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WFRF:(Angelopoulus M.)
 

Sökning: WFRF:(Angelopoulus M.) > Physical properties...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00006095nam a2200841 4500
001oai:gup.ub.gu.se/317837
003SwePub
008240528s2022 | |||||||||||000 ||eng|
024a https://gup.ub.gu.se/publication/3178372 URI
024a https://doi.org/10.1594/PANGAEA.9438172 DOI
040 a (SwePub)gu
041 a eng
042 9 SwePub
072 7a vet2 swepub-contenttype
072 7a ovr2 swepub-publicationtype
100a Angelopoulus, M.4 aut
2451 0a Physical properties of sea ice cores from site MCS_FYI measured on legs 1 to 3 of the MOSAiC expedition.
264 1c 2022
520 a 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.
650 7a NATURVETENSKAPx Annan naturvetenskap0 (SwePub)1072 hsv//swe
650 7a NATURAL SCIENCESx Other Natural Sciences0 (SwePub)1072 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
653 a Arctic Ocean; brine; first-year ice; MOSAiC20192020; MOSAiC_BGC; MOSAiC_ECO; MOSAiC expedition; MOSAiC_ICE; MOSAiC_SNOW; Sea ice; second-year ice; Temperature and Salinity
700a Abrahamsson, Katarina,d 1957u Gothenburg University,Göteborgs universitet,Institutionen för marina vetenskaper,Department of marine sciences4 aut0 (Swepub:gu)xabrak
700a Bauch, D.4 aut
700a Bowman, J.4 aut
700a Castellani, G.4 aut
700a Creamean, J.4 aut
700a Damm, E.4 aut
700a Divine, D.4 aut
700a Dumitrascu, Adelau Gothenburg University,Göteborgs universitet,Institutionen för marina vetenskaper,Department of marine sciences4 aut
700a Eggers, L.4 aut
700a Fong, A.4 aut
700a Fons, S.W.4 aut
700a Gradinger, R.4 aut
700a Granskog, M.A.4 aut
700a Grosse, J.4 aut
700a Happala, J.4 aut
700a Haas, C.4 aut
700a Hoppe, C.J.M.4 aut
700a Hoyland, K.V.4 aut
700a Immerz, A.4 aut
700a Kolabutin, N.4 aut
700a Krumpen, T.4 aut
700a Lei, R.4 aut
700a Marsay, C.M.4 aut
700a Maus, S.4 aut
700a Nicolaus, M.4 aut
700a Nubom, A.4 aut
700a Oggier, M.4 aut
700a Olsen, L.M.4 aut
700a Rember, R.4 aut
700a Ren, J.4 aut
700a Rinke, A.4 aut
700a Sachs, T.4 aut
700a Sheikin, I.4 aut
700a Shimanchuk, E.4 aut
700a Simões Pereira, Patricu Gothenburg University,Göteborgs universitet,Institutionen för marina vetenskaper,Department of marine sciences4 aut0 (Swepub:gu)xsimpa
700a Spahic, S.4 aut
700a Stefels, J.4 aut
700a Stephens, M.4 aut
700a Torres-Valdes, S.4 aut
700a Torstensson, A.4 aut
700a Ulfsbo, Adam,d 1985u Gothenburg University,Göteborgs universitet,Institutionen för marina vetenskaper,Department of marine sciences4 aut0 (Swepub:gu)xulfad
700a Verdugo, J.4 aut
700a Wang, L.4 aut
700a Wischnewski, L.4 aut
700a Zhan, L.4 aut
710a Göteborgs universitetb Institutionen för marina vetenskaper4 org
773t PANGAEA
8564 8u https://gup.ub.gu.se/publication/317837
8564 8u https://doi.org/10.1594/PANGAEA.943817

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