scholarly journals The future Barents Sea, risks, mitigation and adaptation options

Author(s):  
Benjamin Planque ◽  
Per Arneberg ◽  
Mette Skern-Mauritzen ◽  
Tor Eldevik ◽  
Nina Mikkelsen

A joint workshop by the Nansen Legacy and Barents Risk projects, to explore the possible states of the Barents Sea by the horizon 2050, the associated risks and the possible ways to mitigate or adapt to them.

Author(s):  
Felipe S. Freitas ◽  
Katharine R. Hendry ◽  
Sian F. Henley ◽  
Johan C. Faust ◽  
Allyson C. Tessin ◽  
...  

The Barents Sea is experiencing long-term climate-driven changes, e.g. modification in oceanographic conditions and extensive sea ice loss, which can lead to large, yet unquantified disruptions to ecosystem functioning. This key region hosts a large fraction of Arctic primary productivity. However, processes governing benthic and pelagic coupling are not mechanistically understood, limiting our ability to predict the impacts of future perturbations. We combine field observations with a reaction-transport model approach to quantify organic matter (OM) processing and disentangle its drivers. Sedimentary OM reactivity patterns show no gradients relative to sea ice extent, being mostly driven by seafloor spatial heterogeneity. Burial of high reactivity, marine-derived OM is evident at sites influenced by Atlantic Water (AW), whereas low reactivity material is linked to terrestrial inputs on the central shelf. Degradation rates are mainly driven by aerobic respiration (40–75%), being greater at sites where highly reactive material is buried. Similarly, ammonium and phosphate fluxes are greater at those sites. The present-day AW-dominated shelf might represent the future scenario for the entire Barents Sea. Our results represent a baseline systematic understanding of seafloor geochemistry, allowing us to anticipate changes that could be imposed on the pan-Arctic in the future if climate-driven perturbations persist. This article is part of the theme issue ‘The changing Arctic Ocean: consequences for biological communities, biogeochemical processes and ecosystem functioning’.


Author(s):  
Valeriy G. Yakubenko ◽  
Anna L. Chultsova

Identification of water masses in areas with complex water dynamics is a complex task, which is usually solved by the method of expert assessments. In this paper, it is proposed to use a formal procedure based on the application of the method of optimal multiparametric analysis (OMP analysis). The data of field measurements obtained in the 68th cruise of the R/V “Academician Mstislav Keldysh” in the summer of 2017 in the Barents Sea on the distribution of temperature, salinity, oxygen, silicates, nitrogen, and phosphorus concentration are used as a data for research. A comparison of the results with data on the distribution of water masses in literature based on expert assessments (Oziel et al., 2017), allows us to conclude about their close structural similarity. Some differences are related to spatial and temporal shifts of measurements. This indicates the feasibility of using the OMP analysis technique in oceanological studies to obtain quantitative data on the spatial distribution of different water masses.


1990 ◽  
Vol 8 (1) ◽  
pp. 11-16 ◽  
Author(s):  
Lars Midttun

1997 ◽  
Vol 16 (2) ◽  
pp. 73-84 ◽  
Author(s):  
Robert T. Barrett ◽  
Vidar Bakken ◽  
Juri V. Krasnov

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