GLORIA

GEOMAR Library Ocean Research Information Access

X
feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Document type
Keywords
Publisher
Years
  • 1
    facet.materialart.
    Unknown
    Physical Oceanography measured on bottle water samples during ODEN expedition SO21 for the Synoptic Arctic Survey (2022)
    PANGAEA
    Details
    Publication Date: 2024-03-01
    Description: Discrete bottle values of Temperature, Salinity, Dissolved Oxygen, Chlorophyll A fluorescence and Coloured Dissolved Organic Matter (CDOM) collected in the Arctic Ocean, over the western Eurasian Basin and Lomonosov Ridge, between 2 August and 11 September 2021, from I/B Oden. This is the Swedish contribution to the international Synoptic Arctic Survey. This dataset merges the bottle data from the full-depth physical CTD and the shallow biological CTD. Both systems had the standard SeaBird SBE911 plus system with dual sensors to measure in-situ temperature and conductivity and single sensors measuring pressure and oxygen. The physical CTD also had a CDOM sensor (Turner Cyclops fluorometer), while the Chl-A fluorometer (WET Labs, ECO-AFL/FL) was moved throughout the expedition between the two systems. Salinity, Oxygen, Chl-A fluorescence and CDOM were calibrated against sample data collected and analysed by the co-authors: - Salinity samples from the deep stations were analysed post-cruise using a salinometer (Guildline Autosal) and IAPSO standard seawater at the GEOMAR, Germany. - Dissolved oxygen was determined onboard using an automatic Winkler titration setup with UV detection (Scripps Institute of Oceanography Oxygen Titration System version 2.35m). - Chl-A concentration was determined post-cruise from flow cytometry (FCM) at Linnaeus University, Sweden. The samples consisted of 4 mL cryovials, of which 3.8 mL was sample water and 76 μL 25% EM grade glutaraldehyde solution (Glu stock). The samples incubated at room temperature for 5 minutes before flash freezing in liquid nitrogen and then placing in the -80 °C freezer in cryoboxes. - CDOM was determined post-cruise at the National Institute of Aquatic Resources - DTU Aqua, Denmark, following the method of Lawaetz and Stedmon (2009) This dataset contains the bottle data of the casts where bottles were fired. For more information about each sensor and their calibration, the reader is invited to check the cruise report (final version submitted on 20 September; shareable version with DOI coming soon)
    Keywords: Arctic; Arctic Ocean; Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic; ARICE; Bottle data; Bottle number; CDOM; Chl-a; CTD, Sea-Bird, SBE 911plus; CTD/Rosette; DATE/TIME; Density, mass density; DEPTH, water; Der arktische Ozean 2020 – Ventilationszeitskalen, anthropogener Kohlenstoff und Variabilität in einer sich verändernden Umgebung; DFG_456675218; Event label; Fluorescence, chlorophyll; Fluorescence, colored dissolved organic matter; ITS-90, temperature scale; LATITUDE; LONGITUDE; New insights on ocean circulation and the fate of organic carbon in the Arctic Ocean; NOC; oceanography; Oden; Oxygen; Oxygen, dissolved; Practical Salinity Scale – 1978 (PSU78); Pressure, water; PSU78; Quality flag, absolute salinity; Quality flag, conservative water temperature; Quality flag, density; Quality flag, fluorescence, chlorophyll; Quality flag, fluorescence, colored dissolved organic matter; Quality flag, oxygen; Quality