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  • 1
    Keywords: Earth sciences ; Earth Sciences ; Analytical chemistry ; Geochemistry ; Oceanography ; Geobiology ; Geochemie ; Meereskunde ; Ostsee
    Description / Table of Contents: This book provides a comprehensive review of the biogeochemistry in the Baltic Sea. It is based on the fact that biogeochemical processes that are relevant for the ecological state of the Baltic Sea (and other sea areas), are all in some way related to the production and mineralization of organic matter (biomass) and thus are associated with the consumption or release of CO2. The significant progress with regard to our chemical analytical capabilities concerning the marine CO2 system has facilitated new approaches to study the Baltic Sea biogeochemistry, in particular with regard to a quantitative process understanding. To demonstrate this, the authors present the fundamentals of the marine CO2 system in a theoretically sound, but still intelligible way. This is followed by a comprehensive presentation of our current knowledge about the CO2 system in the Baltic Sea and the implications for our understanding of biogeochemical processes such as production/mineralization of organic matter and the stoichiometry involved, nitrogen fixation, denitrification, and phosphate transformations at varying redox conditions. Finally, the CO2 gas exchange balance and related problems such as acidification are addressed
    Type of Medium: Online Resource
    Pages: Online-Ressource (XII, 110 p. 54 illus, online resource)
    ISBN: 9783319616995
    Series Statement: Springer Oceanography
    Language: English
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  • 2
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Biogeochemistry--Baltic Sea. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (119 pages)
    Edition: 1st ed.
    ISBN: 9783319616995
    Series Statement: Springer Oceanography Series
    Language: English
    Note: Intro -- Preface -- Contents -- About the Authors -- Abbreviations -- 1 Introduction -- 1.1 History of CO2 System Research in the Baltic Sea -- 1.2 Objectives of This Book -- References -- 2 The Marine CO2 System and Its Peculiarities in the Baltic Sea -- 2.1 Atmospheric CO2 Over the Baltic Sea -- 2.2 Aqueous Equilibrium Chemistry of CO2 -- 2.3 Measurable Variables of the Marine CO2 System -- 2.3.1 CO2 Equilibrium Fugacity and Partial Pressure -- 2.3.2 Total CO2 and pH -- 2.3.3 Alkalinity -- 2.3.4 Physico-Chemical Properties of the Master Variables -- 2.4 CO2 Air-Sea Gas Exchange -- References -- 3 The Main Hydrographic Characteristics of the Baltic Sea -- 3.1 Water Budget and Estuarine Circulation -- 3.2 Seasonality of the Stratification -- 3.3 Stagnation and Inflow Events -- References -- 4 The Database -- 4.1 Studies of the Surface Water CO2 System -- 4.2 Investigations of the Deep Water CO2 Accumulation -- References -- 5 Surface Water Biogeochemistry as Derived from pCO2 Observations -- 5.1 Seasonal and Regional Patterns of pCO2 and CT -- 5.1.1 Characteristics of the pCO2 Time Series -- 5.1.2 Long-Term Changes in pCO2 -- 5.1.3 The Seasonal Fine Structure of the pCO2 -- 5.1.4 From pCO2 Measurements to Total CO2 Data -- 5.2 A Walk Through the Seasons -- 5.2.1 Timing of the Spring Bloom and the Role of Solar Radiation -- 5.2.2 Quantification of Spring Bloom Productivity -- 5.2.3 Nitrogen Supply for the Spring Bloom -- 5.2.4 Net Community Production and Nutrient Consumption -- 5.2.5 The "Blue Water" Period -- 5.2.6 Control of Mid-Summer Net Community Production and N-fixation -- 5.2.7 Estimation of Depth-Integrated N-fixation -- 5.2.8 Autumn Mixing and Upwelling: The Occurrence of a Last Bloom Event -- 5.2.9 Annual CT* Cycling Presented as CT* Versus SST Diagrams -- References. , 6 Organic Matter Mineralization as Reflected in Deep-Water CT Accumulation -- 6.1 Total CO2 Dynamics During Periods of Stagnation and Water Renewal -- 6.2 Organic Matter Mineralization Rates Derived from CT Mass-Balance Calculations -- 6.3 Release and Transformations of Nutrients During OM Mineralization -- References -- 7 Progress Made by Investigations of the CO2 System and Open Questions -- Index.
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  • 3
    Publication Date: 2022-10-10
    Description: 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 sulphur 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 onboard the RV Knorr in the Indian Ocean in 1994–1995 which are now adjusted using 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, 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.
