Changes in deep water hydrology during the Last Deglaciation
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J. Duplessy | E. Cortijo | C. Waelbroeck | E. Michel | L. Labeyrie | Changes in deep | water hydrology | during the | Last Deglaciation | Elsa Claire Waelbroeck
[1] Elsa Cortijo,et al. Temporal variability of the surface and deep waters of the North West Atlantic Ocean at orbital and , 2013 .
[2] F. Guichard,et al. Distant origin of circulation changes in the Indian Ocean during the last deglaciation , 2006 .
[3] J. Duplessy,et al. Heinrich events: hydrological impact , 2005 .
[4] N. Shackleton,et al. An Atlantic lead over Pacific deep-water change across Termination I: implications for the application of the marine isotope stage stratigraphy , 2005 .
[5] J. McManus,et al. Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes , 2004, Nature.
[6] H. Elderfield,et al. Millennial‐scale variability of deep‐water temperature and δ18Odw indicating deep‐water source variations in the Northeast Atlantic, 0–34 cal. ka BP , 2003 .
[7] G. Knorr,et al. Southern Ocean origin for the resumption of Atlantic thermohaline circulation during deglaciation , 2003, Nature.
[8] R. Zahn,et al. Suborbital intermediate water variability inferred from paired benthic foraminiferal Cd/Ca and δ13C in the tropical West Atlantic and linking with North Atlantic climates , 2002 .
[9] Laurent Labeyrie,et al. Changes in North Atlantic deep-water formation associated with the Dansgaard–Oeschger temperature oscillations (60–10 ka) , 2002 .
[10] Didier Paillard,et al. The timing of the last deglaciation in North Atlantic climate records , 2001, Nature.
[11] F. Joos,et al. Ocean thermohaline circulation and sedimentary 231Pa/230Th ratio , 2000 .
[12] N. Shackleton,et al. Phase relationships between millennial‐scale events 64,000–24,000 years ago , 2000 .
[13] W. Curry,et al. Calibration of stable isotopic data: An enriched δ18O standard used for source gas mixing detection and correction , 2000 .
[14] E. Cortijo,et al. A simulation of the Atlantic meridional circulation during Heinrich event 4 using reconstructed sea surface temperatures and salinities , 1999 .
[15] S. Marshall,et al. Modeling North American Freshwater Runoff through the Last Glacial Cycle , 1999, Quaternary Research.
[16] E. Jansen,et al. Rapid changes in the mechanism of ocean convection during the last glacial period , 1999, Nature.
[17] Pascal Yiou,et al. Macintosh Program performs time‐series analysis , 1996 .
[18] Elsa Cortijo,et al. SURFACE AND DEEP HYDROLOGY OF THE NORTHERN ATLANTIC OCEAN DURING THE PAST 150 000 YEARS , 1995 .
[19] D. Paillard,et al. Role of the thermohaline circulation in the abrupt warming after Heinrich events , 1994, Nature.
[20] Laurent Labeyrie,et al. Changes in east Atlantic deepwater circulation over the last 30 , 1994 .
[21] J. Jouzel,et al. Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores , 1993, Nature.
[22] W. Broecker,et al. Correlations between climate records from North Atlantic sediments and Greenland ice , 1993, Nature.
[23] W. Broecker,et al. Evidence for massive discharges of icebergs into the North Atlantic ocean during the last glacial period , 1992, Nature.
[24] J. Duplessy,et al. Changes in surface salinity of the North Atlantic Ocean during the last deglaciation , 1992, Nature.
[25] T. Stocker,et al. Rapid transitions of the ocean's deep circulation induced by changes in surface water fluxes , 1991, Nature.
[26] J. Duplessy,et al. How fast did the ocean—atmosphere system run during the last deglaciation? , 1991 .
[27] J. Duplessy,et al. A deep hydrological front between intermediate and deep-wafpr , masses in the glacial Indian Ocean , 1988, Nature.
[28] Laurent Labeyrie,et al. Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulation , 1988 .
[29] W. Broecker,et al. The chronology of the last deglaciation: implications to the cause of the Younger Dryas event , 1988 .
[30] J. Duplessy,et al. Retreat velocity of the North Atlantic polar front during the last deglaciation determined by 14C accelerator mass spectrometry , 1987, Nature.
[31] N. J. Shackleton,et al. Carbon isotope data in core V19-30 confirm reduced carbon dioxide concentration in the ice age atmosphere , 1983, Nature.
[32] A. Savitzky,et al. Smoothing and Differentiation of Data by Simplified Least Squares Procedures. , 1964 .
[33] H. Stommel,et al. Thermohaline Convection with Two Stable Regimes of Flow , 1961 .
[34] C. Levi. Etude des variations climatiques de la zone Indo-Pacifique : rôle des basses latitudes dans la variabilité millénaire du climat , 2003 .
[35] T. Stocker,et al. The History of Climate Dynamics in the Late Quaternary , 2003 .
[36] S. John,et al. Comparison of oxygen isotope records from the GISP 2 and GRIP Greenland ice cores , 2002 .
[37] L. Sloan,et al. Sea Level Change Through the Last Glacial Cycle , 2001 .
[38] Robert S. Webb,et al. Mechanisms of global climate change at millennial time scales , 1999 .
[39] J. Duplessy,et al. Changes in sea surface hydrology associated with Heinrich event 4 in the North Atlantic Ocean between 40° and 60°N , 1997 .
[40] J. Duplessy,et al. Evidence for changes in the North Atlantic Deep Water linked to meltwater surges during the Heinrich events , 1997 .
[41] J. Duplessy,et al. North Atlantic sea surface conditions during the Younger Dryas cold event , 1996, Geological Society, London, Special Publications.
[42] P. Reimer,et al. Extended 14C Data Base and Revised CALIB 3.0 14C Age Calibration Program , 1993, Radiocarbon.
[43] P. Kroopnick. The distribution of 13C of ΣCO2 in the world oceans , 1985 .
[44] J. Steinier,et al. Smoothing and differentiation of data by simplified least square procedure. , 1972, Analytical chemistry.