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  • 1
    Keywords: Meridional overturning circulation. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (401 pages)
    Edition: 1st ed.
    ISBN: 9781118671887
    Series Statement: Geophysical Monograph Series ; v.173
    Language: English
    Note: Intro -- Title Page -- Contents -- Preface -- Section 1. Introduction -- Introduction: The Ocean's Meridional Overturning Circulation -- Discovery and Quantification of the Atlantic Meridional Overturning Circulation: The Importance of 25°N -- Section 2. Theory and Perspectives -- A Simple Theory of the Pycnocline and Overturning Revisited -- Buoyancy-Driven Flow and Nature of Vertical Mixing in a Zonally Averaged Model -- The Past and Future Ocean Circulation From a Contemporary Perspective -- Section 3. Current State and Trend -- Present-Day Manifestation of the Nordic Seas Overflows -- Circulation and Deep Water Export of the Subpolar North Atlantic During the 1990's -- Strength and Variability of the Deep Limb of the North Atlantic Meridional Overturning Circulation From Chlorofluorocarbon Inventories -- Section 4. Decadal to Centennial Variability -- Decadal to Centennial Variability of the Atlantic From Observations and Models -- Decadal to Multidecadal Variability of the Atlantic MOC: Mechanisms and Predictability -- Section 5. Past States and Millennial Variability -- Is the Frequency of Abrupt Climate Change Modulated by the Orbital Insolation? -- 14C Reservoir Ages Show Deglacial Changes in Ocean Currents and Carbon Cycle -- Phasing of Millennial Climate Events and Northeast Atlantic Deep-Water Temperature Change Since 50 ka BP -- Mechanisms for an ~7-kyr Climate and Sea-Level Oscillation During Marine Isotope Stage 3 -- North Atlantic Intermediate Depth Variability During the Younger Dryas: Evidence From Benthic Foraminiferal Mg/Ca and the GFDL R30 Coupled Climate Model -- Section 6. Impact on Climate, Ecosystems, and Biogeochemical Cycles -- Musings About the Connection Between Thermohaline Circulation and Climate. , Millennial-Scale Interhemispheric Asymmetry of Low-Latitude Precipitation: Speleothem Evidence and Possible High-Latitude Forcing -- Adjustment of the Global Climate to an Abrupt Slowdown of the Atlantic Meridional Overturning Circulation -- Impact of the Ocean's Overturning Circulation on Atmospheric CO2 -- Antarctic Stratification, Atmospheric Water Vapor, and Heinrich Events: A Hypothesis for Late Pleistocene Deglaciations -- Section 7. Future Projections -- Response of the Meridional Overturning Circulation During Differing Pathways Toward Greenhouse Gas Stabilization -- Projected Strengthening of the Southern Ocean Winds: Some Implications for the Deep Ocean Circulation -- Effect of the Greenland Ice-Sheet Melting on the Response and Stability of the AMOC in the Next Centuries.
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  • 2
    In: Earth & planetary science letters, Amsterdam [u.a.] : Elsevier, 1966, 259(2007), 3/4, Seite 432-441, 0012-821X
    In: volume:259
    In: year:2007
    In: number:3/4
    In: pages:432-441
    Type of Medium: Article
    Pages: Graph. Darst.
    ISSN: 0012-821X
    Language: English
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  • 3
    Keywords: Meridional overturning circulation ; Aufsatzsammlung ; Meridionalzirkulation
    Type of Medium: Book
    Pages: VII, 392 S. , Ill., graph. Darst., Kt.
