Methane concentration and its isotopic composition within sea ice during POLARSTERN cruise PS106/1 (ARK-XXXI/1.1)

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Hauptverfasser: Verdugo, Josefa, Damm, Ellen
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2021
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author Verdugo, Josefa
Damm, Ellen
author_facet Verdugo, Josefa
Damm, Ellen
collection Datos científicos de ciencias marinas y ambientales
contents The methane concentration and stable carbon isotopic signature of methane were measured in different Arctic sea ice types as well as in seawater underneath the ice floe during the Polarstern expedition PS106.1. The ice drift took place between 4 - 15 June 2017, north of Svalbard (Macke and Flores, 2018). Sea ice cores were collected using a Kovacs Mark II 9cm drill ice corer. In all ice stations, the first ice core was used for in situ ice temperature measurements, and the second one for methane concentration, stable carbon isotopic signature of methane, bulk ice salinity and nutrient concentrations (Verdugo et al., 2021). Seawater samples were collected using a shipboard Sea-Bird Scientific SBE 911plus CTD (conductivity–temperature– depth) profiler equipped with ancillary sensors and integrated with a SBE32 CarouselWater Sampler with 24 Niskin bottles of 12L each (Macke and Flores, 2018).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_937078
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Methane concentration and its isotopic composition within sea ice during POLARSTERN cruise PS106/1 (ARK-XXXI/1.1)
Verdugo, Josefa
Damm, Ellen
Arctic; Arctic Ocean; ARK-XXXI/1.1,PASCAL; DATE/TIME; DEPTH, ice/snow; Event label; ICE; Ice station; Identification; Latitude of event; Longitude of event; Methane; Methane concentration; Polarstern; PS106_21-2; PS106_22-1; PS106_25-1; PS106_26-2; PS106_27-1; PS106_28-2; PS106_29-2; PS106_31-2; PS106/1; Sea ice; Sea ice salinity; seawater; stable carbon isotopic composition of methane; Temperature, ice/snow; δ13C, methane
The methane concentration and stable carbon isotopic signature of methane were measured in different Arctic sea ice types as well as in seawater underneath the ice floe during the Polarstern expedition PS106.1. The ice drift took place between 4 - 15 June 2017, north of Svalbard (Macke and Flores, 2018). Sea ice cores were collected using a Kovacs Mark II 9cm drill ice corer. In all ice stations, the first ice core was used for in situ ice temperature measurements, and the second one for methane concentration, stable carbon isotopic signature of methane, bulk ice salinity and nutrient concentrations (Verdugo et al., 2021). Seawater samples were collected using a shipboard Sea-Bird Scientific SBE 911plus CTD (conductivity–temperature– depth) profiler equipped with ancillary sensors and integrated with a SBE32 CarouselWater Sampler with 24 Niskin bottles of 12L each (Macke and Flores, 2018).
title Methane concentration and its isotopic composition within sea ice during POLARSTERN cruise PS106/1 (ARK-XXXI/1.1)
topic Arctic; Arctic Ocean; ARK-XXXI/1.1,PASCAL; DATE/TIME; DEPTH, ice/snow; Event label; ICE; Ice station; Identification; Latitude of event; Longitude of event; Methane; Methane concentration; Polarstern; PS106_21-2; PS106_22-1; PS106_25-1; PS106_26-2; PS106_27-1; PS106_28-2; PS106_29-2; PS106_31-2; PS106/1; Sea ice; Sea ice salinity; seawater; stable carbon isotopic composition of methane; Temperature, ice/snow; δ13C, methane
url https://doi.org/10.1594/PANGAEA.937078