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Observations of Seasonal Upwelling and Downwelling in the Beaufort Sea Mediated by Sea Ice

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TLDR
In this paper, the authors presented observational estimates of Ekman pumping in the Beaufort Gyre region Averaged over the Canada Basin, the results show a 2003-14 average of 23m yr−1 downward with strong seasonal and interannual variability superimposed: monthly and yearly means range from 30 m yr− 1 downward to 10 m yr −1 upward.
Abstract
We present observational estimates of Ekman pumping in the Beaufort Gyre region Averaged over the Canada Basin, the results show a 2003–14 average of 23 m yr−1 downward with strong seasonal and interannual variability superimposed: monthly and yearly means range from 30 m yr−1 downward to 10 m yr−1 upward A clear, seasonal cycle is evident with intense downwelling in autumn and upwelling during the winter months, despite the wind forcing being downwelling favorable year-round Wintertime upwelling is associated with friction between the large-scale Beaufort Gyre ocean circulation and the surface ice pack and contrasts with previous estimates of yearlong downwelling; as a consequence, the yearly cumulative Ekman pumping over the gyre is significantly reduced The spatial distribution of Ekman pumping is also modified, with the Beaufort Gyre region showing alternating, moderate upwelling and downwelling, while a more intense, yearlong downwelling averaging 18 m yr−1 is identified in the northern

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Understanding Arctic Ocean Circulation: A Review of Ocean Dynamics in a Changing Climate

TL;DR: In this paper, the authors present a synthesis of observational data interpreted from the perspective of geophysical fluid dynamics (GFD) and explore the specific drivers of these systems, including wind forcing, ice-ocean interactions and surface buoyancy fluxes.
Journal ArticleDOI

Warming of the interior Arctic Ocean linked to sea ice losses at the basin margins

TL;DR: It is shown that the solar heating, considered together with subduction rates of surface water in this region, is sufficient to account for the observed halocline warming, and heat absorption at the basin margins and its subsequent accumulation in the ocean interior have consequences for Beaufort Gyre sea ice beyond the summer season.
Journal ArticleDOI

The Ice‐Ocean Governor: Ice‐Ocean Stress Feedback Limits Beaufort Gyre Spin‐Up

TL;DR: In this paper, a regulator is described that limits spin up and explains the bilization of the sea-ice covered Beaufort Gyre, even while subject to sustained anticyclonic 12 wind-stress curl.
References
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Journal ArticleDOI

The NCEP/NCAR 40-Year Reanalysis Project

TL;DR: The NCEP/NCAR 40-yr reanalysis uses a frozen state-of-the-art global data assimilation system and a database as complete as possible, except that the horizontal resolution is T62 (about 210 km) as discussed by the authors.
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Beaufort Gyre freshwater reservoir: State and variability from observations

TL;DR: In this paper, the authors investigated basin-scale mechanisms regulating anomalies in freshwater content (FWC) in the Beaufort Gyre (BG) of the Arctic Ocean using historical observations and data collected in 2003-2007.
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Arctic sea ice circulation and drift speed: Decadal trends and ocean currents

TL;DR: In this paper, the authors examined the basinwide trends in sea ice circulation and drift speed and highlighted the changes between 1982 and 2009 in connection to regional winds, multi-year sea ice coverage, ice export, and the thinning of the ice cover.
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Circumpolar thinning of Arctic sea ice following the 2007 record ice extent minimum

TL;DR: Giles et al. as mentioned in this paper used satellite radar altimetry data, covering the Arctic Ocean up to 81.5 degrees North, to show that the average winter sea ice thickness anomaly, after the melt season of 2007, was 0.26 m below the 2002/2003 to 2007/2008 average.
Journal ArticleDOI

Automated Ice-Tethered Profilers for Seawater Observations under Pack Ice in All Seasons

TL;DR: An automated, easily deployed ice-tethered profiler (ITP) instrument system, developed for deployment on perennial sea ice in the polar oceans to measure changes in upper ocean water properties in all seasons, is described in this article.
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