The Deep Ocean Density Structure at the Last Glacial Maximum: What Was It and Why?
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- Type
- dissertation
- Published
- 2014-01-01
- Cited by
- 3
- References
- 140
- OpenAlex
- https://openalex.org/W71718910
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:126701025
Keywords
Last Glacial Maximum, Oceanography, Geology, Interglacial, Deep sea
References
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- Aseismic Deformation in Subduction Megathrusts: Central Andes and North-East Japan
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- Description of a hydraulic sediment squeezer
- Tracer transport timescales and the observed Atlantic‐Pacific lag in the timing of the Last Termination
- Inverse problem theory - and methods for model parameter estimation
- Early Diagenesis: A Theoretical Approach
- Parameter estimation and inverse problems
- Glacial/interglacial variations in atmospheric carbon dioxide
- Temperature and carbonate ion effects on Mg/Ca and Sr/Ca ratios in benthic foraminifera: Aragonitic species Hoeglundina elegans
- Diurnal to decadal global forcing for ocean and sea-ice models: The data sets and flux climatologies
- Impact of strong deep ocean stratification on the glacial carbon cycle
- Oceanic vertical mixing: a review and a model with a nonlocal boundary layer parameterization
- BEDMAP: a new ice thickness and subglacial topographic model of Antarctica
- Formation and discharge of deep and bottom water in the northwestern Weddell Sea
- Calibration of the 14C timescale over the past 30,000 years using mass spectrometric U–Th ages from Barbados corals
- Modeling ice shelf cavities in a z coordinate ocean general circulation model
- An Evaluation of Publicly Available Global Bathymetry Grids
- Melting and freezing beneath Filchner‐Ronne Ice Shelf, Antarctica
- Circulation and bottom water production in the Weddell Sea
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