scholarly journals The role of mesoscale eddies in the spread of freshwaters in the surface layer of the Arctic Ocean

2016 ◽  
Vol 61 (3) ◽  
pp. 106-117
Author(s):  
Dmitriy V. Kondrik ◽  
◽  
Andrey V. Popov ◽  
Andrey V. Rubchenya ◽  
◽  
...  
2021 ◽  
Author(s):  
Rajka Juhrbandt ◽  
Suvarchal Cheedela ◽  
Nikolay Koldunov ◽  
Thomas Jung

<p>The recently completed Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) can serve as reference to evaluate current and future ocean state of the Arctic Ocean. With this premise, we perform a virtual MOSAiC expedition in historical and ssp370-scenario experiments in data generated by CMIP6 models.<br><br>The timespan covered ranges from preindustrial times (1851-1860) through present-day up to a 4K world (2091-2100). Early results using AWI-CM model, suggest that for scenario simulations a thinning of the colder surface layer and a warming of the layer between 200 and 1200 m along the MOSAiC path can be expected, while there is no significant change in temperature below this depth. Results from other models will be presented.<br><br>The Python-centric tool used for the analysis simplifies preprocessing of a pool of CMIP6 data and selecting data on space-time trajectory. It exposes an interface that is agnostic to underlying model or its grid type. Code snippets are presented along to demonstrate the tool's ease of use with a hope to inspire such virtual field campaigns using other past observations or arbitrary trajectories.</p>


2012 ◽  
Vol 47 (2) ◽  
pp. 923-931 ◽  
Author(s):  
James M. Armitage ◽  
Sung-Deuk Choi ◽  
Torsten Meyer ◽  
Trevor N. Brown ◽  
Frank Wania

2019 ◽  
Author(s):  
Susanne Kraemer ◽  
Arthi Ramachandran ◽  
David Colatriano ◽  
Connie Lovejoy ◽  
David A. Walsh

AbstractThe Arctic Ocean is relatively isolated from other oceans and consists of strongly stratified water masses with distinct histories, nutrient, temperature and salinity characteristics, therefore providing an optimal environment to investigate local adaptation. The globally distributed SAR11 bacterial group consists of multiple ecotypes that are associated with particular marine environments, yet relatively little is known about Arctic SAR11 diversity. Here, we examined SAR11 diversity using ITS analysis and metagenome-assembled genomes (MAGs). Arctic SAR11 assemblages were comprised of the S1a, S1b, S2, and S3 clades, and structured by water mass and depth. The fresher surface layer was dominated by an ecotype (S3-derived P3.2) previously associated with Arctic and brackish water. In contrast, deeper waters of Pacific origin were dominated by the P2.3 ecotype of the S2 clade, within which we identified a novel subdivision (P2.3s1) that was rare outside the Arctic Ocean. Arctic S2-derived SAR11 MAGs were restricted to high latitudes and included MAGs related to the recently defined S2b subclade, a finding consistent with bi-polar ecotypes and Arctic endemism. These results place the stratified Arctic Ocean into the SAR11 global biogeography and have identified SAR11 lineages for future investigation of adaptive evolution in the Arctic Ocean.


2019 ◽  
Vol 177 ◽  
pp. 201-212 ◽  
Author(s):  
Igor Niezgodzki ◽  
Jarosław Tyszka ◽  
Gregor Knorr ◽  
Gerrit Lohmann

2019 ◽  
Vol 53 (22) ◽  
pp. 13136-13145 ◽  
Author(s):  
Luis M. Laglera ◽  
Camila Sukekava ◽  
Hans A. Slagter ◽  
Javier Downes ◽  
Alberto Aparicio-Gonzalez ◽  
...  

2013 ◽  
Vol 67 ◽  
pp. 8-13 ◽  
Author(s):  
Xin He ◽  
Liguang Sun ◽  
Zhouqing Xie ◽  
Wen Huang ◽  
Nanye Long ◽  
...  

2018 ◽  
Author(s):  
Andrey Pnyushkov ◽  
Igor V. Polyakov ◽  
Laurie Padman ◽  
An T. Nguyen

Abstract. Heat fluxes steered by mesoscale eddies may be a significant (but still not quantified) source of heat to the surface mixed layer and sea ice cover in the Arctic Ocean, as well as a source of nutrients for enhancing seasonal productivity in the near-surface layers. Here we use four years (2007–2011) of velocity and hydrography records from a moored profiler over the Laptev Sea slope, and 15 months (2008–2009) of acoustic Doppler current profiler data from a nearby mooring, to investigate the structure and dynamics of eddies at the continental margin of the eastern Eurasian Basin. Typical eddy scales are radii of order of 10 km, heights of six hundred meters, and maximum velocities of ~ 0.1 m s −1. Eddies are approximately equally divided between cyclonic and anticyclonic polarizations, contrary to prior observations from the deep basins and along the Lomonosov Ridge. Eddies are present in the mooring records about 20–25 % of the time, taking about one week to pass through the mooring at an average frequency of about one eddy per month. We found the eddies observed are formed in two distinct regions–near Fram Strait, where the western branch of Atlantic Water (AW) enters the Arctic Ocean, and near Severnaya Zemlya, where the Fram Strait and Barents Sea branches of the AW inflow merge. These eddies, embedded in the Arctic Circumpolar Boundary Current, carry anomalous water properties along the eastern Arctic continental slope. The enhanced diapycnal mixing that we found within EB eddies suggests a potentially important role for eddies in the vertical redistribution of heat in the Arctic Ocean interior.


Author(s):  
Mary C. O’Brien ◽  
Humfrey Melling ◽  
Thomas F. Pedersen ◽  
Robie W. Macdonald

2010 ◽  
Vol 44 (22) ◽  
pp. 8422-8428 ◽  
Author(s):  
Xiaoguo Wu ◽  
James C. W. Lam ◽  
Chonghuan Xia ◽  
Hui Kang ◽  
Liguang Sun ◽  
...  

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