    ISBN: 9780875904382
    Series Statement: Geophysical monograph 173
    DDC: 551.46/2
    RVK:
    Language: English
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  • 4
    Publication Date: 2024-02-28
    Description: In the southern Indian Ocean, the position of the subtropical front – the boundary between colder, fresher waters to the south and warmer, saltier waters to the north – has a strong influence on the upper ocean hydrodynamics and biogeochemistry. Here we analyse a sedimentary record from the Agulhas Plateau, located close to the modern position of the subtropical front and use alkenones and coccolith assemblages to reconstruct oceanographic conditions over the past 300,000 years. We identify a strong glacial-interglacial variability in sea surface temperature and productivity associated with subtropical front migration over the Agulhas Plateau, as well as shorter-term high frequency variability aligned with variations in high latitude insolation. Alkenone and coccolith abundances, in combination with diatom and organic carbon records indicate high glacial export productivity. We conclude that the biological pump was more efficient and strengthened during glacial periods, which could partly account for the reported reduction in atmospheric carbon dioxide concentrations.
    Description: Migration of the Subtropical Front during glacial and interglacial periods resulted in variability in the strength of the biological pump in the Southern Ocean sector of the Indian Ocean, according to sedimentary records from the Agulhas Plateau.
    Description: https://doi.pangaea.de/10.1594/PANGAEA.912467
    Keywords: ddc:551.46 ; palaeoceanography ; southern Indian Ocean ; Agulhas Plateau ; upper ocean hydrodynamics ; biogeochemistry
    Language: English
    Type: doc-type:article
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  • 5
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    PANGAEA
    In:  Supplement to: Franzese, Allison M; Hemming, Sidney R; Goldstein, Steven L (2009): Use of strontium isotopes in detrital sediments to constrain the glacial position of the Agulhas Retroflection. Paleoceanography, 24(2), PA2217, https://doi.org/10.1029/2008PA001706
    Publication Date: 2023-05-12
    Description: The Agulhas Leakage represents a significant portion of the warm, surface return flow of the global overturning circulation and thus may be an important feedback in the ocean climate system. Models indicate that reduced leakage could be caused by a stronger Agulhas Current and/or a more upstream (eastward) Agulhas Retroflection, while a weaker Agulhas Current would result in a more westward retroflection and increased leakage. However, data for the Last Glacial Maximum support both a weaker Agulhas Current and less leakage, implying a possible displacement of the retroflection. We present new 87Sr/86Sr results for modern sediments within this region, confirming that the modern pathway of the Agulhas Current, Retroflection, and Leakage can be traced by terrigenous sediment provenance using Sr isotopes. New 87Sr/86Sr data from sediments deposited during the Last Glacial Maximum suggest that the glacial Agulhas Current and Retroflection followed nearly their modern trajectory. The provenance data appear to rule out both a stronger Agulhas Current and a more upstream Agulhas Retroflection. We conclude that the reduced glacial leakage was caused by the weakened Agulhas Current, with no significant change in the retroflection position. This is inconsistent with the model predictions and thus emphasizes the need for further work in this region.
    Type: Dataset
    Format: application/zip, 27 datasets
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  • 6
    Publication Date: 2023-05-12
    Keywords: AGE; Age, comment; ALIENOR; Calculated; Calypso Square Core System; CASQS; DEPTH, sediment/rock; Marion Dufresne (1995); MD04-2829CQ; MD141; Northeast Atlantic; Sedimentation rate
    Type: Dataset
    Format: text/tab-separated-values, 33 data points
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  • 7
    Publication Date: 2023-05-12
    Keywords: Age, dated; Age, dated standard deviation; Age, Uranium-Thorium; Corrected; Depth, bathymetric; DEPTH, sediment/rock; Gregg_Seamount; Identification; Laboratory code/label; Location; North Atlantic; Thorium-230; Thorium-230, standard deviation; Thorium-230/Uranium-238 activity ratio; Thorium-230/Uranium-238 activity ratio, standard deviation; Thorium-232; Thorium-232, standard deviation; Uranium-238; Uranium-238, standard deviation; δ234 Uranium; δ234 Uranium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 200 data points
