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  • 1
    Publication Date: 2023-12-12
    Description: Near-daily concentrations of Chlorophyll a and phaeopigments from RV Polarsterns underway water supply system (inlet at 11m water depth) collected during legs 1,3,4, and 5 of the MOSAiC (PS122) drift expedition in the central Arctic Ocean. 2-4L of water were filtered onto pre-combusted GF/F filters (nominal pore size 0.7µm) and frozen at -80°C. Samples were subsequently extracted in 90°C acetone, homogenized using a cell mill, and measured on the following day using a Turner flourometer, followed by an acidification step to determine phaeopigments (see Knap et al. 1996 for details and calculations). Samples were collected from end of October 2019 to beginning of October 2020, with a gap between mid-December and the end of February.
    Keywords: Acidification method according to Knap et al. (1996); Activity description; Arctic Ocean; Cast number; CHLa; Chl-a; Chlorophyll a; DATE/TIME; DEPTH, water; Device type; Event label; LATITUDE; Leg Number; LONGITUDE; Mosaic; MOSAiC; MOSAiC_ECO; MOSAiC20192020; Multidisciplinary drifting Observatory for the Study of Arctic Climate; North Greenland Sea; Phaeopigments; pigments; Pigments, Turner fluorometer; Polarstern; PS122/1; PS122/1_10-109; PS122/1_10-84; PS122/1_10-85; PS122/1_10-86; PS122/1_10-87; PS122/1_10-88; PS122/1_10-89; PS122/1_11-14; PS122/1_11-2; PS122/1_11-26; PS122/1_11-36; PS122/1_11-48; PS122/1_5-42; PS122/1_5-44; PS122/1_5-87; PS122/1_6-88; PS122/1_6-89; PS122/1_6-90; PS122/1_6-91; PS122/1_6-92; PS122/1_6-94; PS122/1_7-115; PS122/1_7-116; PS122/1_7-117; PS122/1_7-118; PS122/1_7-119; PS122/1_7-132; PS122/1_8-127; PS122/1_8-89; PS122/1_8-90; PS122/1_8-91; PS122/1_8-92; PS122/1_8-93; PS122/1_9-112; PS122/1_9-82; PS122/1_9-83; PS122/1_9-84; PS122/1_9-85; PS122/1_9-86; PS122/3; PS122/3_29-78; PS122/3_29-89; PS122/3_30-15; PS122/3_30-49; PS122/3_30-51; PS122/3_30-63; PS122/3_30-80; PS122/3_30-93; PS122/3_31-14; PS122/3_31-27; PS122/3_31-40; PS122/3_31-48; PS122/3_31-58; PS122/3_31-74; PS122/3_31-83; PS122/3_32-20; PS122/3_32-35; PS122/3_32-4; PS122/3_32-47; PS122/3_32-49; PS122/3_32-69; PS122/3_32-87; PS122/3_33-16; PS122/3_33-49; PS122/3_33-54; PS122/3_33-6; PS122/3_33-77; PS122/3_33-94; PS122/3_33-95; PS122/3_34-19; PS122/3_34-33; PS122/3_34-44; PS122/3_34-48; PS122/3_34-6; PS122/3_34-73; PS122/3_34-82; PS122/3_35-101; PS122/3_35-109; PS122/3_35-27; PS122/3_35-45; PS122/3_35-6; PS122/3_35-68; PS122/3_35-86; PS122/3_36-100; PS122/3_36-126; PS122/3_36-136; PS122/3_36-33; PS122/3_36-36; PS122/3_36-7; PS122/3_36-71; PS122/3_37-10; PS122/3_37-106; PS122/3_37-107; PS122/3_37-113; PS122/3_37-13; PS122/3_37-43; PS122/3_37-54; PS122/3_38-153; PS122/3_38-154; PS122/3_38-156; PS122/3_38-23; PS122/3_38-29; PS122/3_38-73; PS122/3_39-118; PS122/3_39-119; PS122/3_39-120; PS122/3_39-121; PS122/3_39-122; PS122/3_39-123; PS122/3_39-124; PS122/3_40-23; PS122/3_40-24; PS122/3_40-25; PS122/3_40-56; PS122/3_40-57; PS122/3_40-58; PS122/3_40-59; PS122/3_41-28; PS122/3_41-29; PS122/3_41-30; PS122/3_41-31; PS122/3_41-39; PS122/3_41-43; PS122/3_41-49; PS122/3_42-15; PS122/3_42-2; PS122/3_42-22; PS122/3_42-36; PS122/3_42-37; PS122/3_42-46; PS122/3_42-54; PS122/3_42-59; PS122/3_42-7; PS122/4; PS122/4_44-104; PS122/4_44-117; PS122/4_44-132; PS122/4_44-148; PS122/4_44-163; PS122/4_44-168; PS122/4_44-176; PS122/4_44-192; PS122/4_44-20; PS122/4_44-21; PS122/4_44-212; PS122/4_44-33; PS122/4_44-40; PS122/4_44-41; PS122/4_44-55; PS122/4_44-66; PS122/4_44-84; PS122/4_44-86; PS122/4_44-93; PS122/4_44-94; PS122/4_45-109; PS122/4_45-110; PS122/4_45-111; PS122/4_45-134; PS122/4_45-27; PS122/4_45-28; PS122/4_45-49; PS122/4_46-10; PS122/4_46-156; PS122/4_46-157; PS122/4_46-158; PS122/4_46-159; PS122/4_46-34; PS122/4_46-54; PS122/4_47-141; PS122/4_47-142; PS122/4_47-15; PS122/4_47-30; PS122/4_47-78; PS122/4_47-79; PS122/4_47-95; PS122/4_48-107; PS122/4_48-108; PS122/4_48-109; PS122/4_48-110; PS122/4_48-16; PS122/4