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  • 1
    Publication Date: 2023-01-13
    Keywords: Arctic Ocean; Bottle, Niskin; CANADA-BASIN_001; CANADA-BASIN_002; CANADA-BASIN_003; CANADA-BASIN_004; CANADA-BASIN_005; CANADA-BASIN_006; CANADA-BASIN_007; CANADA-BASIN_008; CANADA-BASIN_009; CANADA-BASIN_010; CANADA-BASIN_011; CANADA-BASIN_012; CANADA-BASIN_013; CANADA-BASIN_014; CANADA-BASIN_015; CANADA-BASIN_017; CANADA-BASIN_018; CANADA-BASIN_019; CANADA-BASIN_020; CANADA-BASIN_021; CANADA-BASIN_022; CANADA-BASIN_023; CANADA-BASIN_024; CANADA-BASIN_025; CANADA-BASIN_026; CANADA-BASIN_027; CANADA-BASIN_028; CANADA-BASIN_029; CANADA-BASIN_030; CANADA-BASIN_031; CANADA-BASIN_032; CANADA-BASIN_033; CANADA-BASIN_034; CANADA-BASIN_035; CANADA-BASIN_036; CANADA-BASIN_037; CANADA-BASIN_038; CANADA-BASIN_039; CANADA-BASIN_040; CANADA-BASIN_041; CANADA-BASIN_042; CANADA-BASIN_043; CANADA-BASIN_044; CANADA-BASIN_045; CANADA-BASIN_046; CANADA-BASIN_047; CANADA-BASIN_048; CANADA-BASIN_049; CANADA-BASIN_050; CANADA-BASIN_051; CANADA-BASIN_052; CANADA-BASIN_053; CANADA-BASIN_054; CANADA-BASIN_055; CANADA-BASIN_056; CANADA-BASIN_057; CANADA-BASIN_058; CANADA-BASIN_059; CANADA-BASIN_060; CANADA-BASIN_061; CANADA-BASIN_062; CANADA-BASIN_063; CANADA-BASIN_064; CANADA-BASIN_065; CANADA-BASIN_066; CANADA-BASIN_067; CANADA-BASIN_068; CANADA-BASIN_069; CANADA-BASIN_070; CANADA-BASIN_071; CANADA-BASIN_072; CANADA-BASIN_073; CANADA-BASIN_074; CANADA-BASIN_075; CANADA-BASIN_076; CANADA-BASIN_077; CANADA-BASIN_078; CANADA-BASIN_079; CANADA-BASIN_080; CANADA-BASIN_081; CANADA-BASIN_082; CANADA-BASIN_083; CANADA-BASIN_084; CANADA-BASIN_085; CANADA-BASIN_086; CANADA-BASIN_087; CANADA-BASIN_088; CANADA-BASIN_089; CANADA-BASIN_090; CANADA-BASIN_091; CANADA-BASIN_092; CANADA-BASIN_093; CANADA-BASIN_094; CANADA-BASIN_095; CANADA-BASIN_096; CANADA-BASIN_097; CANADA-BASIN_098; CANADA-BASIN_099; CANADA-BASIN_100; CANADA-BASIN_101; CANADA-BASIN_102; CANADA-BASIN_103; CANADA-BASIN_104; CANADA-BASIN_105; CANADA-BASIN_106; CANADA-BASIN_107; CANADA-BASIN_108; CANADA-BASIN_109; CANADA-BASIN_110; CANADA-BASIN_111; CANADA-BASIN_112; CANADA-BASIN_113; CANADA-BASIN_114; CANADA-BASIN_115; CANADA-BASIN_116; CANADA-BASIN_117; CANADA-BASIN_118; CANADA-BASIN_119; CANADA-BASIN_120; CANADA-BASIN_121; CANADA-BASIN_122; CANADA-BASIN_123; CANADA-BASIN_124; CANADA-BASIN_125; CANADA-BASIN_126; CANADA-BASIN_127; CANADA-BASIN_128; CANADA-BASIN_129; CANADA-BASIN_130; CANADA-BASIN_131; CANADA-BASIN_132; CANADA-BASIN_133; CANADA-BASIN_134; CANADA-BASIN_135; CANADA-BASIN_136; CANADA-BASIN_137; CANADA-BASIN_138; CANADA-BASIN_139; CANADA-BASIN_140; CANADA-BASIN_141; CANADA-BASIN_142; CANADA-BASIN_143; CANADA-BASIN_144; CANADA-BASIN_145; CANADA-BASIN_146; CANADA-BASIN_147; CANADA-BASIN_148; CANADA-BASIN_149; CANADA-BASIN_150; CANADA-BASIN_151; CANADA-BASIN_152; CANADA-BASIN_153; CANADA-BASIN_154; CANADA-BASIN_155; CANADA-BASIN_156; CANADA-BASIN_157; CANADA-BASIN_158; CANADA-BASIN_159; CANADA-BASIN_16; CANADA-BASIN_160; CANADA-BASIN_161; CANADA-BASIN_162; CANADA-BASIN_163; CANADA-BASIN_164; Date/Time of event; DEPTH, water; Event label; Flow cytometry; Latitude of event; Longitude of event; NIS; Prokaryotes
    Type: Dataset
    Format: text/tab-separated-values, 1467 data points
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  • 2
    ISSN: 1520-6882
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2017-01-26
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 4
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2005. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 32 (2005): L03605, doi:10.1029/2004GL021358.