flag, potential water temperature; Quality flag, salinity; Quality flag, water temperature; Salinity; Salinity, absolute; Salinity; Temperature; SAS-Oden_2021; Seadatanet flag: Data quality control procedures according to SeaDataNet (2010); SO21; SO21_01-01; SO21_03-01; SO21_03-02; SO21_05-01; SO21_05-02; SO21_05-03; SO21_07-01; SO21_07-03; SO21_07-04; SO21_07-05; SO21_08-01; SO21_08-02; SO21_08-03; SO21_08-04; SO21_08-06; SO21_08-09; SO21_11-01; SO21_13-01; SO21_13-03; SO21_13-04; SO21_13-05; SO21_16-01; SO21_16-03; SO21_16-04; SO21_16-05; SO21_16-06; SO21_18-01; SO21_18-03; SO21_18-04; SO21_18-05; SO21_20-01; SO21_20-02; SO21_20-03; SO21_22-08; SO21_22-09; SO21_22-10; SO21_22-11; SO21_24-01; SO21_24-02; SO21_24-03; SO21_25-01; SO21_25-02; SO21_26-01; SO21_26-02; SO21_26-03; SO21_26-05; SO21_26-11; SO21_28-01; SO21_28-02; SO21_28-03; SO21_30-01; SO21_30-02; SO21_30-03; SO21_30-11; SO21_30-13; SO21_32-02; SO21_33-01; SO21_33-02; SO21_33-03; SO21_33-05; SO21_35-11; SO21_35-12; SO21_35-13; SO21_35-15; SO21_37-01; SO21_38-08; SO21_38-13; SO21_38-14; SO21_38-15; SO21_38-17; SO21_40-01; SO21_41-01; SO21_42-01; SO21_42-02; SO21_42-06; SO21_42-08; SO21_44-01; SO21_45-01; SO21_46-01; SO21_46-02; SO21_47-01; SO21_48-01; SO21_48-02; SO21_48-04; SO21_50-06; SO21_50-11; SO21_50-13; SO21_50-16; SO21_52-01; SO21_53-07; SO21_53-08; SO21_53-09; SO21_53-14; SO21_53-15; SO21_56-01; SO21_56-03; SO21_56-05; SO21_56-06; SO21_56-07; SO21_56-08; SO21_58-09; SO21_58-12; SO21_58-15; SO21_58-17; SO21_58-18; Synoptic Arctic Survey; Temperature, water; Temperature, water, conservative; Temperature, water, potential; TEOS-10; Thermodynamic Equation Of Seawater - 2010 (TEOS-10); WAOW; Why is the deep Arctic Ocean Warming?
    Type: Dataset
    Format: text/tab-separated-values, 49362 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 2
    facet.materialart.
    Unknown
    Physical Oceanography during ODEN expedition SO21 for the Synoptic Arctic Survey (2022)
    PANGAEA
    Details
    Publication Date: 2024-03-01
    Description: Hydrographic (CTD) profiles of Temperature, Salinity, Dissolved Oxygen, Chlorophyll A fluorescence and Coloured Dissolved Organic Matter (CDOM) collected in the Arctic Ocean, over the western Eurasian Basin and Lomonosov Ridge, between 2 August and 11 September 2021, from I/B Oden. This is the Swedish contribution to the international Synoptic Arctic Survey. This dataset merges the full-depth physical CTD and the shallow biological CTD profiles. Both systems had the standard SeaBird SBE911 plus system with dual sensors to measure in-situ temperature and conductivity and single sensors measuring pressure and oxygen. The physical CTD also had a CDOM sensor (Turner Cyclops fluorometer), while the Chl-A fluorometer (WET Labs, ECO-AFL/FL) was moved throughout the expedition between the two systems. Salinity, Oxygen, Chl-A fluorescence and CDOM were calibrated against sample data collected and analysed by the co-authors: - Salinity samples from the deep stations were analysed post-cruise using a salinometer (Guildline Autosal) and IAPSO standard seawater at the GEOMAR, Germany. - Dissolved oxygen was determined onboard using an automatic Winkler titration setup with UV detection (Scripps Institute of Oceanography Oxygen Titration System version 2.35m). - Chl-A concentration was determined post-cruise from flow cytometry (FCM) at Linnaeus University, Sweden. The