_48-181; PS122/4_48-182; PS122/4_49-104; PS122/4_49-13; PS122/4_49-41; PS122/4_49-42; PS122/4_49-60; PS122/4_49-65; PS122/4_49-84; PS122/4_50-15; PS122/4_50-23; PS122/4_50-33; PS122/4_50-46; PS122/4_50-54; PS122/4_50-6; PS122/4_50-60; PS122/4_50-63; PS122/4_50-76; PS122/5; PS122/5_59-118; PS122/5_59-131; PS122/5_59-150; PS122/5_59-157; PS122/5_59-165; PS122/5_59-166; PS122/5_59-177; PS122/5_59-190; PS122/5_59-205; PS122/5_59-221; PS122/5_59-24; PS122/5_59-257; PS122/5_59-283; PS122/5_59-289; PS122/5_59-3; PS122/5_59-34; PS122/5_59-385; PS122/5_59-386; PS122/5_59-387; PS122/5_59-388; PS122/5_59-48; PS122/5_59-49; PS122/5_59-52; PS122/5_59-54; PS122/5_59-56; PS122/5_59-71; PS122/5_59-9; PS122/5_60-132; PS122/5_60-252; PS122/5_60-253; PS122/5_60-254; PS122/5_60-255; PS122/5_60-256; PS122/5_60-257; PS122/5_61-120; PS122/5_61-121; PS122/5_61-122; PS122/5_61-306; PS122/5_61-307; PS122/5_61-308; PS122/5_61-309; PS122/5_62-245; PS122/5_62-246; PS122/5_62-247; PS122/5_62-248; PS122/5_62-249; PS122/5_62-250; PS122/5_62-251; PS122/5_63-113; PS122/5_63-114; PS122/5_63-147; PS122/5_63-148; PS122/5_63-149; PS122/5_63-22; PS122/5_63-23; PS122/5_63-26; PS122/5_63-65; PS122/5_63-67; PS122/5_63-79; Tap; TAP; under ice; Underway water sampling; UWS; Volume
    Type: Dataset
    Format: text/tab-separated-values, 3863 data points
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2024-03-01
    Description: First-year sea-ice thickness, draft, salinity, temperature, and density were measured during near-weekly surveys at the main first-year ice coring site (MCS-FYI) during the MOSAiC expedition (legs 1 to 4). The ice cores were extracted either with a 9-cm (Mark II) or 7.25-cm (Mark III) internal diameter ice corers (Kovacs Enterprise, US). This data set includes data from 23 coring site visits and were performed from 28 October 2019 to 29 July 2020 at coring locations within 130 m to each other in the MOSAiC Central Observatory. During each coring event, ice temperature was measured in situ from a separate temperature core, using Testo 720 thermometers in drill holes with a length of half-core-diameter at 5-cm vertical resolution. Ice bulk practical salinity was measured from melted core sections at 5-cm resolution using a YSI 30 conductivity meter. Ice density was measured using the hydrostatic weighing method (Pustogvar and Kulyakhtin, 2016) from a density core in the freezer laboratory onboard Polarstern at the temperature of –15°C. Relative volumes of brine and gas were estimated from ice salinity, temperature and density using Cox and Weeks (1983) for cold ice and Leppäranta and Manninen (1988) for ice warmer than –2°C. The data contains the event label (1), time (2), and global coordinates (3,4) of each coring measurement and sample IDs (13, 15). Each salinity core has its manually measured ice thickness (5), ice draft (6), core length (7), and mean snow height (22). Each core section has the total length of its top (8) and bottom (9) measured in situ, as well estimated depth of section top (10), bottom (11), and middle (12). The depth estimates assume that the total length of all core sections is equal to the measured ice thickness. Each core section has the value of its practical salinity (14), isotopic values (16, 17, 18) (Meyer et al., 2000), as well as sea ice temperature (19) and ice density (20) interpolated to the depth of salinity measurements. The global coordinates of coring sites were measured directly. When it was not possible, coordinates of the nearby temperature buoy 2019T66 were used. Ice mass balance buoy 2019T66 installation is described in doi:10.1594/PANGAEA.938134. Brine volume (21) fraction estimates are presented only for fraction values from 0 to 30%. Each core section also has comments (23) describing if the sample is from a false bottom, from rafted ice or has any other special characteristics. Macronutrients from the salinity core, and more isotope data will be published in a subsequent version of this data set.
