GLORIA

GEOMAR Library Ocean Research Information Access

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
Years
  • 1
    Publication Date: 2023-12-31
    Description: The relationship between δ¹⁸O and salinity has been widely studied because it can provide crucial information on the partitioning of isotopes through the hydrological cycle. Current understanding of δ¹⁸O-S characteristics has been used to constrain water cycle models, isotope-enabled atmospheric and ocean models as well as to monitor evaporation (E) and precipitation (P) changes in major ocean basins. However, in the polar regions, where large spatial and temporal variabilities in δ¹⁸O and salinity are expected due to the highly seasonal sea ice melting/formation, river runoff, E-P intensification and rapidly changing summer ice minimum, uncertainties still surround the δ¹⁸O-Salinity relationship. To observe the inputs of freshwater in a poorly-understood, but vastly changing region in the Arctic, we collected matching δ¹⁸O-Salinity data from discrete samples from the surface (bucket sampling) and from profiles (Conductivity, Temperature, Depth (CTD) casts) in the Canadian Arctic Archipelago (CAA) during the Northwest Passage expedition aboard the RV Oden last 17 July – 04 August 2019. Matching δ¹⁸O-Salinity measurements were also obtained from ice core samples as well as from a precipitation event during the cruise. Here, we present more than 200 new and paired δ¹⁸O-Salinity measurements to help represent water mass end-members for freshwater budgeting as well as understanding the changes in the CAA's hydrologic cycle.
    Keywords: CTD profile; ice core isotopes; Northwest Passage Project; NPP; precipitation isotopes; Salinity; surface salinity; water stable isotopes
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2023-12-31
    Description: This data contains one (1) geolocated water stable isotope measurement from one (1) rain event on 29 July 2019. Shipboard rain samples were collected in a separatory funnel filled with a layer of mineral oil to prevent evaporation. Water samples were transferred to a 30-mL Nalgene bottles that were filled to the brim. Bottles were tightly closed, sealed with parafilm, and placed inside sampling bags. It was then transported to the Atmosphere, Climate, and Ecosystems lab at the University of Illinois at Chicago for processing. The δ¹⁸O and dD were measured using a Picarro l2130-I CRDS water isotope analyzer with a wire mesh inserted in the vaporizer inlet. Fifteen injections were made for each sample and necessary corrections to address 'memory effect' were employed. Measurements were normalized using the dD and δ¹⁸O values of internal water standards. Header includes event, latitude, longitude, sampling date, campaign, sampling method, location, isotope analyzer, ¹⁸O values (‰) and D values (‰).
    Keywords: CAA; Canadian Arctic Archipelago; Date/Time of event; Isotope analyzer L2130-i, Picarro Inc.; Latitude of event; Longitude of event; Northwest Passage Project; NPP; NPP19precip; Oden; Oden1907; precipitation isotopes; RAIN; Rain water collector; Salinity; water stable isotopes; δ18O, water; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 2 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2023-12-31
    Description: This data contains 63 geolocated water stable isotopes and salinity measurements from the surface of the ocean along the RV Oden cruise track. Surface seawater sampling was conducted using bucket sampling. This was done by throwing a weighted bucket offboard to sample the surface of the ocean every six (6) hours. Chosen times were 5:00, 11:00, 17:00, and 23:00. Multiple readings of sea surface salinity were recorded using a YSI professional series digital probe per sampling Water samples were transferred to a 30-mL Nalgene bottles that were filled to the brim. Bottles were tightly closed, sealed with parafilm, and placed inside sampling bags. Two samples were collected per sampling point, and all measurements were geolocated. A total of 126 samples were collected from 19 July – 04 August 2019. All water samples were transported to the Atmosphere, Climate, and Ecosystems lab at the University of Illinois at Chicago for processing. The δ¹⁸O and dD were measured using a Picarro l2130-I CRDS water isotope analyzer with a wire mesh inserted in the vaporizer inlet to trap salt from the seawater. Fifteen injections were made for each sample and necessary corrections to address 'memory effect' were employed. Measurements were normalized using the dD and δ¹⁸O values of internal water standards. Data table header includes the event, latitude, longitude, sampling date, campaign, sampling method, location, isotope analyzer model, salinity sensor, ¹⁸O values (‰), D values (‰), and salinity values (psu).
