Oxygen and hydrogen isotopic ratios from sea ice bottom, false bottom ice, under-ice meltwater layer and surface melt pond samples collected during MOSAiC leg 4 (PS122.4) ...

Oxygen and hydrogen isotopic ratio samples were collected from sea ice and water samples. Coring and sampling were completed at six locations on July 25 for measurement of salinity and stable oxygen isotopic composition to better understand the meltwater sources for under-ice meltwater and false bot...

Full description

Bibliographic Details
Main Authors: Lange, Benjamin Allen, Granskog, Mats A, Meyer, Hanno, Bauch, Dorothea, Smith, Madison M, von Albedyll, Luisa, Raphael, Ian, Matero, Ilkka, Salganik, Evgenii
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
isotope composition
melt pond
Meltwater
MOSAiC20192020
oxygen and hydrogen isotopes
Sea ice
Gear
LATITUDE
LONGITUDE
Location
DATE/TIME
Sample ID
Salinity
Description
DEPTH, ice/snow
δ18O, water
δ Deuterium, water
DISTANCE
Core length
False bottom pucks
Comment
Ice corer
Mass spectrometer Finnigan MAT Delta-S ISOLAB
PS122/4
Polarstern
Multidisciplinary drifting Observatory for the Study of Arctic Climate MOSAiC
Polar Terrestrial Environmental Systems @ AWI AWI_Envi
Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean HAVOC
Arctic Ocean
ice core
Online Access:https://dx.doi.org/10.1594/pangaea.943734
https://doi.pangaea.de/10.1594/PANGAEA.943734
Description
Summary:Oxygen and hydrogen isotopic ratio samples were collected from sea ice and water samples. Coring and sampling were completed at six locations on July 25 for measurement of salinity and stable oxygen isotopic composition to better understand the meltwater sources for under-ice meltwater and false bottoms. Cores were collected using a corer (9 cm inner diameter; Mark II coring system, Kovacs Enterprises, US), and ice samples were collected from the bottom 10 centimeters of the ice core in 5 cm increments (0-5 and 5-10 cm above the bottom) and from the false bottom ice. Under-ice meltwater layer samples and water from directly below the false bottom were collected using a peristaltic pump. In order to minimize contamination from coring activities, under-ice meltwater samples from the meltwater layer in the void space between ice and false bottom were collected prior to coring through the false bottom. Surface melt pond water samples were collected by dipping plastic sample cups (rinsed with milliQ water) in the ...

Similar Items