    Keywords: Arctic; Arctic Ocean; Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic; ARICE; Calculated; Comment; Core length; cores; DATE/TIME; density; Density, ice; Depth, adjusted; Depth, adjusted bottom; Depth, adjusted top; Depth, ice/snow, bottom/maximum; Depth, ice/snow, top/minimum; Deuterium excess; Ecological monitoring; Event label; HAVOC; Hydrostatic weighing; IC; Ice corer; ICEGAUGE; Ice thickness gauge; Isotopic liquid water analyzer; LATITUDE; LONGITUDE; MOSAiC; MOSAiC_ECO; MOSAiC_ICE; MOSAiC20192020; Multidisciplinary drifting Observatory for the Study of Arctic Climate; Physical properties; Polarstern; PS122/1; PS122/1_10-19; PS122/1_5-3; PS122/1_6-34; PS122/1_7-6; PS122/1_7-97; PS122/1_8-2; PS122/1_9-6; PS122/1_9-93; PS122/2; PS122/2_17-3; PS122/2_19-7; PS122/2_21-13; PS122/2_23-3; PS122/2_24-8; PS122/3; PS122/3_32-63; PS122/3_35-11; PS122/3_36-21; PS122/3_38-24; PS122/3_39-7; PS122/4; PS122/4_44-134; PS122/4_46-18; PS122/4_47-16; PS122/4_48-23; PS122/4_49-34; Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean; Salinity; Salinometer, inductive; Sample ID; Sea ice; Sea ice draft; Sea ice salinity; Sea ice thickness; Snow height; Tape measure; Temperature; Temperature, ice/snow; Thermometer; time-series; Volume, brine; δ18O, water; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 7847 data points
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  • 3
    Publication Date: 2024-03-01
    Description: We present sea ice temperature and salinity data from first-year ice (FYI) and second-year ice (SYI) relevant to the temporal development of sea ice permeability and brine drainage efficiency from the early growth phase in October 2019 to the onset of spring warming in May 2020. Our dataset was collected in the central Arctic Ocean during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) Expedition in 2019 to 2020. MOSAiC was an international transpolar drift expedition in which the German icebreaker RV Polarstern anchored into an ice floe to gain new insights into Arctic climate over a full annual cycle. In October 2019, RV Polarstern moored to an ice floe in the Siberian sector of the Arctic at 85 degrees north and 137 degrees east to begin the drift towards the North Pole and the Fram Strait via the Transpolar Drift Stream. The data presented here were collected during the first three legs of the expedition, so all the coring activities took place on the same floe. The end dates of legs 1, 2, and 3 were 13 December, 24 February, and 4 June, respectively. The dataset contributed to a baseline study entitled, Deciphering the properties of different Arctic ice types during the growth phase of the MOSAiC floes: Implications for future studies. The study highlights downward directed gas pathways in FYI and SYI by inferring sea ice permeability and potential brine release from several time series of temperature and salinity measurements. The physical properties presented in this paper lay the foundation for subsequent analyses on actual gas contents measured in the ice cores, as well as air-ice and ice-ocean gas fluxes. Sea ice cores were collected with a Kovacs Mark II 9 cm diameter corer. To measure ice temperatures, about 4.5 cm deep holes were drilled into the core (intervals varied by site and leg) . The temperatures were measured by a digital thermometer within minutes after the cores were retrieved. The ice cores were placed into pre-labelled plastic sleeves sealed at the bottom end. The ice cores were transported to RV Polarstern and stored in a -20 degrees Celsius freezer. Each of the cores was sub-sampled, melted at room temperature, and processed for salinity within one or two days. The practical salinity was estimated by measuring the electrical conductivity and temperature of the melted samples using a WTW Cond 3151 salinometer equipped with a Tetra-Con 325 four-electrode conductivity cell. The practical salinity represents the the salinity estimated from the electrical conductivity of the solution. The dataset also contains derived variables, including sea ice density, brine volume fraction, and the Rayleigh number.