    Description: We examine the varieties and spatial distributions of Pacific and Eastern Arctic origin halocline waters in the Canada Basin using 2002–2003 hydrographic data. The halocline structure in the Canada Basin is different from the Eastern Arctic halocline because it includes fresher Pacific Winter Waters that form a “cold halostad” which lies above the Eastern Arctic origin lower halocline waters. The structure of the halostad in the Canada Basin, however, is not spatially uniform, and depends on the pathway and history of the source water. Pacific Winter Water entering through the Bering Strait becomes salty due to sea ice formation and this, in turn, is dependent on the occurrence and distribution of polynyas. In particular, saline water from the eastern Chukchi Sea forms thick halostad and causes depression of the isohalines in the southern Canada Basin. This depression influences thermohaline structure of the oceanic Beaufort Gyre.
    Description: This work was funded in part by the Japan Agency for Marine-Earth Science and Technology, the Fisheries and Oceans Canada, and the U.S. National Science Foundation.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 5
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2006. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 33 (2006): L08605, doi:10.1029/2005GL025624.
    Description: The spatial pattern of recent ice reduction in the Arctic Ocean is similar to the distribution of warm Pacific Summer Water (PSW) that interflows the upper portion of halocline in the southern Canada Basin. Increases in PSW temperature in the basin are also well-correlated with the onset of sea-ice reduction that began in the late 1990s. However, increases in PSW temperature in the basin do not correlate with the temperature of upstream source water in the northeastern Bering Sea, suggesting that there is another mechanism which controls these concurrent changes in ice cover and upper ocean temperature. We propose a feedback mechanism whereby the delayed sea-ice formation in early winter, which began in 1997/1998, reduced internal ice stresses and thus allowed a more efficient coupling of anticyclonic wind forcing to the upper ocean. This, in turn, increased the flux of warm PSW into the basin and caused the catastrophic changes.
    Description: This work was funded in part by Japan Agency for Marine-Earth Science and Technology, Fisheries and Oceans Canada, and the U.S. National Science Foundation.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 6
    Publication Date: 2022-05-25
    Description: © The Author(s), 2012. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Biogeosciences 9 (2012): 1217-1224, doi:10.5194/bg-9-1217-2012.
    Description: Arctic warming is projected to continue throughout the coming century. Yet, our currently limited understanding of the Arctic Ocean carbon cycle hinders our ability to predict how changing conditions will affect local Arctic ecosystems, regional carbon budgets, and global climate. We present here the first set of concurrent, full-depth, dual-isotope profiles for dissolved inorganic carbon (DIC), dissolved organic carbon (DOC), and suspended particulate organic carbon (POCsusp) at two sites in the Canada Basin of the Arctic Ocean. The carbon isotope composition of sinking and suspended POC in the Arctic contrasts strongly with open ocean Atlantic and Pacific sites, pointing to a combination of inputs to Arctic POCsusp at depth, including surface-derived organic carbon (OC), sorbed/advected OC, and OC derived from in situ DIC fixation. The latter process appears to be particularly important at intermediate depths, where mass balance calculations suggest that OC derived from in situ DIC fixation contributes up to 22% of POCsusp. As in other oceans, surface-derived OC is still a dominant source to Arctic POCsusp. Yet, we suggest that significantly smaller vertical POC fluxes in the Canada Basin make it possible to see evidence of DIC fixation in the POCsusp pool even at the bulk isotope level.
    Description: The 2008 JOIS hydrographic program was supported by Fisheries and Oceans Canada, the Canadian International Polar Year Office, and the US National Science Foundation (OPP-0424864; lead-PI Andrey Proshutinsky).
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 7
    Publication Date: 2022-05-25
    Description: Author Posting. © Oceanography Society, 2011. This article is posted here by permission of Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 24 no. 3 (2011): 146–159, doi:10.5670/oceanog.2011.66.
    Description: Sea ice extent in the Arctic Ocean diminished significantly during the first decade of the 2000s, most particularly in the Canada Basin where the loss of both multiyear and first-year ice was greater than in the other three subbasins. Using data collected during basin-wide surveys conducted from 2003–2010 together with data collected during the 1990s and 2000s at one station in the southern Canada Basin, we investigate the response of the Canada Basin water column to this significant decrease in ice cover. Changes were evident from the surface down to the Atlantic layer: some changes were the result of Beaufort Gyre forcing on regional processes, others were the result of Arctic Ocean atmospheric forcing on a hemispheric scale and large-scale advection. These changes have troubling consequences for the ecosystem.
