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  • 06MT59_2; 06MT59_2/450; 06MT59_2/451; 06MT59_2/452; 06MT59_2/453; 06MT59_2/455; 06MT59_2/456; 06MT59_2/457; 06MT59_2/458; 06MT59_2/459; 06MT59_2/460; 06MT59_2/461; 06MT59_2/462; 06MT59_2/463; 06MT59_2/464; 06MT59_2/465; 06MT59_2/466; 06MT59_2/467; 06MT59_2/468; 06MT59_2/469; 06MT59_2/470; 06MT59_2/471; 06MT59_2/472; 06MT59_2/473; 06MT59_2/474; 06MT59_2/475; 06MT59_2/476; 06MT59_2/477; 06MT59_2/478; 06MT59_2/479; 06MT59_2/480; 06MT59_2/481; 06MT59_2/482; 06MT59_2/483; 06MT59_2/484; 06MT59_2/485; 06MT59_2/486; 06MT59_2/487; 06MT59_2/488; 06MT59_2/489; 06MT59_2/490; 06MT59_2/491; 06MT59_2/492; 06MT59_2/493; 06MT59_2/494; 06MT59_2/495; 06MT59_2/496; 06MT59_2/497; 06MT59_2/498; 06MT59_2/499; 06MT59_2/500; 06MT59_2/501; 06MT59_2/502; 06MT59_2/503; 06MT59_2/504; 06MT59_2/505; 06MT59_2/506; 06MT59_2/507-1; 06MT59_2/509; 06MT59_2/510; 06MT59_2/511; 06MT59_2/512; 06MT59_2/513; 06MT59_2/514; 06MT59_2/515; 06MT59_2/517; 06MT59_2/518; 06MT59_2/519; 06MT59_2/520; 06MT59_2/521; 06MT59_2/522; 06MT59_2/523; 06MT59_2/524; 06MT59_2/525; 06MT59_2/526; 06MT59_2/527; 06MT59_2/529; 06MT59_2/530; 06MT59_2/531; 06MT59_2/532; 06MT59_2/533; 06MT59_2/534; 06MT59_2/535; 06MT59_2/536; 06MT59_2/537; 06MT59_2/538; 06MT59_2/539; 06MT59_2/540; 06MT59_2/541; 06MT59_2/542; 06MT59_2/543; 06MT59_2/544; 06MT59_2/545; 06MT59_2/546; 06MT59_2/547; 06MT59_2/548; 06MT59_2/549; 06MT59_2/550; 06MT59_2/551; 06MT59_2/552; 06MT59_2/553; 06MT59_2/554; 06MT59_2/555; 06MT59_2/556; 06MT59_2/557; 06MT59_2/558; 06MT59_2/559; 06MT59_2/560; 06MT59_2/561; 06MT59_2/562; 06MT59_2/563; 06MT59_2/564; 06MT59_2/565; 06MT59_2/566; 06MT59_2/567; 06MT59_2/568; 06MT59_2/569; 06MT59_2/570; 06MT59_2/571; 06MT59_2/572; 06MT59_2/573; 06MT59_2/574; 06MT59_2/576; 06MT59_2/578; 06MT59_2/580; 06MT59_2/582; 06MT59_2/583; 06MT59_2/585; 06MT59_2/586; 06MT59_2/587; 06MT59_2/588; 06MT59_2/589; CTD/Rosette; CTD-RO; M59/2; M59/2_450; M59/2_451; M59/2_452; M59/2_453; M59/2_455; M59/2_456; M59/2_457; M59/2_458; M59/2_459; M59/2_460; M59/2_461; M59/2_462; M59/2_463; M59/2_464; M59/2_465; M59/2_466; M59/2_467; M59/2_468; M59/2_469; M59/2_470; M59/2_471; M59/2_472; M59/2_473; M59/2_474; M59/2_475; M59/2_476; M59/2_477; M59/2_478; M59/2_479; M59/2_480; M59/2_481; M59/2_482; M59/2_483; M59/2_484; M59/2_485; M59/2_486; M59/2_487; M59/2_488; M59/2_489; M59/2_490; M59/2_491; M59/2_492; M59/2_493; M59/2_494; M59/2_495; M59/2_496; M59/2_497; M59/2_498; M59/2_499; M59/2_500; M59/2_501; M59/2_502; M59/2_503; M59/2_504; M59/2_505; M59/2_506; M59/2_507-1; M59/2_509; M59/2_510; M59/2_511; M59/2_512; M59/2_513; M59/2_514; M59/2_515; M59/2_517; M59/2_518; M59/2_519; M59/2_520; M59/2_521; M59/2_522; M59/2_523; M59/2_524; M59/2_525; M59/2_526; M59/2_527; M59/2_529; M59/2_530; M59/2_531; M59/2_532; M59/2_533; M59/2_534; M59/2_535; M59/2_536; M59/2_537; M59/2_538; M59/2_539; M59/2_540; M59/2_541; M59/2_542; M59/2_543; M59/2_544; M59/2_545; M59/2_546; M59/2_547; M59/2_548; M59/2_549; M59/2_550; M59/2_551; M59/2_552; M59/2_553; M59/2_554; M59/2_555; M59/2_556; M59/2_557; M59/2_558; M59/2_559; M59/2_560; M59/2_561; M59/2_562; M59/2_563; M59/2_564; M59/2_565; M59/2_566; M59/2_567; M59/2_568; M59/2_569; M59/2_570; M59/2_571; M59/2_572; M59/2_573; M59/2_574; M59/2_576; M59/2_578; M59/2_580; M59/2_582; M59/2_583; M59/2_585; M59/2_586; M59/2_587; M59/2_588; M59/2_589; Meteor (1986); Northeast Atlantic  (1)
  • Ocean oxygen and nutrients
  • Deep-water
Collection
Keywords
Publisher
Years
  • 1
    Publication Date: 2022-05-25