    Keywords: AC3; Arctic Amplification; Arctic Ocean; Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic; ARICE; brine; first-year ice; HAVOC; MOSAiC; MOSAiC_BGC; MOSAiC_ECO; MOSAiC_ICE; MOSAiC_SNOW; MOSAiC20192020; MOSAiC expedition; Multidisciplinary drifting Observatory for the Study of Arctic Climate; Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean; Sea ice; second-year ice; Temperature and Salinity
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 4
    Publication Date: 2024-03-01
    Description: We present sea ice temperature and salinity data from first-year ice (FYI) and second-year ice (SYI) relevant to the temporal development of sea ice permeability and brine drainage efficiency from the early growth phase in October 2019 to the onset of spring warming in May 2020. Our dataset was collected in the central Arctic Ocean during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) Expedition in 2019 to 2020. MOSAiC was an international transpolar drift expedition in which the German icebreaker RV Polarstern anchored into an ice floe to gain new insights into Arctic climate over a full annual cycle. In October 2019, RV Polarstern moored to an ice floe in the Siberian sector of the Arctic at 85 degrees north and 137 degrees east to begin the drift towards the North Pole and the Fram Strait via the Transpolar Drift Stream. The data presented here were collected during the first three legs of the expedition, so all the coring activities took place on the same floe. The end dates of legs 1, 2, and 3 were 13 December, 24 February, and 4 June, respectively. The dataset contributed to a baseline study entitled, Deciphering the properties of different Arctic ice types during the growth phase of the MOSAiC floes: Implications for future studies. The study highlights downward directed gas pathways in FYI and SYI by inferring sea ice permeability and potential brine release from several time series of temperature and salinity measurements. The physical properties presented in this paper lay the foundation for subsequent analyses on actual gas contents measured in the ice cores, as well as air-ice and ice-ocean gas fluxes. Sea ice cores were collected with a Kovacs Mark II 9 cm diameter corer. To measure ice temperatures, about 4.5 cm deep holes were drilled into the core (intervals varied by site and leg) . The temperatures were measured by a digital thermometer within minutes after the cores were retrieved. The ice cores were placed into pre-labelled plastic sleeves sealed at the bottom end. The ice cores were transported to RV Polarstern and stored in a -20 degrees Celsius freezer. Each of the cores was sub-sampled, melted at room temperature, and processed for salinity within one or two days. The practical salinity was estimated by measuring the electrical conductivity and temperature of the melted samples using a WTW Cond 3151 salinometer equipped with a Tetra-Con 325 four-electrode conductivity cell. The practical salinity represents the the salinity estimated from the electrical conductivity of the solution. The dataset also contains derived variables, including sea ice density, brine volume fraction, and the Rayleigh number.
    Keywords: AC3; after Cox & Weeks (1983); Arctic Amplification; Arctic Ocean; Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic; ARICE; brine; DATE/TIME; Density, ice; DEPTH, ice/snow; Estimated from electrical conductivity and temperature of the melted ice samples; Event label; first-year ice; HAVOC; IC; Ice corer; Linear interpolation at the midpoint of the sample based on the measurements from the ice temperature profile; MOSAiC; MOSAiC_BGC; MOSAiC_ECO; MOSAiC_ICE; MOSAiC_SNOW; MOSAiC20192020; MOSAiC expedition; Multidisciplinary drifting Observatory for the Study of Arctic Climate; Polarstern; PS122/1; PS122/1_10-39; PS122/1_11-11; PS122/1_4-29; PS122/1_5-24; PS122/1_6-61; PS122/1_7-78; PS122/1_8-22; PS122/1_9-40; PS122/2; PS122/2_15-12; PS122/2_18-113; PS122/2_20-92; PS122/2_22-77; PS122/3; PS122/3_30-87; PS122/3_31-5; PS122/3_32-58; PS122/3_39-83; Rayleigh number; Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean; Salinity; Sea ice; second-year ice; see comment; Site; Temperature, ice/snow; Temperature and Salinity; Utility; Volume, brine
    Type: Dataset
    Format: text/tab-separated-values, 2163 data points
    Location Call Number Expected Availability
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  • 5
    Publication Date: 2024-03-01
    Description: We present sea ice temperature and salinity data from first-year ice (FYI) and second-year ice (SYI) relevant to the temporal development of sea ice permeability and brine drainage efficiency from the early growth phase in October 2019 to the onset of spring warming in May 2020. Our dataset was collected in the central Arctic Ocean during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) Expedition in 2019 to 2020. MOSAiC was an international transpolar drift expedition in which the German icebreaker RV Polarstern anchored into an ice floe to gain new insights into Arctic climate over a full annual cycle. In October 2019, RV Polarstern moored to an ice floe in the Siberian sector of the Arctic at 85 degrees north and 137 degrees east to begin the drift towards the North Pole and the Fram Strait via the Transpolar Drift Stream. The data presented here were collected during the first three legs of the expedition, so all the coring activities took place on the same floe. The end dates of legs 1, 2, and 3 were 13 December, 24 February, and 4 June, respectively. The dataset contributed to a baseline study entitled, Deciphering the properties of different Arctic ice types during the growth phase of the MOSAiC floes: Implications for future studies. The study highlights downward directed gas pathways in FYI and SYI by inferring sea ice permeability and potential brine release from several time series of temperature and salinity measurements. The physical properties presented in this paper lay the foundation for subsequent analyses on actual gas contents measured in the ice cores, as well as air-ice and ice-ocean gas fluxes. Sea ice cores were collected with a Kovacs Mark II 9 cm diameter corer. To measure ice temperatures, about 4.5 cm deep holes were drilled into the core (intervals varied by site and leg) . The temperatures were measured by a digital thermometer within minutes after the cores were retrieved. The ice cores were placed into pre-labelled plastic sleeves sealed at the bottom end. The ice cores were transported to RV Polarstern and stored in a -20 degrees Celsius freezer. Each of the cores was sub-sampled, melted at room temperature, and processed for salinity within one or two days. The practical salinity was estimated by measuring the electrical conductivity and temperature of the melted samples using a WTW Cond 3151 salinometer equipped with a Tetra-Con 325 four-electrode conductivity cell. The practical salinity represents the the salinity estimated from the electrical conductivity of the solution. The dataset also contains derived variables, including sea ice density, brine volume fraction, and the Rayleigh number.