    Description: We acknowledge support from Fisheries and Oceans Canada, the US National Science Foundation Office of Polar Programs (grant OPP-0424864), and the Canadian International Polar Year office.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 8
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 31 (2004): L20301, doi:10.1029/2004GL020860.
    Description: Penetration of the 1990s warm temperature anomaly (WTA) of the Fram Strait branch of Atlantic Water (FSBW) in the Canada Basin is described using available temperature, salinity, and velocity data. The core temperatures of FSBW show distinct pathways. Over the Chukchi Borderland advective velocities of the FSBW are well-correlated with bottom topography. The resulting multifarious pathways over the Chukchi Borderland act to modulate and substantially increase the time scale of WTA spreading and advancement. Further downstream two WTA tongues are observed. One tongue followed the Beaufort Slope and, along this pathway, the core temperatures of FSBW decreased rapidly. The depth integrated value of heat content remained near constant however, suggesting enhanced vertical mixing. The second tongue debouched from the northern tip of the Northwind Ridge and spread eastward into the deep Canada Basin, suggesting a complex recirculation structure within the Beaufort Gyre.
    Description: This work was funded in part by the Fisheries and Oceans Canada, the Japan Marine Science and Technology Center and the U.S. National Science Foundation.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 9
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2009. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 114 (2009): C00A10, doi:10.1029/2008JC005104.
    Description: We investigate 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. Specifically, the mean annual cycle and interannual and decadal FWC variability are explored. The major cause of the large FWC in the BG is the process of Ekman pumping (EP) due to the Arctic High anticyclonic circulation centered in the BG. The mean seasonal cycle of liquid FWC is a result of interplay between the mechanical (EP) and thermal (ice transformations) factors and has two peaks. One peak occurs around June–July when the sea ice thickness reaches its minimum (maximum ice melt). The second maximum is observed in November–January when wind curl is strongest (maximum EP) and the salt input from the growing ice has not yet reached its maximum. Interannual changes in FWC during 2003–2007 are characterized by a strong positive trend in the region varying by location with a maximum of approximately 170 cm a−1 in the center of EP influenced region. Decadal FWC variability in the period 1950–2000 is dominated by a significant change in the 1990s forced by an atmospheric circulation regime change. The center of maximum FWC shifted to the southeast and appeared to contract in area relative to the pre-1990s climatology. In spite of the areal reduction, the spatially integrated FWC increased by over 1000 km3 relative to climatology.
    Description: The funding for Andrey Proshutinsky, Richard Krishfield, John Toole, and Mary-Louise Timmermans (partial financial support of logistics, hydrographic observations on the board of Canadian icebreaker, and full financial coverage of all mooring instrumentation) was provided by the National Science Foundation (under grants ARC- 0806115, ARC-0631951, and ARC-0806306) and Woods Hole Oceanographic Institution internal funding.
    Keywords: Beaufort Gyre oceanography ; Freshwater balance ; Circulation and water masses
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 10
    Publication Date: 2022-05-25
    Description: © The Author(s), 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Journal of Geophysical Research: Oceans 120 (2015): 2784–2799, doi:10.1002/2014JC010643.
    Description: To better understand the current carbon cycle and potentially detect its change in the rapidly changing Arctic Ocean, we examined sinking particles collected quasi-continuously over a period of 7 years (2004–2011) by bottom-tethered sediment trap moorings in the central Canada Basin. Total mass flux was very low (〈100 mg m−2 d−1) at all sites and was temporally decoupled from the cycle of primary production in surface waters. Extremely low radiocarbon contents of particulate organic carbon and high aluminum contents in sinking particles reveal high contributions of resuspended sediment to total sinking particle flux in the deep Canada Basin. Station A (75°N, 150°W) in the southwest quadrant of the Canada Basin is most strongly influenced while Station C (77°N, 140°W) in the northeast quadrant is least influenced by lateral particle supply based on radiocarbon content and Al concentration. The results at Station A, where three sediment traps were deployed at different depths, imply that the most likely mode of lateral particle transport was as thick clouds of enhanced particle concentration extending well above the seafloor. At present, only 1%–2% of the low levels of new production in Canada Basin surface waters reaches the interior basin. Lateral POC supply therefore appears to be the major source of organic matter to the interior basin. However, ongoing changes to surface ocean boundary conditions may influence both lateral and vertical supply of particulate material to the deep Canada Basin.
    Description: This research was funded by the NSF Division of Polar Programs (ARC-0909377), the Ocean and Climate Change Institute of Woods Hole Oceanographic Institution, and ETH Zürich. J.H. and M.K. were partly supported by the National Research Foundation of Korea grant funded by the Korean Government (2011–0013629).
    Keywords: Canada Basin ; Particulate organic carbon ; Lateral supply ; Radiocarbon ; Carbon cycle
    Repository Name: Woods Hole Open Access Server
    Type: Article
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    Format: application/vnd.ms-excel
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