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  • 8
    Publication Date: 2023-05-12
    Keywords: AGE; Age, standard deviation; Depth, bathymetric; DEPTH, sediment/rock; Gregg_Seamount; Identification; Laboratory code/label; Location; Neodymium-143/Neodymium-144 ratio; Neodymium-143/Neodymium-144 ratio, error; North Atlantic; ε-Neodymium; ε-Neodymium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 108 data points
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  • 9
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    PANGAEA
    In:  Supplement to: van de Flierdt, Tina; Robinson, Laura F; Adkins, Jess F; Hemming, Sidney R; Goldstein, Steven L (2006): Temporal stability of the neodymium isotope signature of the Holocene to glacial North Atlantic. Paleoceanography, 21, PA4102, https://doi.org/10.1029/2006PA001294
    Publication Date: 2023-05-12
    Description: The neodymium isotopic composition of marine precipitates is increasingly recognized as a powerful tool for identifying changes in ocean circulation and mixing on million year to millennial timescales. Unlike nutrient proxies such as d13C or Cd/Ca, Nd isotopes are not thought to be altered in any significant way by biological processes, and thus they can serve as a quasi-conservative water mass tracer. However, the application of Nd isotopes in understanding the role of thermohaline circulation in rapid climate change is currently hindered by the lack of direct constraints on the signature of the North Atlantic end-member through time. Here we present the first results of Nd isotopes measured in U-Th-dated deep-sea corals from the New England seamounts in the northwest Atlantic Ocean. Our data are consistent with the conclusion that the Nd isotopic composition of North Atlantic deep and intermediate water has remained nearly constant through the last glacial cycle. The results address long-standing concerns that there may have been significant changes in the Nd isotopic composition of the North Atlantic end-member during this interval and substantiate the applicability of this novel tracer on millennial timescales for paleoceanography research.
    Keywords: Gregg_Seamount; North Atlantic
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 10
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    PANGAEA
    In:  Supplement to: Marchitto, Thomas M; Lynch-Stieglitz, Jean; Hemming, Sidney R (2005): Deep Pacific CaCO3 compensation and glacial-interglacial atmospheric CO2. Earth and Planetary Science Letters, 231(3-4), 317-336, https://doi.org/10.1016/j.epsl.2004.12.024
    Publication Date: 2023-06-27
    Description: Benthic foraminiferal delta13C suggests that there was a net shift of isotopically light metabolic CO2 from the upper ocean into the deep ocean during the last glacial period. According to the 'CaCO3 compensation' hypothesis, this should have caused a transient drop in deep ocean CO3[2-] that was eventually reversed by seafloor dissolution of CaCO3. The resulting increase in whole-ocean pH may have had a significant impact on atmospheric CO2, compounding any decrease that was due to the initial vertical CO2 shift. The opposite hypothetically occurred during deglaciation, when CO2 was returned to the upper ocean (and atmosphere) and deep ocean CO3[2-] temporarily increased, followed by excess burial of CaCO3 and a drop in whole-ocean pH. The deep sea record of CaCO3 preservation appears to reflect these processes, with the largest excursion during deglaciation (as expected), but various factors make quantification of deep sea paleo-CO3[2-] difficult. Here we reconstruct deep equatorial Pacific CO3[2-] over the last glacial-interglacial cycle using benthic foraminiferal Zn/Ca, which is strongly affected by saturation state during calcite precipitation. Our data are in agreement with the CaCO3 compensation theory, including glacial CO3[2-] concentrations similar to (or slightly lower than) today, and a Termination I CO3[2-] peak of ~25-30 µmol kg**-1. The deglacial CO3[2-] rise precedes ice sheet melting, consistent with the timing of the atmospheric CO2 rise. A later portion of the peak could reflect removal of CO2 from the atmosphere-ocean system due to boreal forest regrowth. CaCO3 compensation alone may explain more than one third of the atmospheric CO2 lowering during glacial times.
    Keywords: Cadmium/Calcium ratio; DEPTH, sediment/rock; Manganese/Calcium ratio; PC; Piston corer; RC13; RC13-114; Robert Conrad; Zinc/Calcium ratio
    Type: Dataset
    Format: text/tab-separated-values, 202 data points
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