    Keywords: AC3; after Cox & Weeks (1983); Arctic Amplification; Arctic Ocean; Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic; ARICE; brine; DATE/TIME; Density, ice; DEPTH, ice/snow; Estimated from electrical conductivity and temperature of the melted ice samples; Event label; first-year ice; HAVOC; IC; Ice corer; Linear interpolation at the midpoint of the sample based on the measurements from the ice temperature profile; MOSAiC; MOSAiC_BGC; MOSAiC_ECO; MOSAiC_ICE; MOSAiC_SNOW; MOSAiC20192020; MOSAiC expedition; Multidisciplinary drifting Observatory for the Study of Arctic Climate; Polarstern; PS122/1; PS122/1_6-135; PS122/1_8-37; PS122/2; PS122/2_17-29; PS122/2_19-180; PS122/2_23-65; PS122/3; PS122/3_32-6; PS122/3_37-32; Rayleigh number; Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean; Salinity; Sea ice; second-year ice; see comment; Site; Temperature, ice/snow; Temperature and Salinity; Utility; Volume, brine
    Type: Dataset
    Format: text/tab-separated-values, 1120 data points
    Location Call Number Expected Availability
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  • 6
    Publication Date: 2024-03-01
    Description: We present sea ice temperature and salinity data from first-year ice (FYI) and second-year ice (SYI) relevant to the temporal development of sea ice permeability and brine drainage efficiency from the early growth phase in October 2019 to the onset of spring warming in May 2020. Our dataset was collected in the central Arctic Ocean during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) Expedition in 2019 to 2020. MOSAiC was an international transpolar drift expedition in which the German icebreaker RV Polarstern anchored into an ice floe to gain new insights into Arctic climate over a full annual cycle. In October 2019, RV Polarstern moored to an ice floe in the Siberian sector of the Arctic at 85 degrees north and 137 degrees east to begin the drift towards the North Pole and the Fram Strait via the Transpolar Drift Stream. The data presented here were collected during the first three legs of the expedition, so all the coring activities took place on the same floe. The end dates of legs 1, 2, and 3 were 13 December, 24 February, and 4 June, respectively. The dataset contributed to a baseline study entitled, Deciphering the properties of different Arctic ice types during the growth phase of the MOSAiC floes: Implications for future studies. The study highlights downward directed gas pathways in FYI and SYI by inferring sea ice permeability and potential brine release from several time series of temperature and salinity measurements. The physical properties presented in this paper lay the foundation for subsequent analyses on actual gas contents measured in the ice cores, as well as air-ice and ice-ocean gas fluxes. Sea ice cores were collected with a Kovacs Mark II 9 cm diameter corer. To measure ice temperatures, about 4.5 cm deep holes were drilled into the core (intervals varied by site and leg) . The temperatures were measured by a digital thermometer within minutes after the cores were retrieved. The ice cores were placed into pre-labelled plastic sleeves sealed at the bottom end. The ice cores were transported to RV Polarstern and stored in a -20 degrees Celsius freezer. Each of the cores was sub-sampled, melted at room temperature, and processed for salinity within one or two days. The practical salinity was estimated by measuring the electrical conductivity and temperature of the melted samples using a WTW Cond 3151 salinometer equipped with a Tetra-Con 325 four-electrode conductivity cell. The practical salinity represents the the salinity estimated from the electrical conductivity of the solution. The dataset also contains derived variables, including sea ice density, brine volume fraction, and the Rayleigh number.