samples consisted of 4 mL cryovials, of which 3.8 mL was sample water and 76 μL 25% EM grade glutaraldehyde solution (Glu stock). The samples incubated at room temperature for 5 minutes before flash freezing in liquid nitrogen and then placing in the -80 °C freezer in cryoboxes. - CDOM was determined post-cruise at the National Institute of Aquatic Resources - DTU Aqua, Denmark, following the method of Lawaetz and Stedmon (2009) This dataset contains the 1-m bin-averaged profiles. For more information about each sensor and their calibration, the reader is invited to check the cruise report (final version submitted on 20 September; shareable version with DOI coming soon)
    Keywords: Arctic; Arctic Ocean; Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic; ARICE; CDOM; Chl-a; CTD; CTD, Sea-Bird, SBE 911plus; CTD/Rosette; DATE/TIME; Density, mass density; DEPTH, water; Der arktische Ozean 2020 – Ventilationszeitskalen, anthropogener Kohlenstoff und Variabilität in einer sich verändernden Umgebung; DFG_456675218; Event label; Fluorescence, chlorophyll; Fluorescence, colored dissolved organic matter; ITS-90, temperature scale; LATITUDE; LONGITUDE; New insights on ocean circulation and the fate of organic carbon in the Arctic Ocean; NOC; oceanography; Oden; Oxygen; Oxygen, dissolved; Practical Salinity Scale – 1978 (PSU78); Pressure, water; PSU78; Quality flag, absolute salinity; Quality flag, conservative water temperature; Quality flag, density; Quality flag, fluorescence, chlorophyll; Quality flag, fluorescence, colored dissolved organic matter; Quality flag, oxygen; Quality flag, potential water temperature; Quality flag, salinity; Quality flag, water temperature; Salinity; Salinity, absolute; Salinity; Temperature; SAS-Oden_2021; Seadatanet flag: Data quality control procedures according to SeaDataNet (2010); SO21; SO21_01-01; SO21_03-01; SO21_03-02; SO21_05-01; SO21_05-02; SO21_05-03; SO21_07-01; SO21_07-03; SO21_07-04; SO21_07-05; SO21_08-01; SO21_08-02; SO21_08-03; SO21_08-04; SO21_08-06; SO21_08-09; SO21_11-01; SO21_11-02; SO21_13-01; SO21_13-03; SO21_13-04; SO21_13-05; SO21_14-05; SO21_16-01; SO21_16-03; SO21_16-04; SO21_16-05; SO21_16-06; SO21_18-01; SO21_18-03; SO21_18-04; SO21_18-05; SO21_20-01; SO21_20-02; SO21_20-03; SO21_22-03; SO21_22-08; SO21_22-09; SO21_22-10; SO21_22-11; SO21_24-01; SO21_24-02; SO21_24-03; SO21_25-01; SO21_25-02; SO21_26-01; SO21_26-02; SO21_26-03; SO21_26-05; SO21_26-11; SO21_28-01; SO21_28-02; SO21_28-03; SO21_30-01; SO21_30-02; SO21_30-03; SO21_30-11; SO21_30-13; SO21_30-16; SO21_32-01; SO21_32-02; SO21_33-01; SO21_33-02; SO21_33-03; SO21_33-05; SO21_35-08; SO21_35-11; SO21_35-12; SO21_35-13; SO21_35-15; SO21_37-01; SO21_38-08; SO21_38-13; SO21_38-14; SO21_38-15; SO21_38-17; SO21_40-01; SO21_41-01; SO21_42-01; SO21_42-02; SO21_42-06; SO21_42-08; SO21_44-01; SO21_45-01; SO21_46-01; SO21_46-02; SO21_47-01; SO21_48-01; SO21_48-02; SO21_48-04; SO21_50-06; SO21_50-11; SO21_50-13; SO21_50-16; SO21_52-01; SO21_53-05; SO21_53-06; SO21_53-07; SO21_53-08; SO21_53-09; SO21_53-14; SO21_53-15; SO21_56-01; SO21_56-03; SO21_56-05; SO21_56-06; SO21_56-07; SO21_56-08; SO21_58-09; SO21_58-12; SO21_58-15; SO21_58-17; SO21_58-18; Synoptic Arctic Survey; Temperature, water; Temperature, water, conservative; Temperature, water, potential; TEOS-10; Thermodynamic Equation Of Seawater - 2010 (TEOS-10); WAOW; Why is the deep Arctic Ocean Warming?