    Description: This paper is not subject to U.S. copyright. The definitive version was published in Deep Sea Research Part I: Oceanographic Research Papers 74 (2013): 48-63, doi:10.1016/j.dsr.2012.12.005.
    Description: Detection and attribution of hydrographic and biogeochemical changes in the deep ocean are challenging due to the small magnitude of their signals and to limitations in the accuracy of available data. However, there are indications that anthropogenic and climate change signals are starting to manifest at depth. The deep ocean below 2000 m comprises about 50% of the total ocean volume, and changes in the deep ocean should be followed over time to accurately assess the partitioning of anthropogenic carbon dioxide (CO2) between the ocean, terrestrial biosphere, and atmosphere. Here we determine the changes in the interior deep-water inorganic carbon content by a novel means that uses the partial pressure of CO2 measured at 20 °C, pCO2(20), along three meridional transects in the Atlantic and Pacific oceans. These changes are measured on decadal time scales using observations from the World Ocean Circulation Experiment (WOCE)/World Hydrographic Program (WHP) of the 1980s and 1990s and the CLIVAR/CO2 Repeat Hydrography Program of the past decade. The pCO2(20) values show a consistent increase in deep water over the time period. Changes in total dissolved inorganic carbon (DIC) content in the deep interior are not significant or consistent, as most of the signal is below the level of analytical uncertainty. Using an approximate relationship between pCO2(20) and DIC change, we infer DIC changes that are at the margin of detectability. However, when integrated on the basin scale, the increases range from 8–40% of the total specific water column changes over the past several decades. Patterns in chlorofluorocarbons (CFCs), along with output from an ocean model, suggest that the changes in pCO2(20) and DIC are of anthropogenic origin.
    Description: Rik Wanninkhof, Geun-Ha Park, John L. Bullister, and Richard A. Feely appreciate the support from the NOAA Office of Atmospheric and Oceanic Research and the Climate Observation Division. S.C.D. acknowledges support from NOAA Grant NA07OAR4310098. T.T. has been supported by grants from NSF and NOAA.
    Keywords: Ocean ; Carbon dioxide ; CO2 sink ; Anthropogenic carbon ; Deep-water
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © The Author(s), 2015. This is the author's version of the work. It is posted here for personal use, not for redistribution. The definitive version was published in Annual Review of Marine Science 8 (2016): 185-215, doi:10.1146/annurev-marine-052915-100829.
    Description: The ocean, a central component of Earth’s climate system, is changing. Given the global scope of these changes, highly accurate measurements of physical and biogeochemical properties need to be conducted over the full water column, spanning the ocean basins from coast to coast, and repeated every decade at a minimum, with a ship-based observing system. Since the late 1970s, when the Geochemical Ocean Sections Study (GEOSECS) conducted the first global survey of this kind, the World Ocean Circulation Experiment (WOCE) and Joint Global Ocean Flux Study (JGOFS), and now the Global Ocean Ship-based Hydrographic Investigations Program (GO-SHIP) have collected these “reference standard” data that allow quantification of ocean heat and carbon uptake, and variations in salinity, oxygen, nutrients, and acidity on basin scales. The evolving GO-SHIP measurement suite also provides new global information about dissolved organic carbon, a large bioactive reservoir of carbon.