    Keywords: AC3; after Cox & Weeks (1983); Arctic Amplification; Arctic Ocean; Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic; ARICE; brine; DATE/TIME; Density, ice; DEPTH, ice/snow; Estimated from electrical conductivity and temperature of the melted ice samples; Event label; first-year ice; HAVOC; IC; Ice corer; Linear interpolation at the midpoint of the sample based on the measurements from the ice temperature profile; MOSAiC; MOSAiC_BGC; MOSAiC_ECO; MOSAiC_ICE; MOSAiC_SNOW; MOSAiC20192020; MOSAiC expedition; Multidisciplinary drifting Observatory for the Study of Arctic Climate; Polarstern; PS122/1; PS122/1_10-69; PS122/1_6-59; PS122/1_7-52; PS122/2; PS122/2_17-124; PS122/2_19-152; PS122/3; PS122/3_31-33; PS122/3_35-151; Rayleigh number; Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean; Salinity; Sea ice; second-year ice; see comment; Site; Snow sampler metal; SSM; Temperature, ice/snow; Temperature and Salinity; Utility; Volume, brine
    Type: Dataset
    Format: text/tab-separated-values, 1575 data points
    Location Call Number Expected Availability
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  • 7
    Publication Date: 2024-03-01
    Description: We present sea ice temperature and salinity data from first-year ice (FYI) and second-year ice (SYI) relevant to the temporal development of sea ice permeability and brine drainage efficiency from the early growth phase in October 2019 to the onset of spring warming in May 2020. Our dataset was collected in the central Arctic Ocean during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) Expedition in 2019 to 2020. MOSAiC was an international transpolar drift expedition in which the German icebreaker RV Polarstern anchored into an ice floe to gain new insights into Arctic climate over a full annual cycle. In October 2019, RV Polarstern moored to an ice floe in the Siberian sector of the Arctic at 85 degrees north and 137 degrees east to begin the drift towards the North Pole and the Fram Strait via the Transpolar Drift Stream. The data presented here were collected during the first three legs of the expedition, so all the coring activities took place on the same floe. The end dates of legs 1, 2, and 3 were 13 December, 24 February, and 4 June, respectively. The dataset contributed to a baseline study entitled, Deciphering the properties of different Arctic ice types during the growth phase of the MOSAiC floes: Implications for future studies. The study highlights downward directed gas pathways in FYI and SYI by inferring sea ice permeability and potential brine release from several time series of temperature and salinity measurements. The physical properties presented in this paper lay the foundation for subsequent analyses on actual gas contents measured in the ice cores, as well as air-ice and ice-ocean gas fluxes. Sea ice cores were collected with a Kovacs Mark II 9 cm diameter corer. To measure ice temperatures, about 4.5 cm deep holes were drilled into the core (intervals varied by site and leg) . The temperatures were measured by a digital thermometer within minutes after the cores were retrieved. The ice cores were placed into pre-labelled plastic sleeves sealed at the bottom end. The ice cores were transported to RV Polarstern and stored in a -20 degrees Celsius freezer. Each of the cores was sub-sampled, melted at room temperature, and processed for salinity within one or two days. The practical salinity was estimated by measuring the electrical conductivity and temperature of the melted samples using a WTW Cond 3151 salinometer equipped with a Tetra-Con 325 four-electrode conductivity cell. The practical salinity represents the the salinity estimated from the electrical conductivity of the solution. The dataset also contains derived variables, including sea ice density, brine volume fraction, and the Rayleigh number.
    Keywords: AC3; AF-MOSAiC-1; AF-MOSAiC-1_22; AF-MOSAiC-1_23; AF-MOSAiC-1_28; after Cox & Weeks (1983); Akademik Fedorov; Arctic Amplification; Arctic Ocean; Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic; ARICE; brine; Comment; DATE/TIME; Density, ice; DEPTH, ice/snow; Estimated from electrical conductivity and temperature of the melted ice samples; Event label; first-year ice; HAVOC; IC; Ice corer; Linear interpolation at the midpoint of the sample based on the measurements from the ice temperature profile; MOSAiC; MOSAiC_BGC; MOSAiC_ECO; MOSAiC_ICE; MOSAiC_SNOW; MOSAiC20192020; MOSAiC20192020, AF122/1; MOSAiC expedition; Multidisciplinary drifting Observatory for the Study of Arctic Climate; PS122/1_3-22; PS122/1_3-23; PS122/1_3-28; Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean; Salinity; Sea ice; second-year ice; see comment; Site; Temperature, ice/snow; Temperature and Salinity; Utility; Volume, brine
    Type: Dataset
    Format: text/tab-separated-values, 115 data points
    Location Call Number Expected Availability
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  • 8
    Publication Date: 2024-03-01
    Description: We present sea ice temperature and salinity data from first-year ice (FYI) and second-year ice (SYI) relevant to the temporal development of sea ice permeability and brine drainage efficiency from the early growth phase in October 2019 to the onset of spring warming in May 2020. Our dataset was collected in the central Arctic Ocean during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) Expedition in 2019 to 2020. MOSAiC was an international transpolar drift expedition in which the German icebreaker RV Polarstern anchored into an ice floe to gain new insights into Arctic climate over a full annual cycle. In October 2019, RV Polarstern moored to an ice floe in the Siberian sector of the Arctic at 85 degrees north and 137 degrees east to begin the drift towards the North Pole and the Fram Strait via the Transpolar Drift Stream. The data presented here were collected during the first three legs of the expedition, so all the coring activities took place on the same floe. The end dates of legs 1, 2, and 3 were 13 December, 24 February, and 4 June, respectively. The dataset contributed to a baseline study entitled, Deciphering the properties of different Arctic ice types during the growth phase of the MOSAiC floes: Implications for future studies. The study highlights downward directed gas pathways in FYI and SYI by inferring sea ice permeability and potential brine release from several time series of temperature and salinity measurements. The physical properties presented in this paper lay the foundation for subsequent analyses on actual gas contents measured in the ice cores, as well as air-ice and ice-ocean gas fluxes. Sea ice cores were collected with a Kovacs Mark II 9 cm diameter corer. To measure ice temperatures, about 4.5 cm deep holes were drilled into the core (intervals varied by site and leg) . The temperatures were measured by a digital thermometer within minutes after the cores were retrieved. The ice cores were placed into pre-labelled plastic sleeves sealed at the bottom end. The ice cores were transported to RV Polarstern and stored in a -20 degrees Celsius freezer. Each of the cores was sub-sampled, melted at room temperature, and processed for salinity within one or two days. The practical salinity was estimated by measuring the electrical conductivity and temperature of the melted samples using a WTW Cond 3151 salinometer equipped with a Tetra-Con 325 four-electrode conductivity cell. The practical salinity represents the the salinity estimated from the electrical conductivity of the solution. The dataset also contains derived variables, including sea ice density, brine volume fraction, and the Rayleigh number.
