Meridional overturning circulation in the South Atlantic at the last glacial maximum

scientific article published in October 2006

Meridional overturning circulation in the South Atlantic at the last glacial maximum is …
instance of (P31):
scholarly articleQ13442814

External links are
P819ADS bibcode2006GGG.....710N03L
P356DOI10.1029/2005GC001226

P50authorDelia OppoQ57164974
Jean Lynch-StieglitzQ58109957
P2093author name stringWilliam B. Curry
Christopher D. Charles
Ulysses S. Ninneman
Jenna Munson
P2860cites workBenthic foraminiferal Mg/Ca-paleothermometry: a revised core-top calibrationQ29037551
Mid-Depth Circulation of the Subpolar North Atlantic During the Last Glacial MaximumQ29301537
Improved estimates of global ocean circulation, heat transport and mixing from hydrographic dataQ30620397
Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changesQ34315674
Meltwater pulse 1A from Antarctica as a trigger of the Bølling-Allerød warm intervalQ47314359
Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical EvidenceQ47585729
North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperatureQ56444055
Intermediate depth warming in the tropical Atlantic related to weakened thermohaline circulation: Combining paleoclimate data and modeling results for the last deglaciationQ58081247
Temperature and carbonate ion effects on Mg/Ca and Sr/Ca ratios in benthic foraminifera: Aragonitic speciesHoeglundina elegansQ58244941
Evidence for enhanced mixing over rough topography in the abyssal oceanQ59048300
A 210,000-year record of barium variability in the deep northwest Atlantic OceanQ59065133
Weaker Gulf Stream in the Florida Straits during the Last Glacial MaximumQ59068682
Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical dataQ59088380
Constraints on the ocean oxygen isotopic enrichment between the Last Glacial Maximum and the Holocene: Paleoceanographic implicationsQ59407375
Similar glacial and Holocene deep water circulation inferred from southeast Pacific benthic foraminiferal carbon isotope compositionQ60149980
Spatial Variability of Turbulent Mixing in the Abyssal OceanQ73182440
Using ocean margin density to constrain ocean circulation and surface wind strength in the pastQ105427102
A geostrophic transport estimate for the Florida Current from the oxygen isotope composition of benthic foraminiferaQ105427108
Trade wind forcing of upwelling, seasonally, and Heinrich events as a response to sub-Milankovitch climate variabilityQ107105105
P433issue10
P921main subjectlast glacial maximumQ1979625
Atlantic meridional overturning circulationQ4652675
P577publication date2006-10-01
P1433published inG3: Geochemistry, Geophysics, GeosystemsQ15759647
P1476titleMeridional overturning circulation in the South Atlantic at the last glacial maximum
P478volume7

Reverse relations

cites work (P2860)
Q105427035Assessing the Ability of Zonal δ 18 O Contrast in Benthic Foraminifera to Reconstruct Deglacial Evolution of Atlantic Meridional Overturning Circulation
Q58073979Data Constraints on Glacial Atlantic Water Mass Geometry and Properties
Q58239133Muted change in Atlantic overturning circulation over some glacial-aged Heinrich events
Q101245975Paleocirculation and Ventilation History of Southern Ocean Sourced Deep Water Masses During the Last 800,000 Years

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