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Paleosalinity
Modeling the Paleocirculation of the Mediterranean
New Oceanic Proxies for Paleoclimate
Climate and Deep Water Formation Regions
Meteorology and Oceanography of the Middle East
Reconstruction of Past Changes in Ocean Salinity – a Compound Specific Stable Hydrogen Isotope Approach
Constraints on Surface Seawater Oxygen Isotope Change Between the Last Glacial Maximum and the Late Holocene
International Ocean Discovery Program Expedition 369 Preliminary Report
VARIATIONSUS CLIVAR VARIATIONS CUS CLIVAR Lim Ity a Bil Te V Cta Ariability & Predi
High-Resolution Sea Surface Reconstructions Off Cape Hatteras Over the Last 10 Ka C
Paleosalinity: Confidence Limits and Future Applications
Chapter 4, Potential for Abrupt Change in the Atlantic Meridional Overturning Circulation, Final Report, Abrupt Climate Change
Eastern Pacific Warm Pool Paleosalinity and Climate Variability: 0-30 Ky
Simulation of Oxygen Isotopes in a Global Ocean Model A. Paul*, S. Mulitza, J. Pätzold and T. Wolff
Integrated Microfossil and OC-Sr Isotopic Evidence from the Late
Is Ocean Thermohaline Circulation Linked to Abrupt Stadial/Interstadial Transitions? Edward A
The Atlantic Ocean at the Last Glacial Maximum: 1
Arctic Closure As a Trigger for Atlantic Overturning at the Eocene-Oligocene Transition
Global Climate Evolution During the Last Deglaciation PNAS PLUS
Top View
Oxygen and Carbon Isotopes and Coral Growth in the Gulf Of
Coupled Model Simulations of the Last Glacial Maximum, Last Interglacial and Late Holocene
A Late Holocene Reconstruction of Ocean Climate Variability in The
A Simulation of the Atlantic Meridional Circulation During Heinrich Event 4 Using Reconstructed Sea Surface Temperatures and Salinities Didier Paillard, Elsa Cortijo