Articles | Volume 15, issue 4
https://doi.org/10.5194/tc-15-2083-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-15-2083-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Early spring subglacial discharge plumes fuel under-ice primary production at a Svalbard tidewater glacier
Tobias Reiner Vonnahme
CORRESPONDING AUTHOR
Department of Arctic and Marine Biology, UiT The Arctic University
of Norway, Tromsø, Norway
Emma Persson
Department of Arctic and Marine Biology, UiT The Arctic University
of Norway, Tromsø, Norway
Ulrike Dietrich
Department of Arctic and Marine Biology, UiT The Arctic University
of Norway, Tromsø, Norway
Eva Hejdukova
Department of Ecology, Faculty of Science, Charles University,
Prague, Czech Republic
Christine Dybwad
Department of Arctic and Marine Biology, UiT The Arctic University
of Norway, Tromsø, Norway
Josef Elster
Centre for Polar Ecology, University of South Bohemia, České Budějovice, Czech Republic
Institute of Botany ASCR, Třeboň, Czech Republic
Melissa Chierici
Institute of Marine Research, Tromsø, Norway
University Centre in Svalbard (UNIS), Longyearbyen, Svalbard
Rolf Gradinger
Department of Arctic and Marine Biology, UiT The Arctic University
of Norway, Tromsø, Norway
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Discipline: Other | Subject: Arctic (e.g. Greenland)
Characterizing southeast Greenland fjord surface ice and freshwater flux to support biological applications
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Arctic freshwater fluxes: sources, tracer budgets and inconsistencies
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Twila A. Moon, Benjamin Cohen, Taryn E. Black, Kristin L. Laidre, Harry L. Stern, and Ian Joughin
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The complex geomorphology of southeast Greenland (SEG) creates dynamic fjord habitats for top marine predators, featuring glacier-derived floating ice, pack and landfast sea ice, and freshwater flux. We study the physical environment of SEG fjords, focusing on surface ice conditions, to provide a regional characterization that supports biological research. As Arctic warming persists, SEG may serve as a long-term refugium for ice-dependent wildlife due to the persistence of regional ice sheets.
Tingfeng Dou, Cunde Xiao, Jiping Liu, Qiang Wang, Shifeng Pan, Jie Su, Xiaojun Yuan, Minghu Ding, Feng Zhang, Kai Xue, Peter A. Bieniek, and Hajo Eicken
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Rain-on-snow (ROS) events can accelerate the surface ablation of sea ice, greatly influencing the ice–albedo feedback. We found that spring ROS events have shifted to earlier dates over the Arctic Ocean in recent decades, which is correlated with sea ice melt onset in the Pacific sector and most Eurasian marginal seas. There has been a clear transition from solid to liquid precipitation, leading to a reduction in spring snow depth on sea ice by more than −0.5 cm per decade since the 1980s.
Alexander Forryan, Sheldon Bacon, Takamasa Tsubouchi, Sinhué Torres-Valdés, and Alberto C. Naveira Garabato
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We compare control volume and geochemical tracer-based methods of estimating the Arctic Ocean freshwater budget and find both methods in good agreement. Inconsistencies arise from the distinction between
Atlanticand
Pacificwaters in the geochemical calculations. The definition of Pacific waters is particularly problematic due to the non-conservative nature of the nutrients underpinning the definition and the low salinity characterizing waters entering the Arctic through Bering Strait.
Felix L. Müller, Claudia Wekerle, Denise Dettmering, Marcello Passaro, Wolfgang Bosch, and Florian Seitz
The Cryosphere, 13, 611–626, https://doi.org/10.5194/tc-13-611-2019, https://doi.org/10.5194/tc-13-611-2019, 2019
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Knowledge of the dynamic ocean topography (DOT) enables studying changes of ocean surface currents. The DOT can be derived by satellite altimetry measurements or by models. However, in polar regions, altimetry-derived sea surface heights are affected by sea ice. Model representations are consistent but impacted by the underlying functional backgrounds and forcing models. The present study compares results from both data sources in order to investigate the potential for a combination of the two.
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Short summary
We describe the impact of subglacial discharge in early spring on a sea-ice-covered fjord on Svalbard by comparing a site influenced by a shallow tidewater glacier with two reference sites. We found a moderate under-ice phytoplankton bloom at the glacier front, which we attribute to subglacial upwelling of nutrients; a strongly stratified surface layer; and higher light penetration. In contrast, sea ice algae biomass was limited by low salinities and brine volumes.
We describe the impact of subglacial discharge in early spring on a sea-ice-covered fjord on...