    Keywords: AC3; after Cox & Weeks (1983); Arctic Amplification; Arctic Ocean; Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic; ARICE; brine; DATE/TIME; Density, ice; DEPTH, ice/snow; Estimated from electrical conductivity and temperature of the melted ice samples; Event label; first-year ice; HAVOC; IC; Ice corer; Linear interpolation at the midpoint of the sample based on the measurements from the ice temperature profile; MOSAiC; MOSAiC_BGC; MOSAiC_ECO; MOSAiC_ICE; MOSAiC_SNOW; MOSAiC20192020; MOSAiC expedition; Multidisciplinary drifting Observatory for the Study of Arctic Climate; Polarstern; PS122/1; PS122/1_10-19; PS122/1_5-3; PS122/1_6-34; PS122/1_7-6; PS122/1_8-2; PS122/1_9-6; PS122/2; PS122/2_17-3; PS122/2_19-7; PS122/2_21-13; PS122/2_23-3; PS122/2_24-8; PS122/3; PS122/3_32-63; PS122/3_35-11; PS122/3_36-21; PS122/3_38-24; PS122/3_39-7; Rayleigh number; Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean; Salinity; Sea ice; second-year ice; see comment; Site; Temperature, ice/snow; Temperature and Salinity; Utility; Volume, brine
    Type: Dataset
    Format: text/tab-separated-values, 2653 data points
    Location Call Number Expected Availability
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  • 9
    Publication Date: 2024-03-01
    Description: We present sea ice temperature and salinity data from first-year ice (FYI) and second-year ice (SYI) relevant to the temporal development of sea ice permeability and brine drainage efficiency from the early growth phase in October 2019 to the onset of spring warming in May 2020. Our dataset was collected in the central Arctic Ocean during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) Expedition in 2019 to 2020. MOSAiC was an international transpolar drift expedition in which the German icebreaker RV Polarstern anchored into an ice floe to gain new insights into Arctic climate over a full annual cycle. In October 2019, RV Polarstern moored to an ice floe in the Siberian sector of the Arctic at 85 degrees north and 137 degrees east to begin the drift towards the North Pole and the Fram Strait via the Transpolar Drift Stream. The data presented here were collected during the first three legs of the expedition, so all the coring activities took place on the same floe. The end dates of legs 1, 2, and 3 were 13 December, 24 February, and 4 June, respectively. The dataset contributed to a baseline study entitled, Deciphering the properties of different Arctic ice types during the growth phase of the MOSAiC floes: Implications for future studies. The study highlights downward directed gas pathways in FYI and SYI by inferring sea ice permeability and potential brine release from several time series of temperature and salinity measurements. The physical properties presented in this paper lay the foundation for subsequent analyses on actual gas contents measured in the ice cores, as well as air-ice and ice-ocean gas fluxes. Sea ice cores were collected with a Kovacs Mark II 9 cm diameter corer. To measure ice temperatures, about 4.5 cm deep holes were drilled into the core (intervals varied by site and leg) . The temperatures were measured by a digital thermometer within minutes after the cores were retrieved. The ice cores were placed into pre-labelled plastic sleeves sealed at the bottom end. The ice cores were transported to RV Polarstern and stored in a -20 degrees Celsius freezer. Each of the cores was sub-sampled, melted at room temperature, and processed for salinity within one or two days. The practical salinity was estimated by measuring the electrical conductivity and temperature of the melted samples using a WTW Cond 3151 salinometer equipped with a Tetra-Con 325 four-electrode conductivity cell. The practical salinity represents the the salinity estimated from the electrical conductivity of the solution. The dataset also contains derived variables, including sea ice density, brine volume fraction, and the Rayleigh number.