    Description: Climate Observations Division of the U.S. NOAA Climate Program Office and NOAA Research; Joint Institute for the Study of the Atmosphere and Ocean (JISAO) under NOAA Cooperative Agreement NA10OAR4320148; U.S. National Science Foundation [OCE- 0223869; OCE-0752970; OCE-0825163; OCE-1434000; OCE 0752972; OCE-0752980; OCE-1232962; OCE-1155983; OCE-1436748]; U.S. CLIVAR Project Office; Global Environment and Marine Department, Japan Meteorological Agency; Australian Climate Change Science Program (Australian Department of Environment and CSIRO); U.K. Natural Environment Research Council; European Union’s FP7 grant agreement 264879 (CarboChange); Horizon 2020 grant agreement No 633211; ETH Zurich Switzerland.
    Keywords: Anthropogenic climate change ; Ocean temperature change ; Salinity change ; Ocean carbon cycle ; Ocean oxygen and nutrients ; Ocean chlorofluorocarbons ; Ocean circulation change ; Ocean mixing
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Steinfeldt, Reiner; Rhein, Monika; Bullister, John L; Tanhua, Toste (2009): Inventory changes in anthropogenic carbon from 1997–2003 in the Atlantic Ocean between 20°S and 65°N. Global Biogeochemical Cycles, 23, GB3010, https://doi.org/10.1029/2008GB003311
    Publication Date: 2024-02-02
    Description: The oceans absorb and store a significant portion of anthropogenic CO2 emissions, but large uncertainties remain in the quantification of this sink. An improved assessment of the present and future oceanic carbon sink is therefore necessary to provide recommendations for long-term global carbon cycle and climate policies. The formation of North Atlantic Deep Water (NADW) is a unique fast track for transporting anthropogenic CO2 into the ocean's interior, making the deep waters rich in anthropogenic carbon. Thus the Atlantic is presently estimated to hold 38% of the oceanic anthropogenic CO2 inventory, although its volume makes up only 25% of the world ocean. Here we analyze the inventory change of anthropogenic CO2 in the Atlantic between 1997 and 2003 and its relationship to NADW formation. For the whole region between 20°S and 65°N the inventory amounts to 32.5 ± 9.5 Petagram carbon (Pg C) in 1997 and increases up to 36.0 ± 10.5 Pg C in 2003. This result is quite similar to earlier studies. Moreover, the overall increase of anthropogenic carbon is in close agreement with the expected change due to rising atmospheric CO2 levels of 1.69% a?1. On the other hand, when considering the subpolar region only, the results demonstrate that the recent weakening in the formation of Labrador Sea Water, a component of NADW, has already led to a decrease of the anthropogenic carbon inventory in this water mass. As a consequence, the overall inventory for the total water column in the western subpolar North Atlantic increased only by 2% between 1997 and 2003, much less than the 11% that would be expected from the increase in atmospheric CO2 levels.