    Keywords: BUCKET; Bucket water sampling; CAA; Canadian Arctic Archipelago; Date/Time of event; Event label; Isotope analyzer L2130-i, Picarro Inc.; Latitude of event; Longitude of event; Northwest Passage Project; NPP; NPP19surface_station_1; NPP19surface_station_10; NPP19surface_station_11; NPP19surface_station_12; NPP19surface_station_13; NPP19surface_station_14; NPP19surface_station_15; NPP19surface_station_16; NPP19surface_station_17; NPP19surface_station_18; NPP19surface_station_19; NPP19surface_station_2; NPP19surface_station_20; NPP19surface_station_21; NPP19surface_station_22; NPP19surface_station_23; NPP19surface_station_24; NPP19surface_station_25; NPP19surface_station_26; NPP19surface_station_27; NPP19surface_station_28; NPP19surface_station_29; NPP19surface_station_3; NPP19surface_station_30; NPP19surface_station_31; NPP19surface_station_32; NPP19surface_station_33; NPP19surface_station_34; NPP19surface_station_35; NPP19surface_station_36; NPP19surface_station_37; NPP19surface_station_38; NPP19surface_station_39; NPP19surface_station_4; NPP19surface_station_40; NPP19surface_station_41; NPP19surface_station_42; NPP19surface_station_43; NPP19surface_station_44; NPP19surface_station_45; NPP19surface_station_46; NPP19surface_station_47; NPP19surface_station_48; NPP19surface_station_49; NPP19surface_station_5; NPP19surface_station_50; NPP19surface_station_51; NPP19surface_station_52; NPP19surface_station_53; NPP19surface_station_54; NPP19surface_station_55; NPP19surface_station_56; NPP19surface_station_57; NPP19surface_station_58; NPP19surface_station_59; NPP19surface_station_6; NPP19surface_station_60; NPP19surface_station_61; NPP19surface_station_62; NPP19surface_station_63; NPP19surface_station_7; NPP19surface_station_8; NPP19surface_station_9; Oden; Oden1907; Salinity; surface salinity; water stable isotopes; YSI Professional Plus Multiparameter Instrument; YSI Pro Plus; δ18O, water; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 189 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2023-12-31
    Description: This data contains ten (10) geolocated water stable isotopes and salinity measurements from three (3) sea ice cores collected during the cruise. Sea ice core sampling was conducted for three (3) ice coring stations. A sea ice core drill was used to collect the cores. Total length of each core was recorded as well as the temperature per 10 cm interval. The cores were then sectioned per 20 cm and the sections were thawed in different Marvin bottles. Once thawed, multiple water salinity measurements were taken using a YSI professional series digital probe. Water samples were transferred to a 30-mL Nalgene bottles that were filled to the brim. Bottles were tightly closed, sealed with parafilm, and placed inside sampling bags. A total of ten (10) samples were collected from the ice core collected. All water samples were transported to the Atmosphere, Climate, and Ecosystems lab at the University of Illinois at Chicago for processing. The δ¹⁸O and dD were measured using a Picarro l2130-I CRDS water isotope analyzer with a wire mesh inserted in the vaporizer inlet to trap salt from the seawater. Fifteen injections were made for each sample and necessary corrections to address 'memory effect' were employed. Measurements were normalized using the dD and δ¹⁸O values of internal water standards. Header includes following details: event, core segment (cm), latitude, longitude, sampling date, campaign, sampling method, location, isotope analyzer, salinity sensor, ¹⁸O values (‰), D values (‰), salinity values (psu).
