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  • 1
    In: Global Biogeochemical Cycles, American Geophysical Union (AGU), Vol. 37, No. 11 ( 2023-11)
    Kurzfassung: The Arctic Ocean is estimated to be a net sink of CO 2 of 116 ± 4 TgC yr −1 in p CO 2 products and 92 ± 30 TgC yr −1 in ocean models The Arctic Ocean CO 2 uptake is explained by a steady‐state natural flux (70%) with atmospheric CO 2 increase (19%) and climate change (11%) The CO 2 uptake increased (31 ± 13 TgC yr −1  dec −1 in products and 10 ± 4 TgC yr −1  dec −1 in models) mostly by decreasing sea ice
    Materialart: Online-Ressource
    ISSN: 0886-6236 , 1944-9224
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 2023
    ZDB Id: 2021601-4
    SSG: 12
    SSG: 13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    In: Global Biogeochemical Cycles, American Geophysical Union (AGU)
    Kurzfassung: The RECCAP2 global ocean analysis provides an authoritative multi‐model and observation‐based assessment of global ocean CO 2 uptake pCO 2 ‐based products yield a mean sea‐air CO 2 flux from 1985‐2018 of ‐1.6±0.2 PgC yr ‐1 with a trend of ‐0.61 PgC yr ‐1 decade ‐1 since 2001 Ocean anthropogenic CO 2 uptake averages ‐2.1‐2.4 PgC yr ‐1 from 1985‐2018, with a trend of ‐0.34‐0.41 PgC yr ‐1 decade ‐1 since 2001
    Materialart: Online-Ressource
    ISSN: 0886-6236 , 1944-9224
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 2023
    ZDB Id: 2021601-4
    SSG: 12
    SSG: 13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    In: Global Biogeochemical Cycles, American Geophysical Union (AGU), Vol. 37, No. 9 ( 2023-09)
    Kurzfassung: p CO 2 seasonal cycle amplitude changes over 1985–2018 are detectable against both mapping uncertainty and natural variability uncertainty The dominant driver of p CO 2 amplitude increases over decadal timescales is attributed to the direct effect of C ant invasion A discrepancy is found with surface dissolved inorganic carbon (DIC) seasonality being systematically less in global ocean biogeochemistry models than in surface DIC observation‐based products
    Materialart: Online-Ressource
    ISSN: 0886-6236 , 1944-9224
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 2023
    ZDB Id: 2021601-4
    SSG: 12
    SSG: 13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    In: Biogeosciences, Copernicus GmbH, Vol. 18, No. 17 ( 2021-09-07), p. 4889-4917
    Kurzfassung: Abstract. Organic matter production by cyanobacteria blooms is a major environmental concern for the Baltic Sea, as it promotes the spread of anoxic zones. Partial pressure of carbon dioxide (pCO2) measurements carried out on Ships of Opportunity (SOOP) since 2003 have proven to be a powerful tool to resolve the carbon dynamics of the blooms in space and time. However, SOOP measurements lack the possibility to directly constrain depth-integrated net community production (NCP) in moles of carbon per surface area due to their restriction to the sea surface. This study tackles the knowledge gap through (1) providing an NCP best guess for an individual cyanobacteria bloom based on repeated profiling measurements of pCO2 and (2) establishing an algorithm to accurately reconstruct depth-integrated NCP from surface pCO2 observations in combination with modelled temperature profiles. Goal (1) was achieved by deploying state-of-the-art sensor technology from a small-scale sailing vessel. The low-cost and flexible platform enabled observations covering an entire bloom event that occurred in July–August 2018 in the Eastern Gotland Sea. For the biogeochemical interpretation, recorded pCO2 profiles were converted to CT*, which is the dissolved inorganic carbon concentration normalised to alkalinity. We found that the investigated bloom event was dominated by Nodularia and had many biogeochemical characteristics in common with blooms in previous years. In particular, it lasted for about 3 weeks, caused a CT* drawdown of 90 µmol kg−1, and was accompanied by a sea surface temperature increase of 10 ∘C. The novel finding of this study is the vertical extension of the CT* drawdown up to the compensation depth located at around 12 m. Integration of the CT* drawdown across this depth and correction for vertical fluxes leads to an NCP best guess of ∼1.2 mol m−2 over the productive period. Addressing goal (2), we combined modelled hydrographical profiles with surface pCO2 observations recorded by SOOP Finnmaid within the study area. Introducing the temperature penetration depth (TPD) as a new parameter to integrate SOOP observations across depth, we achieve an NCP reconstruction that agrees to the best guess within 10 %, which is considerably better than the reconstruction based on a classical mixed-layer depth constraint. Applying the TPD approach to almost 2 decades of surface pCO2 observations available for the Baltic Sea bears the potential to provide new insights into the control and long-term trends of cyanobacteria NCP. This understanding is key for an effective design and monitoring of conservation measures aiming at a Good Environmental Status of the Baltic Sea.
