Ridge ice temperature, salinity, oxygen and hydrogen isotope composition data MOSAiC Leg 4 (PS122/4) ...

Temperature, salinity, and isotopic values data from sea ice samples taken during MOSAiC leg 4 (PS122/4). Sea ice samples were taken from Jaridge, Alli's Ridge, and the Remote Sensing site. The ice cores were extracted either with a 9-cm (Mark II) or 7.25-cm (Mark III) internal diameter ice cor...

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Bibliographic Details
Main Authors: Salganik, Evgenii, Lange, Benjamin Allen, Müller, Oliver, Sheikin, Igor, Balmonte, John Paul, Høyland, Knut Vilhelm, Granskog, Mats A
Format: Dataset
Language:English
Published: PANGAEA 2024
Subjects:
isotope composition
Mosaic
pressure ridges
Salinity
Sea ice
Temperate
Event label
DATE/TIME
LATITUDE
LONGITUDE
Site
Distance, relative, X
Distance, relative, Y
Sea ice thickness
Sea ice draft
Snow height
Core length
DEPTH, ice/snow
Material
Temperature, ice/snow
Sea ice salinity
δ Deuterium, water
δ18O, water
Volume, brine
Ice corer
PS122/4
Polarstern
Multidisciplinary drifting Observatory for the Study of Arctic Climate MOSAiC
Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean HAVOC
Arctic
Arctic Ocean
Leppäranta
Manninen
Online Access:https://dx.doi.org/10.1594/pangaea.964522
https://doi.pangaea.de/10.1594/PANGAEA.964522
Description
Summary:Temperature, salinity, and isotopic values data from sea ice samples taken during MOSAiC leg 4 (PS122/4). Sea ice samples were taken from Jaridge, Alli's Ridge, and the Remote Sensing site. 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). 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 5–20 cm vertical resolution. Salinity ice cores were stored in sterile U-Lines bags and transported back to the ship within 2 hours of sampling. Ice bulk practical salinity was measured from melted core sections at 5 cm resolution using a YSI 30 conductivity meter (practical salinity scale, unitless). The relative volume of brine was estimated from ice salinity and temperature 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), ...

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