, https://doi.org/10.5194/essd-6-273-2014
    Publication Date: 2023-01-13
    Description: Large-scale studies of ocean biogeochemistry and carbon cycling have often partitioned the ocean into regions along lines of latitude and longitude despite the fact that spatially more complex boundaries would be closer to the true biogeography of the ocean. Herein, we define 17 open-ocean biomes classified from four observational data sets: sea surface temperature (SST), spring/summer chlorophyll a concentrations (Chl a), ice fraction, and maximum mixed layer depth (maxMLD) on a 1° × 1° grid. By considering interannual variability for each input, we create dynamic ocean biome boundaries that shift annually between 1998 and 2010. Additionally we create a core biome map, which includes only the grid cells that do not change biome assignment across the 13 years of the time-varying biomes. These biomes can be used in future studies to distinguish large-scale ocean regions based on biogeochemical function.
    Type: Dataset
    Format: application/x-netcdf, 7.4 MBytes
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  • 2
    Publication Date: 2021-03-31
    Description: By means of a variety of international observing and modeling efforts, the ocean carbon community has developed several independent estimates for ocean carbon uptake. In this presentation, we report on the synthesis effort we are undertaking under the auspices of an Ocean Carbon and Biogeochemistry Working Group. Our initial goal for this working group is to determine the best estimate for the net and anthropogenic carbon sink from 1994-2007, and then to infer the total magnitude of the poorly quantified fluxes that constitute their difference. Estimates for the net, or contemporary, ocean carbon uptake are derived from surface ocean pCO2 data interpolated to global coverage. From 4 of these products, we find Fnet = -1.7 PgC/yr for 1994-2007. Estimates for uptake of anthropogenic carbon comes from (1) interior observations of dissolved inorganic carbon and other tracers, (2) an ocean model constrained with observations, and (3) a suite of nine free-running ocean hindcast models in which the natural carbon cycle is assumed to be in a long-term steady state. Fant = -2.3 PgC/yr from the mean of these approaches. The difference between these two estimates is -0.6 PgC/yr, and acts as a quantitative constraint on the sum of the additional fluxes. As coastal zones and the Arctic are additional net carbon sinks, the sum of outgassed river-derived carbon, skin temperature effects on air-sea CO2 exchange, and non-steady state natural carbon fluxes in the open ocean can be no larger than a few tenths of PgC/yr. Our presentation details the uncertainties and assumptions made in deriving these estimates, and suggests paths forward to further reduce uncertainties.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 3
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2015-01-13
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
    Format: application/x-netcdf
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    Format: application/rtf
    Format: application/x-netcdf
    Format: video/quicktime
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