    Materialart: Online-Ressource
    ISSN: 1726-4189
    Sprache: Englisch
    Verlag: Copernicus GmbH
    Publikationsdatum: 2021
    ZDB Id: 2158181-2
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Online-Ressource
    Online-Ressource
    Springer Science and Business Media LLC ; 2023
    In:  Nature Reviews Earth & Environment Vol. 4, No. 2 ( 2023-01-24), p. 119-134
    In: Nature Reviews Earth & Environment, Springer Science and Business Media LLC, Vol. 4, No. 2 ( 2023-01-24), p. 119-134
    Materialart: Online-Ressource
    ISSN: 2662-138X
    Sprache: Englisch
    Verlag: Springer Science and Business Media LLC
    Publikationsdatum: 2023
    ZDB Id: 3005281-6
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    In: Earth System Science Data, Copernicus GmbH, Vol. 16, No. 4 ( 2024-04-30), p. 2047-2072
    Kurzfassung: Abstract. The Global Ocean Data Analysis Project (GLODAP) is a synthesis effort providing regular compilations of surface to bottom ocean biogeochemical bottle data, with an emphasis on seawater inorganic carbon chemistry and related variables determined through chemical analysis of seawater samples. GLODAPv2.2023 is an update of the previous version, GLODAPv2.2022 (Lauvset et al., 2022). The major changes are as follows: data from 23 new cruises were added. In addition, a number of changes were made to the data included in GLODAPv2.2022. GLODAPv2.2023 includes measurements from more than 1.4 million water samples from the global oceans collected on 1108 cruises. The data for the now 13 GLODAP core variables (salinity, oxygen, nitrate, silicate, phosphate, dissolved inorganic carbon, total alkalinity, pH, chlorofluorocarbon-11 (CFC-11), CFC-12, CFC-113, CCl4, and SF6) have undergone extensive quality control with a focus on the systematic evaluation of bias. The data are available in two formats: (i) as submitted by the data originator but converted to World Ocean Circulation Experiment (WOCE) exchange format and (ii) as a merged data product with adjustments applied to minimize bias. For the present annual update, adjustments for the 23 new cruises were derived by comparing those data with the data from the 1085 quality-controlled cruises in the GLODAPv2.2022 data product using crossover analysis. SF6 data from all cruises were evaluated by comparison with CFC-12 data measured on the same cruises. For nutrients and ocean carbon dioxide (CO2), chemistry comparisons to estimates based on empirical algorithms provided additional context for adjustment decisions. The adjustments that we applied are intended to remove potential biases from errors related to measurement, calibration, and data-handling practices without removing known or likely time trends or variations in the variables evaluated. The compiled and adjusted data product is believed to be consistent to better than 0.005 in salinity, 1 % in oxygen, 2 % in nitrate, 2 % in silicate, 2 % in phosphate, 4 µmol kg−1 in dissolved inorganic carbon, 4 µmol kg−1 in total alkalinity, 0.01–0.02 in pH (depending on region), and 5 % in the halogenated transient tracers. The other variables included in the compilation, such as isotopic tracers and discrete CO2 fugacity (fCO2), were not subjected to bias comparison or adjustments. The original data, their documentation, and DOI codes are available at the Ocean Carbon and Acidification Data System of NOAA National Centers for Environmental Information (NCEI), which also provides access to the merged data product. This is provided as a single global file and as four regional ones – the Arctic, Atlantic, Indian, and Pacific oceans – under https://doi.org/10.25921/zyrq-ht66 (Lauvset et al., 2023). These bias-adjusted product files also include significant ancillary and approximated data, which were obtained by interpolation of, or calculation from, measured data. This living data update documents the GLODAPv2.2023 methods and provides a broad overview of the secondary quality control procedures and results.
