Search Results - "Umling, N. E."

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  1. 1

    Deglacial Carbon Escape From the Northern Rim of the Southern Ocean by Umling, N. E., Sikes, E., Rafter, P., Goodkin, N. F., Southon, J. R.

    Published in Geophysical research letters (28-04-2024)
    “…The Southern Ocean regulates atmospheric CO2 and Earth's climate as a critical region for air‐sea gas exchange, delicately poised between being a CO2 source…”
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    Journal Article
  2. 2

    Proximity to Undersaturation and the Influences on G. bulloides Area‐Density in Southern Indian Ocean Marine Sediments by Umling, N. E., Saad, B., Sikes, E., Goodkin, N. F.

    Published in Paleoceanography and paleoclimatology (01-06-2021)
    “…The area density proxy of foraminiferal shell thickness and calcification intensity has the potential to provide information about past ocean CO2 content and…”
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  3. 3

    Deglacial Temperature and Carbonate Saturation State Variability in the Tropical Atlantic at Antarctic Intermediate Water Depths by Oppo, D. W., Lu, W., Huang, K.‐F., Umling, N. E., Guo, W., Yu, J., Curry, W. B., Marchitto, T. M., Wang, S.

    Published in Paleoceanography and paleoclimatology (01-09-2023)
    “…Variations in the Atlantic Meridional Overturning Circulation (AMOC) redistribute heat and nutrients, causing pronounced anomalies of temperature and nutrient…”
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  4. 4

    Deepwater Expansion and Enhanced Remineralization in the Eastern Equatorial Pacific During the Last Glacial Maximum by Umling, N. E., Thunell, R. C., Bizimis, M.

    Published in Paleoceanography and paleoclimatology (01-06-2018)
    “…Published estimates of the radiocarbon content of middepth waters suggest a decrease in ventilation in multiple locations during the last glacial maximum (LGM;…”
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  5. 5

    Atlantic Circulation and Ice Sheet Influences on Upper South Atlantic Temperatures During the Last Deglaciation by Umling, N. E., Oppo, D. W., Chen, P., Yu, J., Liu, Z., Yan, M., Gebbie, G., Lund, D. C., Pietro, K. R., Jin, Z. D., Huang, K.‐F., Costa, K. B., Toledo, F. A. L.

    Published in Paleoceanography and paleoclimatology (01-06-2019)
    “…Atlantic Meridional Overturning Circulation (AMOC) disruption during the last deglaciation is hypothesized to have caused large subsurface ocean temperature…”
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    Journal Article