2022
DOI: 10.5194/essd-2022-66
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Mesoscale observations of temperature and salinity in the Arctic Transpolar Drift: a high-resolution dataset from the MOSAiC Distributed Network

Abstract: Abstract. Measurements targeting mesoscale and submesoscale processes in the ice-covered part of the Arctic Ocean are sparse in all seasons. As a result, there are significant knowledge gaps with respect to these processes, in particular related to the role of eddies and fronts in the coupled ocean–atmosphere–sea ice system. Here we present a unique observational dataset of upper ocean temperature and salinity collected by a set of buoys installed on ice floes as part of the Multidisciplinary drifting Observator… Show more

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Cited by 13 publications
(3 citation statements)
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“…The transmission interval was set to 10 minutes. A more detailed description of the buoy is given in Hoppmann, 2022 55 . The data of this buoy are available online at https://data.meereisportal.de/ 56 and are currently being archived in PANGAEA.…”
Section: Ctd Buoymentioning
confidence: 99%
“…The transmission interval was set to 10 minutes. A more detailed description of the buoy is given in Hoppmann, 2022 55 . The data of this buoy are available online at https://data.meereisportal.de/ 56 and are currently being archived in PANGAEA.…”
Section: Ctd Buoymentioning
confidence: 99%
“…The sensor stability rating is 0.003 mS cm −1 and 0.0002 per month for conductivity and temperature, respectively, with a yearly rating of 0.05% of the full scale for pressure. The detailed description of the instruments and the data obtained are given by Hoppmann et al (2022). We further, used data from three Ice-tethered profilers (ITP; Toole and Krishfield, 2016).…”
Section: Observational Datamentioning
confidence: 99%
“…Moreover, the looping of the DN drift trajectory and the intersection of the trajectories of different buoys add complexity to the observed data. Nevertheless, using relatively simple data analysis methods, several mesoscale eddies were identified in the Amundsen Basin (Hoppmann et al, 2022;Fang et al, 2023 (submitted;Quintanilla-Zurita and et al, (in prep.). However, these methods have limitations in showing the overall 3D picture, as the buoy measurements can be complex to analyze spatially, due to the above mentioned complex drift trajectories.…”
Section: Introductionmentioning
confidence: 99%