    Keywords: CAA; Canadian Arctic Archipelago; Date/Time of event; Depth, bottom/max; DEPTH, ice/snow; Depth, top/min; Event label; ice core isotopes; Ice drilling corer (Kovacs); Isotope analyzer L2130-i, Picarro Inc.; Latitude of event; Longitude of event; Northwest Passage Project; NPP; NPP19icecore_station_2; NPP19icecore_station_4; NPP19icecore_station_5; Oden; Oden1907; Salinity; water stable isotopes; YSI Professional Plus Multiparameter Instrument; YSI Pro Plus; δ18O, water; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 74 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2024-02-27
    Description: This data contains 125 geolocated water stable isotope, salinity, and temperature measurements from niskin bottle samples at varying depths from 52 Conductivity, Temperature, Depth (CTD) casts along the RV Oden cruise track. The CTD rosette water sampling was conducted following the CLIVAR/GO-SHIP protocol with a 'water cop' keeping track of the sampling order. Sampling for gases goes first, followed by nutrients, water stable isotopes, and then microbiological and DNA sampling during each cast. Samples for water stable isotopes analyses were collected by filling 30-mL Nalgene bottles to the brim. Bottles were closed tightly, sealed with parafilm, and stored in a labeled sample bag. Sampling depths chosen were based on the profile, location, and whether samples were collected for nutrients. Two samples were collected per depth. A total of 250 samples were collected from the 52 CTD casts from 19 July – 04 August 2019. The corresponding salinity and temperature measurements per sampling depth were collected from the CTD data. All water samples were transported to the Atmosphere, Climate, and Ecosystems lab at the University of Illinois at Chicago for processing. The δ¹⁸O and dD were measured using a Picarro l2130-I CRDS water isotope analyzer with a wire mesh inserted in the vaporizer inlet to trap salt from the seawater. Fifteen injections were made for each sample and necessary corrections to address 'memory effect' were employed. Measurements were normalized using the dD and δ¹⁸O values of internal water standards. Data table header includes the event, depth (m) latitude, longitude, sampling date, campaign, sampling method, location, isotope analyzer, salinity and temperature sensor, ¹⁸O values (‰), D values (‰), salinity values (psu), and temperature values (°C).
    Keywords: CAA; Canadian Arctic Archipelago; CTD; CTD, Sea-Bird SBE 911plus; CTD profile; Date/Time of event; DEPTH, water; Event label; Isotope analyzer L2130-i, Picarro Inc.; Latitude of event; Longitude of event; Northwest Passage Project; NPP; NPP19profile_station_1; NPP19profile_station_10; NPP19profile_station_11; NPP19profile_station_12; NPP19profile_station_13; NPP19profile_station_14; NPP19profile_station_15; NPP19profile_station_16; NPP19profile_station_18; NPP19profile_station_19; NPP19profile_station_2; NPP19profile_station_20; NPP19profile_station_21; NPP19profile_station_23; NPP19profile_station_24; NPP19profile_station_25; NPP19profile_station_26; NPP19profile_station_27; NPP19profile_station_28; NPP19profile_station_29; NPP19profile_station_30; NPP19profile_station_31; NPP19profile_station_32; NPP19profile_station_34; NPP19profile_station_35; NPP19profile_station_36; NPP19profile_station_39; NPP19profile_station_40; NPP19profile_station_41; NPP19profile_station_43; NPP19profile_station_45; NPP19profile_station_46; NPP19profile_station_5; NPP19profile_station_51; NPP19profile_station_52; NPP19profile_station_6; NPP19profile_station_7; NPP19profile_station_8; NPP19profile_station_9; Oden; Oden1907; Salinity; Temperature, water; water stable isotopes; δ18O, water; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 500 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Lennartz, Sinikka T; Marandino, Christa A; von Hobe, Marc; Andreae, Meinrat O; Aranami, Kazushi; Atlas, Elliot L; Berkelhammer, Max; Bingemer, Heinz G; Booge, Dennis; Cutter, Gregory A; Cortes, Pau; Kremser, Stefanie; Law, Cliff S; Marriner, Andrew; Simo, Rafel; Quack, Birgit; Uher, Günther; Xie, Huixiang; Xu, Xiaobin (2020): Marine carbonyl sulfide (OCS) and carbon disulfide (CS2): a compilation of measurements in seawater and the marine boundary layer. Earth System Science Data, 12(1), 591-609, https://doi.org/10.5194/essd-12-591-2020
