scholarly article | Q13442814 |
P819 | ADS bibcode | 2006GGG.....710N03L |
P356 | DOI | 10.1029/2005GC001226 |
P50 | author | Delia Oppo | Q57164974 |
Jean Lynch-Stieglitz | Q58109957 | ||
P2093 | author name string | William B. Curry | |
Christopher D. Charles | |||
Ulysses S. Ninneman | |||
Jenna Munson | |||
P2860 | cites work | Benthic foraminiferal Mg/Ca-paleothermometry: a revised core-top calibration | Q29037551 |
Mid-Depth Circulation of the Subpolar North Atlantic During the Last Glacial Maximum | Q29301537 | ||
Improved estimates of global ocean circulation, heat transport and mixing from hydrographic data | Q30620397 | ||
Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes | Q34315674 | ||
Meltwater pulse 1A from Antarctica as a trigger of the Bølling-Allerød warm interval | Q47314359 | ||
Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical Evidence | Q47585729 | ||
North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature | Q56444055 | ||
Intermediate depth warming in the tropical Atlantic related to weakened thermohaline circulation: Combining paleoclimate data and modeling results for the last deglaciation | Q58081247 | ||
Temperature and carbonate ion effects on Mg/Ca and Sr/Ca ratios in benthic foraminifera: Aragonitic speciesHoeglundina elegans | Q58244941 | ||
Evidence for enhanced mixing over rough topography in the abyssal ocean | Q59048300 | ||
A 210,000-year record of barium variability in the deep northwest Atlantic Ocean | Q59065133 | ||
Weaker Gulf Stream in the Florida Straits during the Last Glacial Maximum | Q59068682 | ||
Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data | Q59088380 | ||
Constraints on the ocean oxygen isotopic enrichment between the Last Glacial Maximum and the Holocene: Paleoceanographic implications | Q59407375 | ||
Similar glacial and Holocene deep water circulation inferred from southeast Pacific benthic foraminiferal carbon isotope composition | Q60149980 | ||
Spatial Variability of Turbulent Mixing in the Abyssal Ocean | Q73182440 | ||
Using ocean margin density to constrain ocean circulation and surface wind strength in the past | Q105427102 | ||
A geostrophic transport estimate for the Florida Current from the oxygen isotope composition of benthic foraminifera | Q105427108 | ||
Trade wind forcing of upwelling, seasonally, and Heinrich events as a response to sub-Milankovitch climate variability | Q107105105 | ||
P433 | issue | 10 | |
P921 | main subject | last glacial maximum | Q1979625 |
Atlantic meridional overturning circulation | Q4652675 | ||
P577 | publication date | 2006-10-01 | |
P1433 | published in | G3: Geochemistry, Geophysics, Geosystems | Q15759647 |
P1476 | title | Meridional overturning circulation in the South Atlantic at the last glacial maximum | |
P478 | volume | 7 |
Q105427035 | Assessing the Ability of Zonal δ 18 O Contrast in Benthic Foraminifera to Reconstruct Deglacial Evolution of Atlantic Meridional Overturning Circulation |
Q58073979 | Data Constraints on Glacial Atlantic Water Mass Geometry and Properties |
Q58239133 | Muted change in Atlantic overturning circulation over some glacial-aged Heinrich events |
Q101245975 | Paleocirculation and Ventilation History of Southern Ocean Sourced Deep Water Masses During the Last 800,000 Years |
Search more.