    Keywords: 06MT59_2; 06MT59_2/450; 06MT59_2/451; 06MT59_2/452; 06MT59_2/453; 06MT59_2/455; 06MT59_2/456; 06MT59_2/457; 06MT59_2/458; 06MT59_2/459; 06MT59_2/460; 06MT59_2/461; 06MT59_2/462; 06MT59_2/463; 06MT59_2/464; 06MT59_2/465; 06MT59_2/466; 06MT59_2/467; 06MT59_2/468; 06MT59_2/469; 06MT59_2/470; 06MT59_2/471; 06MT59_2/472; 06MT59_2/473; 06MT59_2/474; 06MT59_2/475; 06MT59_2/476; 06MT59_2/477; 06MT59_2/478; 06MT59_2/479; 06MT59_2/480; 06MT59_2/481; 06MT59_2/482; 06MT59_2/483; 06MT59_2/484; 06MT59_2/485; 06MT59_2/486; 06MT59_2/487; 06MT59_2/488; 06MT59_2/489; 06MT59_2/490; 06MT59_2/491; 06MT59_2/492; 06MT59_2/493; 06MT59_2/494; 06MT59_2/495; 06MT59_2/496; 06MT59_2/497; 06MT59_2/498; 06MT59_2/499; 06MT59_2/500; 06MT59_2/501; 06MT59_2/502; 06MT59_2/503; 06MT59_2/504; 06MT59_2/505; 06MT59_2/506; 06MT59_2/507-1; 06MT59_2/509; 06MT59_2/510; 06MT59_2/511; 06MT59_2/512; 06MT59_2/513; 06MT59_2/514; 06MT59_2/515; 06MT59_2/517; 06MT59_2/518; 06MT59_2/519; 06MT59_2/520; 06MT59_2/521; 06MT59_2/522; 06MT59_2/523; 06MT59_2/524; 06MT59_2/525; 06MT59_2/526; 06MT59_2/527; 06MT59_2/529; 06MT59_2/530; 06MT59_2/531; 06MT59_2/532; 06MT59_2/533; 06MT59_2/534; 06MT59_2/535; 06MT59_2/536; 06MT59_2/537; 06MT59_2/538; 06MT59_2/539; 06MT59_2/540; 06MT59_2/541; 06MT59_2/542; 06MT59_2/543; 06MT59_2/544; 06MT59_2/545; 06MT59_2/546; 06MT59_2/547; 06MT59_2/548; 06MT59_2/549; 06MT59_2/550; 06MT59_2/551; 06MT59_2/552; 06MT59_2/553; 06MT59_2/554; 06MT59_2/555; 06MT59_2/556; 06MT59_2/557; 06MT59_2/558; 06MT59_2/559; 06MT59_2/560; 06MT59_2/561; 06MT59_2/562; 06MT59_2/563; 06MT59_2/564; 06MT59_2/565; 06MT59_2/566; 06MT59_2/567; 06MT59_2/568; 06MT59_2/569; 06MT59_2/570; 06MT59_2/571; 06MT59_2/572; 06MT59_2/573; 06MT59_2/574; 06MT59_2/576; 06MT59_2/578; 06MT59_2/580; 06MT59_2/582; 06MT59_2/583; 06MT59_2/585; 06MT59_2/586; 06MT59_2/587; 06MT59_2/588; 06MT59_2/589; CTD/Rosette; CTD-RO; M59/2; M59/2_450; M59/2_451; M59/2_452; M59/2_453; M59/2_455; M59/2_456; M59/2_457; M59/2_458; M59/2_459; M59/2_460; M59/2_461; M59/2_462; M59/2_463; M59/2_464; M59/2_465; M59/2_466; M59/2_467; M59/2_468; M59/2_469; M59/2_470; M59/2_471; M59/2_472; M59/2_473; M59/2_474; M59/2_475; M59/2_476; M59/2_477; M59/2_478; M59/2_479; M59/2_480; M59/2_481; M59/2_482; M59/2_483; M59/2_484; M59/2_485; M59/2_486; M59/2_487; M59/2_488; M59/2_489; M59/2_490; M59/2_491; M59/2_492; M59/2_493; M59/2_494; M59/2_495; M59/2_496; M59/2_497; M59/2_498; M59/2_499; M59/2_500; M59/2_501; M59/2_502; M59/2_503; M59/2_504; M59/2_505; M59/2_506; M59/2_507-1; M59/2_509; M59/2_510; M59/2_511; M59/2_512; M59/2_513; M59/2_514; M59/2_515; M59/2_517; M59/2_518; M59/2_519; M59/2_520; M59/2_521; M59/2_522; M59/2_523; M59/2_524; M59/2_525; M59/2_526; M59/2_527; M59/2_529; M59/2_530; M59/2_531; M59/2_532; M59/2_533; M59/2_534; M59/2_535; M59/2_536; M59/2_537; M59/2_538; M59/2_539; M59/2_540; M59/2_541; M59/2_542; M59/2_543; M59/2_544; M59/2_545; M59/2_546; M59/2_547; M59/2_548; M59/2_549; M59/2_550; M59/2_551; M59/2_552; M59/2_553; M59/2_554; M59/2_555; M59/2_556; M59/2_557; M59/2_558; M59/2_559; M59/2_560; M59/2_561; M59/2_562; M59/2_563; M59/2_564; M59/2_565; M59/2_566; M59/2_567; M59/2_568; M59/2_569; M59/2_570; M59/2_571; M59/2_572; M59/2_573; M59/2_574; M59/2_576; M59/2_578; M59/2_580; M59/2_582; M59/2_583; M59/2_585; M59/2_586; M59/2_587; M59/2_588; M59/2_589; Meteor (1986); Northeast Atlantic
    Type: Dataset
    Format: application/zip, 131 datasets
    Location Call Number Expected Availability
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