    Keywords: AC3; after Cox & Weeks (1983); Arctic Amplification; Arctic Ocean; Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic; ARICE; brine; DATE/TIME; Density, ice; DEPTH, ice/snow; Estimated from electrical conductivity and temperature of the melted ice samples; Event label; first-year ice; HAVOC; IC; Ice corer; Linear interpolation at the midpoint of the sample based on the measurements from the ice temperature profile; MOSAiC; MOSAiC_BGC; MOSAiC_ECO; MOSAiC_ICE; MOSAiC_SNOW; MOSAiC20192020; MOSAiC expedition; Multidisciplinary drifting Observatory for the Study of Arctic Climate; Polarstern; PS122/1; PS122/1_10-16; PS122/1_5-78; PS122/1_6-36; PS122/1_7-9; PS122/1_9-11; PS122/2; PS122/2_20-5; PS122/2_22-7; PS122/2_25-15; PS122/3; PS122/3_33-18; PS122/3_36-4; PS122/3_38-16; PS122/3_39-18; Rayleigh number; Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean; Salinity; Sea ice; second-year ice; see comment; Site; Temperature, ice/snow; Temperature and Salinity; Utility; Volume, brine
    Type: Dataset
    Format: text/tab-separated-values, 2331 data points
    Location Call Number Expected Availability
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  • 10
    Publication Date: 2024-04-24
    Description: Second-year sea-ice thickness, draft, salinity, temperature, and density were measured during near-weekly surveys at the main second-year ice coring site (MCS-SYI) during the MOSAiC expedition (legs 1 to 3) and new second-year ice coring site leg 4, since the earlier site was not accessible any longer. The ice cores were extracted either with a 9-cm (Mark II) or 7.25-cm (Mark III) internal diameter ice corers (Kovacs Enterprise, US). This data set includes data from 18 coring site visits and were performed from 28 October 2019 to 20 July 2020 at coring locations within 50 m to each other in the MOSAiC Central Observatory. During each coring event, ice temperature was measured in situ from a separate temperature core, using Testo 720 thermometers in drill holes with a length of half-core-diameter at 5-cm vertical resolution. Ice bulk practical salinity was measured from melted core sections at 5-cm resolution using a YSI 30 conductivity meter. Ice density was measured using the hydrostatic weighing method (Pustogvar and Kulyakhtin, 2016) from a density core in the freezer laboratory onboard Polarstern at the temperature of –15°C. Relative volumes of brine and gas were estimated from ice salinity, temperature and density using Cox and Weeks (1983) for cold ice and Leppäranta and Manninen (1988) for ice warmer than –2°C. The data contains the event label (1), time (2), and global coordinates (3,4) of each coring measurement and sample IDs (13, 15). Each salinity core has its manually measured ice thickness (5), ice draft (6), core length (7), and mean snow height (22). Each core section has the total length of its top (8) and bottom (9) measured in situ, as well estimated depth of section top (10), bottom (11), and middle (12). The depth estimates assume that the total length of all core sections is equal to the measured ice thickness. Each core section has the value of its practical salinity (14), isotopic values (16, 17, 18) (Meyer et al., 2000), as well as sea ice temperature (19) and ice density (20) interpolated to the depth of salinity measurements. The global coordinates of coring sites were measured directly. When it was not possible, coordinates of the nearby temperature buoy 2019T62 (legs 1-3) or 2019T61 (leg 4) were used. Ice mass balance buoy 2019T62 installation is described in doi:10.1594/PANGAEA.940231, ice mass balance buoy 2020T61 installation is described in doi: 10.1594/PANGAEA.926580. Brine volume (21) fraction estimates are presented only for fraction values from 0 to 30%. Each core section also has comments (23) describing if the sample is from a new coring site or has any other special characteristics. Macronutrients from the salinity core will be published in a subsequent version of this data set.
    Keywords: Arctic; Arctic Ocean; Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic; ARICE; Calculated; Comment; Core length; cores; DATE/TIME; density; Density, ice; Depth, adjusted; Depth, adjusted bottom; Depth, adjusted top; Depth, ice/snow, bottom/maximum; Depth, ice/snow, top/minimum; Deuterium excess; Ecological monitoring; Event label; HAVOC; Hydrostatic weighing; IC; Ice corer; ICEGAUGE; Ice thickness gauge; Isotopic liquid water analyzer; LATITUDE; LONGITUDE; MOSAiC; MOSAiC_ECO; MOSAiC_ICE; MOSAiC20192020; Multidisciplinary drifting Observatory for the Study of Arctic Climate; Physical properties; Polarstern; PS122/1; PS122/1_10-16; PS122/1_5-78; PS122/1_6-36; PS122/1_7-53; PS122/1_7-9; PS122/1_9-11; PS122/2; PS122/2_20-5; PS122/2_22-7; PS122/2_25-15; PS122/3; PS122/3_33-18; PS122/3_35-4; PS122/3_36-4; PS122/3_38-16; PS122/3_39-18; PS122/4; PS122/4_45-29; PS122/4_46-20; PS122/4_47-18; PS122/4_48-25; Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean; Salinity; Temperature; Salinometer, inductive; Sample ID; Sea ice; Sea ice draft; Sea ice salinity; Sea ice thickness; Snow height; Tape measure; Temperature, ice/snow; Thermometer; time-series; Volume, brine; δ18O, water; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 9395 data points
    Location Call Number Expected Availability
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