Search Results - "Schmittner, A."

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  1. 1

    Complementary constraints from carbon (13C) and nitrogen (15N) isotopes on the glacial ocean's soft‐tissue biological pump by Schmittner, A., Somes, C. J.

    Published in Paleoceanography (01-06-2016)
    “…A three‐dimensional, process‐based model of the ocean's carbon and nitrogen cycles, including 13C and 15N isotopes, is used to explore effects of idealized…”
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  2. 2

    Air-sea disequilibrium enhances ocean carbon storage during glacial periods by Khatiwala, S, Schmittner, A, Muglia, J

    Published in Science advances (01-06-2019)
    “…The prevailing hypothesis for lower atmospheric carbon dioxide (CO ) concentrations during glacial periods is an increased efficiency of the ocean's biological…”
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  3. 3

    Early deglacial Atlantic overturning decline and its role in atmospheric CO2 rise inferred from carbon isotopes (?13C) by Schmittner, A, Lund, D C

    Published in Climate of the past (01-01-2015)
    “…The reason for the initial rise in atmospheric CO2 during the last deglaciation remains unknown. Most recent hypotheses invoke Southern Hemisphere processes…”
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  4. 4

    Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting by Bakker, P., Schmittner, A., Lenaerts, J. T. M., Abe‐Ouchi, A., Bi, D., Broeke, M. R., Chan, W.‐L., Hu, A., Beadling, R. L., Marsland, S. J., Mernild, S. H., Saenko, O. A., Swingedouw, D., Sullivan, A., Yin, J.

    Published in Geophysical research letters (16-12-2016)
    “…The most recent Intergovernmental Panel on Climate Change assessment report concludes that the Atlantic Meridional Overturning Circulation (AMOC) could weaken…”
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  5. 5

    Model projections of the North Atlantic thermohaline circulation for the 21st century assessed by observations by Schmittner, A., Latif, M., Schneider, B.

    Published in Geophysical research letters (01-12-2005)
    “…Most climate models predict a weakening of the North Atlantic thermohaline circulation for the 21st century when forced by increasing levels of greenhouse gas…”
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  6. 6

    Biology and air–sea gas exchange controls on the distribution of carbon isotope ratios (δ 13 C) in the ocean by Schmittner, A, Gruber, N, Mix, A. C, Key, R. M, Tagliabue, A, Westberry, T. K

    Published in Biogeosciences (04-09-2013)
    “…Analysis of observations and sensitivity experiments with a new three-dimensional global model of stable carbon isotope cycling elucidate processes that…”
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  7. 7

    Glacial ocean overturning intensified by tidal mixing in a global circulation model by Schmittner, A., Green, J. A. M., Wilmes, S.-B.

    Published in Geophysical research letters (28-05-2015)
    “…Due to lower sea levels during the Last Glacial Maximum (LGM), tidal energy dissipation was shifted from the shallow margins into the deep ocean. Here using a…”
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  8. 8

    Southwest Atlantic water mass evolution during the last deglaciation by Lund, D. C., Tessin, A. C., Hoffman, J. L., Schmittner, A.

    Published in Paleoceanography (01-05-2015)
    “…The rise in atmospheric CO2 during Heinrich Stadial 1 (HS1; 14.5–17.5 kyr B.P.) may have been driven by the release of carbon from the abyssal ocean. Model…”
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  9. 9

    Isotopic constraints on the pre-industrial oceanic nitrogen budget by Somes, C. J, Oschlies, A, Schmittner, A

    Published in Biogeosciences (06-09-2013)
    “…The size of the bioavailable (i.e., "fixed") nitrogen inventory in the ocean influences global marine productivity and the biological carbon pump. Despite its…”
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  10. 10

    Simulating the impact of the Panamanian seaway closure on ocean circulation, marine productivity and nutrient cycling by Schneider, Birgit, Schmittner, Andreas

    Published in Earth and planetary science letters (30-06-2006)
    “…The closure of the Panama Isthmus, ∼14–3 Ma, caused large reorganizations of ocean circulation. Here we use a global climate–ocean ecosystem model to…”
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  12. 12

    Glacial Ice Sheet Extent Effects on Modeled Tidal Mixing and the Global Overturning Circulation by Wilmes, S.‐B., Schmittner, A., Green, J. A. M.

    Published in Paleoceanography and paleoclimatology (01-08-2019)
    “…At present, tides supply approximately half (1 TW) of the energy necessary to sustain the global deep meridional overturning circulation (MOC) through…”
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  13. 13

    Climatic Consequences of a Pine Island Glacier Collapse by Green, J. A. M., Schmittner, A.

    Published in Journal of climate (01-12-2015)
    “…An intermediate-complexity climate model is used to simulate the impact of an accelerated Pine Island Glacier mass loss on the large-scale ocean circulation…”
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  14. 14

    An improved parameterization of tidal mixing for ocean models by Schmittner, A, Egbert, G. D

    Published in Geoscientific model development (28-01-2014)
    “…Two modifications to an existing scheme of tidal mixing are implemented in the coarse resolution ocean component of a global climate model. First, the vertical…”
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  15. 15

    A global model of the marine ecosystem for long-term simulations: Sensitivity to ocean mixing, buoyancy forcing, particle sinking, and dissolved organic matter cycling by Schmittner, A., Oschlies, A., Giraud, X., Eby, M., Simmons, H. L.

    Published in Global biogeochemical cycles (01-09-2005)
    “…A new model of the marine ecosystem coupled into a global Earth System Climate Model suitable for long‐term (multimillennial timescale) simulations is…”
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  16. 16

    Mid-Pliocene shifts in ocean overturning circulation and the onset of Quaternary-style climates by Sarnthein, M., Bartoli, G., Prange, M., Schmittner, A., Schneider, B., Weinelt, M., Andersen, N., Garbe-Schönberg, D.

    Published in Climate of the past (30-06-2009)
    “…A major tipping point of Earth's history occurred during the mid-Pliocene: the onset of major Northern-Hemisphere Glaciation (NHG) and of pronounced,…”
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  17. 17

    Early deglacial Atlantic overturning decline and its role in atmospheric CO 2 rise inferred from carbon isotopes (δ 13 C) by Schmittner, A., Lund, D. C.

    Published in Climate of the past (05-02-2015)
    “…The reason for the initial rise in atmospheric CO2 during the last deglaciation remains unknown. Most recent hypotheses invoke Southern Hemisphere processes…”
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    Journal Article
  18. 18

    Coupling of the hemispheres in observations and simulations of glacial climate change by Schmittner, A., Saenko, O.A., Weaver, A.J.

    Published in Quaternary science reviews (01-03-2003)
    “…We combine reconstructions, climate model simulations and a conceptual model of glacial climate change on millennial time scales to examine the relation…”
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  19. 19

    Evaluation of a present-day climate simulation with a new coupled atmosphere-ocean model GENMOM by Alder, J R, Hostetler, S W, Pollard, D, Schmittner, A

    Published in Geoscientific Model Development (01-01-2011)
    “…We present a new, non-flux corrected AOGCM, GENMOM, that combines the GENESIS version 3 atmospheric GCM (Global Environmental and Ecological Simulation of…”
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  20. 20

    Calcium carbonate production response to future ocean warming and acidification by Pinsonneault, A. J, Matthews, H. D, Galbraith, E. D, Schmittner, A

    Published in Biogeosciences (29-06-2012)
    “…Anthropogenic carbon dioxide (CO2) emissions are acidifying the ocean, affecting calcification rates in pelagic organisms, and thereby modifying the oceanic…”
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