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  • Carbon flux  (2)
  • BATS-Counts#2271-2277; Carbon fixation rate per chlorophyll; Chlorophyll total; DEPTH, water; Fixation of carbon in chlorophyll; Irradiance; OPPWG_0321; Optical depth; ORFOIS; Origin and Fate of Biogenic Particle Fluxes in the Ocean; Primary production of carbon; Primary production of carbon per area, daily; Sunshine duration, daily  (1)
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  • 1
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    PANGAEA
    Publikationsdatum: 2024-03-09
    Schlagwort(e): BATS-Counts#2271-2277; Carbon fixation rate per chlorophyll; Chlorophyll total; DEPTH, water; Fixation of carbon in chlorophyll; Irradiance; OPPWG_0321; Optical depth; ORFOIS; Origin and Fate of Biogenic Particle Fluxes in the Ocean; Primary production of carbon; Primary production of carbon per area, daily; Sunshine duration, daily
    Materialart: Dataset
    Format: text/tab-separated-values, 34 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2022-05-25
    Beschreibung: Author Posting. © American Geophysical Union, 2018. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Global Biogeochemical Cycles 32 (2018): 1312-1328, doi:10.1029/2018GB005934.
    Beschreibung: Ocean biological processes mediate the transport of roughly 10 petagrams of carbon from the surface to the deep ocean each year and thus play an important role in the global carbon cycle. Even so, the globally integrated rate of carbon export out of the surface ocean remains highly uncertain. Quantifying the processes underlying this biological carbon export requires a synthesis between model predictions and available observations of particulate organic carbon (POC) flux; yet the scale dissimilarities between models and observations make this synthesis difficult. Here we compare carbon export predictions from a mechanistic model with observations of POC fluxes from several data sets compiled from the literature spanning different space, time, and depth scales as well as using different observational methodologies. We optimize model parameters to provide the best match between model‐predicted and observed POC fluxes, explicitly accounting for sources of error associated with each data set. Model‐predicted globally integrated values of POC flux at the base of the euphotic layer range from 3.8 to 5.5 Pg C/year, depending on the data set used to optimize the model. Modeled carbon export pathways also vary depending on the data set used to optimize the model, as well as the satellite net primary production data product used to drive the model. These findings highlight the importance of collecting field data that average over the substantial natural temporal and spatial variability in carbon export fluxes, and advancing satellite algorithms for ocean net primary production, in order to improve predictions of biological carbon export.
    Beschreibung: NASA Ocean Biology and Biogeochemistry Program Grant Numbers: NNX16AR49G, NNXA122G, NNX16AR47G, OBB16_2‐0031; National Science Foundation
    Beschreibung: 2019-03-13
    Schlagwort(e): Carbon flux ; Remote sensing ; Carbon cycle ; Mechanistic model ; Optimization
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Publikationsdatum: 2017-01-04
    Beschreibung: Citation only. Published in Science 316: 567-570, doi: 10.1126/science.1137959
    Beschreibung: Funding was obtained primarily through the NSF, Ocean Sciences Programs in Chemical and Biological Oceanography, with additional support from the U.S. Department of Energy, Office of Science, Biological and Environmental Research Program, and other national programs, including the Australian Cooperative Research Centre program and Australian Antarctic Division.
    Schlagwort(e): Carbon flux ; Carbon sequestration ; Biological pump
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Standort Signatur Erwartet Verfügbarkeit
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