    Publication Date: 2024-05-11
    Description: The database includes measurements of the trace gases carbonyl sulfide (OCS) and carbon disulfide (CS2) in seawater (in picomol per liter) and the marine boundary layer (parts per trillion, ppt). It consists of individual datasets compiled from published original data, digitalization from publications (pdf documents) and unpublished data. Only shipborne measurements or measurements from time series stations with a dominant marine signal are included. The database contains mainly surface ocean measurements, but few available profiles down to 〉1000 m are included as well. Temporal resolution ranges from 12 minutes to hourly or monthly intervals. The database includes the following metadata (if available): latitude, longitude, depth, time of sampling, meteorological and physical parameters, main reference, method, contributor(s). The database is intended to facilitate model evaluation and the identification of global patterns. Data in excel and txt-files are identical.
    Keywords: air-sea exchange; carbon disulfide; carbonyl sulfide; File content; File format; File name; File size; OCS_CS2_db; trace gas; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2021-02-08
    Description: For the past decade, observations of carbonyl sulfide (OCS or COS) have been investigated as a proxy for carbon uptake by plants. OCS is destroyed by enzymes that interact with CO2 during photosynthesis, namely carbonic anhydrase (CA) and RuBisCO, where CA is the more important one. The majority of sources of OCS to the atmosphere are geographically separated from this large plant sink, whereas the sources and sinks of CO2 are co-located in ecosystems. The drawdown of OCS can therefore be related to the uptake of CO2 without the added complication of co-located emissions comparable in magnitude. Here we review the state of our understanding of the global OCS cycle and its applications to ecosystem carbon cycle science. OCS uptake is correlated well to plant carbon uptake, especially at the regional scale. OCS can be used in conjunction with other independent measures of ecosystem function, like solar-induced fluorescence and carbon and water isotope studies. More work needs to be done to generate global coverage for OCS observations and to link this powerful atmospheric tracer to systems where fundamental questions concerning the carbon and water cycle remain.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2018-12-17
    Description: Current climate models disagree on how much carbon dioxide land ecosystems take up for photosynthesis. Tracking the stronger carbonyl sulfide signal could help.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2023-02-08
    Description: Carbonyl sulfide (OCS) and carbon disulfide (CS2) are volatile sulfur gases that are naturally formed in seawater and exchanged with the atmosphere. OCS is the most abundant sulfur gas in the atmosphere, and CS2 is its most important precursor. They have gained interest due to their direct (OCS) or indirect (CS2 via oxidation to OCS) contribution to the stratospheric sulfate aerosol layer. Furthermore, OCS serves as a proxy to constrain terrestrial CO2 uptake by vegetation. Oceanic emissions of both gases contribute a major part to their atmospheric concentration. Here we present a database of previously published and unpublished, mainly ship-borne measurements in seawater and the marine boundary layer for both gases, available at https://doi.pangaea.de/10.1594/PANGAEA.905430 (Lennartz et al., 2019). The database contains original measurements as well as data digitalized from figures in publications from 42 measurement campaigns, i.e. cruises or time series stations, ranging from 1982 to 2019. OCS data cover all ocean basins except for the Arctic Ocean, as well as all months of the year, while the CS2 dataset shows large gaps in spatial and temporal coverage. Concentrations are consistent across different sampling and analysis techniques for OCS. The database is intended to support the identification of global spatial and temporal patterns and to facilitate the evaluation of model simulations.
    Type: Article , PeerReviewed
    Format: text
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...