    Type: Article , NonPeerReviewed
    Format: text
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  • 4
    Publication Date: 2024-02-07
    Description: The oceanic uptake and resulting storage of the anthropogenic CO2 (Cant) that humans have emitted into the atmosphere moderates climate change. Yet our knowledge about how this uptake and storage has progressed in time remained limited. Here, we determine decadal trends in the storage of Cant by applying the eMLR(C*) regression method to ocean interior observations collected repeatedly since the 1990s. We find that the global ocean storage of Cant grew from 1994 to 2004 by 29 ± 3 Pg C dec−1 and from 2004 to 2014 by 27 ± 3 Pg C dec−1 (±1σ). The storage change in the second decade is about 15 ± 11% lower than one would expect from the first decade and assuming proportional increase with atmospheric CO2. We attribute this reduction in sensitivity to a decrease of the ocean buffer capacity and changes in ocean circulation. In the Atlantic Ocean, the maximum storage rate shifted from the Northern to the Southern Hemisphere, plausibly caused by a weaker formation rate of North Atlantic Deep Waters and an intensified ventilation of mode and intermediate waters in the Southern Hemisphere. Our estimates of the Cant accumulation differ from cumulative net air-sea flux estimates by several Pg C dec−1, suggesting a substantial and variable, but uncertain net loss of natural carbon from the ocean. Our findings indicate a considerable vulnerability of the ocean carbon sink to climate variability and change. Key Points: - The global ocean storage of anthropogenic carbon grew by 29 ± 3 and 27 ± 3 Pg C dec−1 from 1994 to 2004 and 2004 to 2014, respectively - The change in oceanic storage of anthropogenic carbon relative to the atmospheric CO2 growth decreased by 15 ± 11% from the first to the second decade - This reduction is attributed to a decrease of the ocean buffer capacity and changes in ocean circulation
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
    Format: text
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  • 5
    Publication Date: 2024-02-07
    Description: 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 sulphur 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 onboard the RV Knorr in the Indian Ocean in 1994–1995 which are now adjusted using 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, 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.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 6
    Publication Date: 2024-02-07
    Description: This contribution to the RECCAP2 (REgional Carbon Cycle Assessment and Processes) assessment analyzes the processes that determine the global ocean carbon sink, and its trends and variability over the period 1985-2018, using a combination of models and observation-based products. The mean sea-air CO2 flux from 1985 to 2018 is -1.6 +/- 0.2 PgC yr(-1) based on an ensemble of reconstructions of the history of sea surface pCO(2) (pCO(2) products). Models indicate that the dominant component of this flux is the net oceanic uptake of anthropogenic CO2, which is estimated at -2.1 +/- 0.3 PgC yr(-1) by an ensemble of ocean biogeochemical models, and -2.4 +/- 0.1 PgC yr(-1) by two ocean circulation inverse models. The ocean also degasses about 0.65 +/- 0.3 PgC yr(-1) of terrestrially derived CO2, but this process is not fully resolved by any of the models used here. From 2001 to 2018, the pCO2 products reconstruct a trend in the ocean carbon sink of -0.61 +/- 0.12 PgC yr(-1) decade(-1), while biogeochemical models and inverse models diagnose an anthropogenic CO2-driven trend of -0.34 +/- 0.06 and -0.41 +/- 0.03 PgC yr(-1) decade(-1), respectively. This implies a climate-forced acceleration of the ocean carbon sink in recent decades, but there are still large uncertainties on the magnitude and cause of this trend. The interannual to decadal variability of the global carbon sink is mainly driven by climate variability, with the climate-driven variability exceeding the CO2-forced variability by 2-3 times. These results suggest that anthropogenic CO2 dominates the ocean CO2 sink, while climate-driven variability is potentially large but highly uncertain and not consistently captured across different methods.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 7
    Publication Date: 2023-03-14
    Description: This dataset is part of a dataset collection. Please read the documentation in Kiel fjord carbonate chemistry data between 2015 (February) and 2016 (January) doi:10.1594/PANGAEA.876551 for details on sampling, measurement and data processing.
    Keywords: Alkalinity, total; Carbon, inorganic, dissolved; Carbon dioxide, partial pressure; CO2S; CO2 Sensor; DATE/TIME; DEPTH, water; interpolated; Kiel Fjord; Kiel-Fjord_GEOMAR; pH; Phosphate; Salinity; Silicate; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 232 data points
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  • 8
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Carbon, total; Carbon dioxide, partial pressure; CT; DATE/TIME; DEPTH, water; Discretely sampled from water stream of Underway-Equilibrator-System; LATITUDE; LONGITUDE; OC16/11; OC16/11-track; Oceania; Oxygen; Oxygen saturation; pH; Salinity; Temperature, water; Underway cruise track measurements; Underway-Equilibrator-System
    Type: Dataset
    Format: text/tab-separated-values, 286 data points
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  • 9
    Publication Date: 2023-01-13
    Description: A HydroC® CO2 sensor was deployed from a pontoon at the waterfront of the GEOMAR west shore building into Kiel Fjord, Western Baltic Sea (Kiel, Germany; 54°19'48.78"N, 010° 8'59.44"E). Since the pontoon is floating the deployment depth of the sensor was constant at 1m. Data of two deployment intervals are published here: February 2015 – May 2015 and August 2015 – January 2016.
    Keywords: CO2S; CO2 Sensor; Kiel Fjord; Kiel-Fjord_GEOMAR
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 10
    Publication Date: 2023-01-13
    Keywords: Carbon dioxide, partial pressure; CT; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; OC16/11; OC16/11-track; Oceania; Salinity; Temperature, water; Underway cruise track measurements; Underway-Equilibrator-System
    Type: Dataset
    Format: text/tab-separated-values, 10134 data points
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