Data Description

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Roeske, T et al. (2012): Barium measured on water bottle samples during POLARSTERN cruise ARK-XXII/2 (SPACE). Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research, Bremerhaven, doi:10.1594/PANGAEA.758745,
Supplement to: Roeske, Tobias; Bauch, Dorothea; Rutgers van der Loeff, Michiel M; Rabe, Benjamin (2012): Utility of dissolved barium in distinguishing North American from Eurasian runoff in the Arctic Ocean. Marine Chemistry, 132-133, 1-14, doi:10.1016/j.marchem.2012.01.007
Dissolved barium has been shown to have the potential to distinguish Eurasian from North American (NA) river runoff. As part of the ARK-XXII/2 Polarstern expedition in summer 2007, Ba was analyzed in the Barents, Kara, Laptev seas, and the Eurasian Basins as well as the Makarov Basin up to the Alpha and Mendeleyev Ridges. By combining salinity, d18O and initial phosphate corrected for mineralization with oxygen (PO4*) or N/P ratios we identified the water mass fractions of meteoric water, sea ice meltwater, and marine waters of Atlantic as well as Pacific origin in the upper water column. In all basins inside the lower halocline layer and the Arctic intermediate waters we find Ba concentrations close to those of the Fram Strait branch of the lower halocline (41-45 nM), reflecting the composition of the incoming Atlantic water. A layer of upper halocline water (UHW) with higher Ba concentrations (45-55 nM) is identified in the Makarov Basin. Atop of the UHW, the Surface Mixed Layer (SML), including the summer and winter mixed layers, has high concentrations of Ba (58-67 nM). In the SML of the investigated area of the central Arctic the meteoric fraction can be identified by assuming a conservative behavior of Ba to be primarily of Eurasian river origin. However, in productive coastal regions biological removal compromises the use of Ba to distinguish between Eurasian and NA rivers. As a consequence, the NA river water fraction is underestimated in productive surface waters or waters that have passed a productive region, whereas this fraction is overestimated in subsurface waters containing remineralised Ba, particularly when these waters have passed productive shelf regions. Especially in the Laptev Sea and small regions in the Barents Sea, Ba concentrations are low in surface waters. In the Laptev Sea exceptionally high Ba concentrations in shelf bottom waters indicate that Ba is removed from surface waters to deep waters by biological activity enhanced by increasing ice-free conditions as well as by scavenging by organic matter of terrestrial origin. We interpret high Ba concentrations in the UHW of the Makarov Basin to result from enrichment by remineralisation in bottom waters on the shelf of the Chukchi Sea and therefore the calculated NA runoff is an artefact. We conclude that no NA runoff can be demonstrated unequivocally anywhere during our expedition with the set of tracers considered here. Small contributions of NA runoff may have been masked by Ba depletion and could only be resolved by supportive tracers on the uptake history. We thus suggest that Ba has to be used with care as it can put limits but not yield quantitative water mass distributions. Only if the extra Ba inputs exceed the cumulative biological uptake the signal can be unequivocally attributed to NA runoff.
Related to:
Roeske, Tobias; Rutgers van der Loeff, Michiel M; Middag, Rob; Bakker, Karel (2012): Deep water circulation and composition in the Arctic Ocean by dissolved barium, aluminium and silicate. Marine Chemistry, 132-133, 56-67, doi:10.1016/j.marchem.2012.02.001 *
Median Latitude: 83.054391 * Median Longitude: 99.437541 * South-bound Latitude: 75.000500 * West-bound Longitude: 33.950100 * North-bound Latitude: 88.667500 * East-bound Longitude: -135.034800
Date/Time Start: 2007-07-30T10:14:00 * Date/Time End: 2007-09-23T22:42:00
Minimum DEPTH, water: 3.8 m * Maximum DEPTH, water: 5200.6 m
PS70/228-1 * * Latitude: 75.000500 * Longitude: 34.000000 * Date/Time: 2007-07-30T10:14:00 * Elevation: -178.0 m * Location: Arctic Ocean * * Campaign: ARK-XXII/2 (PS70 SPACE DAMOCLES) * * Basis: Polarstern * * Device: CTD/Rosette, ultra clean (CTD-UC) *
PS70/236-1 * * Latitude: 77.500800 * Longitude: 33.986600 * Date/Time: 2007-07-31T07:47:00 * Elevation: -190.0 m * Location: Arctic Ocean * * Campaign: ARK-XXII/2 (PS70 SPACE DAMOCLES) * * Basis: Polarstern * * Device: CTD/Rosette, ultra clean (CTD-UC) *
PS70/237-1 * * Latitude: 78.997200 * Longitude: 33.989800 * Date/Time: 2007-07-31T18:35:00 * Elevation: -275.0 m * Location: Arctic Ocean * * Campaign: ARK-XXII/2 (PS70 SPACE DAMOCLES) * * Basis: Polarstern * * Device: CTD/Rosette, ultra clean (CTD-UC) *
#NameShort NameUnitPrincipal InvestigatorMethodComment
1Event label *EventMetadata
2DATE/TIME *Date/TimeGeocode
3LATITUDE *LatitudeGeocode
4LONGITUDE *LongitudeGeocode
5Elevation of event *ElevationmMetadata
6DEPTH, water *Depth watermGeocode
7Barium *Baµmol/lRoeske, Tobias *ID-ICP-MS, Isotope dilution - inductively coupled plasma - mass spectrometry *
8Barium, standard deviation *Ba std dev±Roeske, Tobias *ID-ICP-MS, Isotope dilution - inductively coupled plasma - mass spectrometry *
9Bottle number *BottleRoeske, Tobias *
1338 data points

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