    Materialart: Online-Ressource
    ISSN: 1866-3516
    Sprache: Englisch
    Verlag: Copernicus GmbH
    Publikationsdatum: 2024
    ZDB Id: 2475469-9
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    In: Annual Review of Earth and Planetary Sciences, Annual Reviews, Vol. 50, No. 1 ( 2022-05-31), p. 593-626
    Kurzfassung: This review examines the current understanding of the global coastal ocean carbon cycle and provides a new quantitative synthesis of air-sea CO 2 exchange. This reanalysis yields an estimate for the globally integrated coastal ocean CO 2 flux of −0.25 ± 0.05 Pg C year −1 , with polar and subpolar regions accounting for most of the CO 2 removal ( 〉 90%). A framework that classifies river-dominated ocean margin (RiOMar) and ocean-dominated margin (OceMar) systems is used to conceptualizecoastal carbon cycle processes. The carbon dynamics in three contrasting case study regions, the Baltic Sea, the Mid-Atlantic Bight, and the South China Sea, are compared in terms of the spatio-temporal variability of surface pCO 2 . Ocean carbon models that range from box models to three-dimensional coupled circulation-biogeochemical models are reviewed in terms of the ability to simulate key processes and project future changes in different continental shelf regions. Common unresolved challenges remain for implementation of these models across RiOMar and OceMar systems. The long-term trends in coastal ocean carbon fluxes for different coastal systems under anthropogenic stress that are emerging in observations and numerical simulations are highlighted. Knowledge gaps in projecting future perturbations associated with before and after net-zero CO 2 emissions in the context of concurrent changes in the land-ocean-atmosphere coupled system pose a key challenge. ▪ A new synthesis yields an estimate for a globally integrated coastal ocean carbon sink of −0.25 Pg C year −1 , with greater than 90% of atmospheric CO 2 removal occurring in polar and subpolar regions. ▪ The sustained coastal and open ocean carbon sink is vital in mitigating climate change and meeting the target set by the Paris Agreement. ▪ Uncertainties in the future coastal ocean carbon cycle are associated with concurrent trends and changes in the land-ocean-atmosphere coupled system. ▪ The major gaps and challenges identified for current coastal ocean carbon research have important implications for climate and sustainability policies.
    Materialart: Online-Ressource
    ISSN: 0084-6597 , 1545-4495
    URL: Issue
    Sprache: Englisch
    Verlag: Annual Reviews
    Publikationsdatum: 2022
    ZDB Id: 124813-3
    ZDB Id: 2010309-8
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    In: Earth System Science Data, Copernicus GmbH, Vol. 14, No. 12 ( 2022-12-16), p. 5543-5572
    Kurzfassung: Abstract. The Global Ocean Data Analysis Project (GLODAP) is a synthesis effort providing regular compilations of surface-to-bottom ocean biogeochemical bottle data, with an emphasis on seawater inorganic carbon chemistry and related variables determined through chemical analysis of seawater samples. GLODAPv2.2022 is an update of the previous version, GLODAPv2.2021 (Lauvset et al., 2021). The major changes are as follows: data from 96 new cruises were added, data coverage was extended until 2021, and for the first time we performed secondary quality control on all sulfur hexafluoride (SF6) data. In addition, a number of changes were made to data included in GLODAPv2.2021. These changes affect specifically the SF6 data, which are now subjected to secondary quality control, and carbon data measured on board the RV Knorr in the Indian Ocean in 1994–1995 which are now adjusted using certified reference material (CRM) measurements made at the time. GLODAPv2.2022 includes measurements from almost 1.4 million water samples from the global oceans collected on 1085 cruises. The data for the now 13 GLODAP core variables (salinity, oxygen, nitrate, silicate, phosphate, dissolved inorganic carbon, total alkalinity, pH, chlorofluorocarbon-11 (CFC-11), CFC-12, CFC-113, CCl4, and SF6) have undergone extensive quality control with a focus on systematic evaluation of bias. The data are available in two formats: (i) as submitted by the data originator but converted to World Ocean Circulation Experiment (WOCE) exchange format and (ii) as a merged data product with adjustments applied to minimize bias. For the present annual update, adjustments for the 96 new cruises were derived by comparing those data with the data from the 989 quality-controlled cruises in the GLODAPv2.2021 data