    Type: Dataset
    Format: text/tab-separated-values, 3139799 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 3
    facet.materialart.
    Unknown
    Transient Tracers and Eddies along GO-SHIP section A10.5 (2017)
    In:  (Bachelor thesis), Christian-Albrechts-Universität zu Kiel, Kiel, Germany, 51 pp
    Details
    Publication Date: 2020-10-15
    Type: Thesis , NonPeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    OceanRep: Thesis - not published by a publisher
  • 4
    facet.materialart.
    Unknown
    pCO2 in the Mediterranean Sea during the cruise MSM 72 (2020)
    Details
    Publication Date: 2023-09-19
    Type: Thesis , NonPeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    OceanRep: Thesis - not published by a publisher
  • 5
    facet.materialart.
    Unknown
    Physical and biogeochemical parameters of the Mediterranean Sea during a cruise with RV Maria S. Merian in March 2018 (2020)
    Copernicus Publications (EGU)
    Details
    Publication Date: 2023-02-08
    Description: The last few decades have seen dramatic changes in the hydrography and biogeochemistry of the Mediterranean Sea. The complex bathymetry and highly variable spatial and temporal scales of atmospheric forcing, convective and ventilation processes contribute to generate complex and unsteady circulation patterns and significant variability in biogeochemical systems. Part of the variability of this system can be influenced by anthropogenic contributions. Consequently, it is necessary to document details and to understand trends in place to better relate the observed processes and to possibly predict the consequences of these changes. In this context we report data from an oceanographic cruise in the Mediterranean Sea on the German research vessel Maria S. Merian (MSM72) in March 2018. The main objective of the cruise was to contribute to the understanding of long-term changes and trends in physical and biogeochemical parameters, such as the anthropogenic carbon uptake and to further assess the hydrographical situation after the major climatological shifts in the eastern and western part of the basin, known as the Eastern and Western Mediterranean Transients. During the cruise, multidisciplinary measurements were conducted on a predominantly zonal section throughout the Mediterranean Sea, contributing to the Med-SHIP and GO-SHIP long-term repeat cruise section that is conducted at regular intervals in the Mediterranean Sea to observe changes and impacts on physical and biogeochemical variables.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    OceanRep: Article in a Scientific Journal - peer-reviewed
  • 6
    facet.materialart.
    Unknown
    Western Subpolar North Atlantic transport variability, Cruise No. MSM94, 02. August - 06. September 2020, Emden (Germany) - Emden (Germany) (2020)
    Gutachterpanel Forschungsschiffe
    Details
    Publication Date: 2023-03-31
    Description: SPNA transport 2020 The scientific program of the MARIA S. MERIAN MSM94 expedition was dedicated to studies on the intensity of water mass transformation and the transport of water masses in the boundary current systems off Labrador and at the southwestern tip of Greenland. During the expedition we redeployed 11 moorings and recovered 1 bottom lander. Measurements of the vertical structure of temperature, salinity, density, oxygen, optical properties and the flow along selected sections have been surveyed during the MSM94 expedition. Close to the surface, permanent registrations are carried out with the thermosalinograph (temperature, salinity) and meteorological data are continuously collected. Flow measurements up to 1000m depth are performed with the ships installed ADCPs. Argo floats (IFREMER, BSH) and surface drifter (NOC, UK) were also deployed. The expedition is a contribution to international projects (OSNAP, Blue Action, EuroSea). The expedition was conducted during the COVID-19 pandemic and modifications to the science program had to be applied (e.g. Start/end-port Emden, Germany, reduced science crew and respective cut’s in data acquisition).
    Type: Report , NonPeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    OceanRep: Report - Cruise Report
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...