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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)
  • Oceanography; Meteorology and Climatology
Collection
Keywords
Publisher
Years
  • 1
    Publication Date: 2019-07-13
    Description: The Ocean Model Intercomparison Project (OMIP) focuses on the physics and biogeochemistry of the ocean component of Earth system models participating in the sixth phase of the Coupled Model Intercomparison Project (CMIP6). OMIP aims to provide standard protocols and diagnostics for ocean models, while offering a forum to promote their common assessment and improvement. It also offers to compare solutions of the same ocean models when forced with reanalysis data (OMIP simulations) vs. when integrated within fully coupled Earth system models (CMIP6). Here we detail simulation protocols and diagnostics for OMIP's biogeochemical and inert chemical tracers. These passive-tracer simulations will be coupled to ocean circulation models, initialized with observational data or output from a model spin-up, and forced by repeating the 1948-2009 surface fluxes of heat, fresh water, and momentum. These so-called OMIP-BGC simulations include three inert chemical tracers (CFC-11, CFC-12, SF [subscript] 6) and biogeochemical tracers (e.g., dissolved inorganic carbon, carbon isotopes, alkalinity, nutrients, and oxygen). Modelers will use their preferred prognostic BGC model but should follow common guidelines for gas exchange and carbonate chemistry. Simulations include both natural and total carbon tracers. The required forced simulation (omip1) will be initialized with gridded observational climatologies. An optional forced simulation (omip1-spunup) will be initialized instead with BGC fields from a long model spin-up, preferably for 2000 years or more, and forced by repeating the same 62-year meteorological forcing. That optional run will also include abiotic tracers of total dissolved inorganic carbon and radiocarbon, CTabio and 14CTabio, to assess deep-ocean ventilation and distinguish the role of physics vs. biology. These simulations will be forced by observed atmospheric histories of the three inert gases and CO2 as well as carbon isotope ratios of CO2. OMIP-BGC simulation protocols are founded on those from previous phases of the Ocean Carbon-Cycle Model Intercomparison Project. They have been merged and updated to reflect improvements concerning gas exchange, carbonate chemistry, and new data for initial conditions and atmospheric gas histories. Code is provided to facilitate their implementation.
    Keywords: Oceanography; Meteorology and Climatology
    Type: GSFC-E-DAA-TN43737 , Geoscientific Model Development (e-ISSN 1991-9603); 10; 6; 2169–2199
    Format: text
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  • 2
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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
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