product using crossover analysis. SF6 data from all cruises were evaluated by comparison with CFC-12 data measured on the same cruises. For nutrients and ocean carbon dioxide (CO2) chemistry comparisons to estimates based on empirical algorithms provided additional context for adjustment decisions. The adjustments that we applied are intended to remove potential biases from errors related to measurement, calibration, and data handling practices without removing known or likely time trends or variations in the variables evaluated. The compiled and adjusted data product is believed to be consistent to better than 0.005 in salinity, 1 % in oxygen, 2 % in nitrate, 2 % in silicate, 2 % in phosphate, 4 µmol kg−1 in dissolved inorganic carbon, 4 µmol kg−1 in total alkalinity, 0.01–0.02 in pH (depending on region), and 5 % in the halogenated transient tracers. The other variables included in the compilation, such as isotopic tracers and discrete CO2 fugacity (fCO2), were not subjected to bias comparison or adjustments. The original data, their documentation, and DOI codes are available at the Ocean Carbon and Acidification Data System of NOAA NCEI (https://www.ncei.noaa.gov/access/ocean-carbon-acidification-data-system/oceans/GLODAPv2_2022/, last access: 15 August 2022). This site also provides access to the merged data product, which is provided as a single global file and as four regional ones – the Arctic, Atlantic, Indian, and Pacific oceans – under https://doi.org/10.25921/1f4w-0t92 (Lauvset et al., 2022). These bias-adjusted product files also include significant ancillary and approximated data, which were obtained by interpolation of, or calculation from, measured data. This living data update documents the GLODAPv2.2022 methods and provides a broad overview of the secondary quality control procedures and results.
    Materialart: Online-Ressource
    ISSN: 1866-3516
    Sprache: Englisch
    Verlag: Copernicus GmbH
    Publikationsdatum: 2022
    ZDB Id: 2475469-9
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    Online-Ressource
    Online-Ressource
    Wiley ; 2018
    In:  Limnology and Oceanography: Methods Vol. 16, No. 2 ( 2018-02), p. 68-82
    In: Limnology and Oceanography: Methods, Wiley, Vol. 16, No. 2 ( 2018-02), p. 68-82
    Kurzfassung: Spectrophotometric pH measurements were first introduced for oceanic environments and they facilitated the determination of the marine CO 2 system, including the direct observation of Ocean Acidification. Extended characterizations of the indicator dye m‐Cresol purple over the past two decades enabled the application of this method to natural waters ranging from brines to freshwaters. However, the required determination of the dye's dissociation constants and absorbance properties were exclusively performed in buffer solutions prepared with artificial seawater. Potential perturbations by substances that occur in natural waters, but are not included in the buffer solutions, have never been tested. Therefore, we studied the impact of elevated amounts of dissolved organic matter (DOM) and hydrogen sulfide (H 2 S) on spectrophotometric pH measurements. We did not observe an impact on spectrophotometric pH measurements by H 2 S concentrations up to 400 μmol kg −1 , which reflect high levels such as those reported from the Black Sea. Likewise, natural DOM did not interfere with the spectrophotometric measurements at concentrations typical for oceanic environments and large estuarine systems. However, strongly colored river waters can cause spectral disturbances resulting in calculated pH values that are up to tenths of pH units too low. To circumvent such disturbances, we recommend using intense light sources, a shorter cuvette length or spectrophotometrically calibrated glass electrodes when performing spectrophotometric measurements under critical conditions.
    Materialart: Online-Ressource
    ISSN: 1541-5856 , 1541-5856
    URL: Issue
    Sprache: Englisch
    Verlag: Wiley
    Publikationsdatum: 2018
    ZDB Id: 2161715-6
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    Online-Ressource
    Online-Ressource
    Wiley ; 2016
    In:  Limnology and Oceanography Vol. 61, No. 6 ( 2016-11), p. 1984-2002
    In: Limnology and Oceanography, Wiley, Vol. 61, No. 6 ( 2016-11), p. 1984-2002
    Materialart: Online-Ressource
    ISSN: 0024-3590
    Sprache: Englisch
    Verlag: Wiley
    Publikationsdatum: 2016
    ZDB Id: 2033191-5
    ZDB Id: 412737-7
    SSG: 12
    SSG: 14
    Standort Signatur Einschränkungen Verfügbarkeit
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