About: Deepwater circulation on Blake Outer Ridge (western North Atlantic) during the Holocene, Younger Dryas, and Last Glacial Maximum

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About: Deepwater circulation on Blake Outer Ridge (western North Atlantic) during the Holocene, Younger Dryas, and Last Glacial Maximum Goto Sponge NotDistinct Permalink

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scholarly article

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rdf:type	Item
description	wetenschappelijk artikel (nl) scholarly article (en) наукова стаття, опублікована в березні 2008 (uk) im März 2008 veröffentlichter wissenschaftlicher Artikel (de)
publication date	wds:Q57532748-11BB81F6-BBC9-4D68-BCE8-96CFF494BA23
publication date	2008-03-01 00:00:00Z (xsd:dateTime)
cites work	wds:Q57532748-03CC0605-08D0-4E54-AC3D-71384202FB78 wds:Q57532748-0C0E185F-BCF0-4D0F-92A5-3EC674E93D94 wds:Q57532748-14AF353A-DF69-446D-BB44-FCD8B4509A0E wds:Q57532748-1BD7411F-6A13-4F3C-9464-5F8190370E80 wds:Q57532748-1EF97DC0-0F77-4C2C-BD56-D1B027F27D8A wds:Q57532748-1F96214F-FC18-4501-B5C6-A5659333EFF1 wds:Q57532748-21645B5D-5127-451B-BE56-1692260A2B90 wds:Q57532748-26319ACD-5510-4896-8810-F7A7A0A08C73 wds:Q57532748-34386039-1814-4670-B34D-341C2E16B1C3 wds:Q57532748-3C7101ED-8040-4E59-9B72-1D2EB4309E2C wds:Q57532748-4CBF58E0-9BE7-49E4-A8A0-52905F4C119A wds:Q57532748-50102371-583E-4648-AD47-6F5666A992A2 wds:Q57532748-5666389C-2E8A-4BF3-A3FC-5BE35FC40F48 wds:Q57532748-5F219606-8A43-4F76-9F6F-D48571F2014A wds:Q57532748-6064740B-C798-4485-B2C6-039B80AB514A wds:Q57532748-61B8BFCB-DC4A-4BC5-AAA4-1DA7C4AEEB96 wds:Q57532748-62E7BF18-7452-4598-A4ED-25303B0EA8BF wds:Q57532748-64556F04-0D26-4E30-8C1D-6D990F188DF4 wds:Q57532748-6C88348D-D832-463B-9C65-DCA4FB86FCA3 wds:Q57532748-727546AD-88FB-4098-AD6C-F18D0CBAF723 wds:Q57532748-7E0B7638-031F-45D5-9F98-1BCF01FF9637 wds:Q57532748-8B35AB58-EA88-410B-8BE8-BFC385CDCC4D wds:Q57532748-9606B922-D869-4C5D-A132-01D667AD6E70 wds:Q57532748-99EA7413-417D-40E9-B49E-C2CB050B12D0 wds:Q57532748-A12FE884-9C7A-4EA7-AD36-53CCCBCD2315 wds:Q57532748-A545F849-B07B-4145-B1E3-DD8D9AF53107 wds:Q57532748-AEE5F584-4E42-4A96-93EA-1AF0B4553E31 wds:Q57532748-B1A03DCF-E011-4F33-9EFE-7B454A1D0851 wds:Q57532748-C23CB41C-EEFC-4D2F-AF18-E48186CCB01A wds:Q57532748-C7AC15B5-E880-42FA-B4FA-11D3BD1C3266 wds:Q57532748-D49D59DA-B3DF-4271-B8AB-727778F605DF wds:Q57532748-D9B6EBFD-7B1B-4EC1-BED8-BC5BCB638591 wds:Q57532748-DEA6F208-4D18-4350-A945-FA0EDACFA974 wds:Q57532748-DEF5C4F6-15E1-40D7-B736-B2FCD2A27C21 wds:Q57532748-FB41D777-9AAD-460B-8DEC-4C3E4F6A4F49 wds:Q57532748-FCEAD6C3-1893-44B6-A4C1-DBA0F23289A9 wds:Q57532748-FE3760F4-BA2C-4B64-822B-44B9B641ACBF
cites work	Oxygen 18/16 variability in Greenland snow and ice with 10−3- to 105-year time resolution Mid-Depth Circulation of the Subpolar North Atlantic During the Last Glacial Maximum North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature Does the ocean–atmosphere system have more than one stable mode of operation? Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data Intcal04 Terrestrial Radiocarbon Age Calibration, 0–26 Cal Kyr BP The Little Ice Age and Medieval Warm Period in the Sargasso Sea Weaker Gulf Stream in the Florida Straits during the Last Glacial Maximum Deep Flow along the Western Boundary South of the Blake Bahama Outer Ridge A 210,000-year record of barium variability in the deep northwest Atlantic Ocean Paleocean circulation during the Last Deglaciation: A bipolar seesaw? Coupled ocean-atmosphere model response to freshwater input: Comparison to Younger Dryas Event Ocean circulation and climate during the past 120,000 years Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes Radiocarbon variability in the western North Atlantic during the last deglaciation Cooling and ventilating the Abyssal Ocean Intensified deep Pacific inflow and ventilation in Pleistocene glacial times Shaping of the continental rise by deep geostrophic contour currents Atlantic meridional overturning circulation during the Last Glacial Maximum Simulation of modern and glacial climates with a coupled global model of intermediate complexity Sortable silt and fine sediment size/composition slicing: Parameters for palaeocurrent speed and palaeoceanography Accelerated drawdown of meridional overturning in the late-glacial Atlantic triggered by transient pre-H event freshwater perturbation Deep water mass geometry in the glacial Atlantic Ocean: A review of constraints from the paleonutrient proxy Cd/Ca Size sorting in marine muds: Processes, pitfalls, and prospects for paleoflow-speed proxies Measurement of the sortable silt current speed proxy using the Sedigraph 5100 and Coulter Multisizer IIe: precision and accuracy Ocean thermohaline circulation and sedimentary231Pa/230Th ratio Marine control of biological production in the eastern equatorial Pacific Ocean Millennial-scale changes in North Atlantic circulation since the last glaciation Rapid climate transitions in a coupled ocean–atmosphere model The influence of air and sea exchange on the carbon isotope distribution in the sea The high-velocity core of the Western boundary undercurrent at the base of the u.s. Continental rise Paleoceanography of the Deep Western Boundary Undercurrent on the North American continental margin for the past 25 000 yr Excepftonally strong near-bottom flows on the continental rise of nova scotia Deep Western Boundary Current variability in the subtropical northwest Atlantic Ocean during marine isotope stages 12-10 Abyssal currents and advection of resuspended sediment along the northeastern Bermuda Rise Antarctic link to deep flow speed variation during Marine Isotope Stage 3 in the western North Atlantic
author name string	wds:Q57532748-0A63793F-7FDD-4F8E-809E-863405689DFE
author name string	Helena K. Evans
rdfs:label	Deepwater circulation on Blake Outer Ridge (western North Atlantic) during the Holocene, Younger Dryas, and Last Glacial Maximum (en) Deepwater circulation on Blake Outer Ridge (western North Atlantic) during the Holocene, Younger Dryas, and Last Glacial Maximum (nl)
skos:prefLabel	Deepwater circulation on Blake Outer Ridge (western North Atlantic) during the Holocene, Younger Dryas, and Last Glacial Maximum (en) Deepwater circulation on Blake Outer Ridge (western North Atlantic) during the Holocene, Younger Dryas, and Last Glacial Maximum (nl)
name	Deepwater circulation on Blake Outer Ridge (western North Atlantic) during the Holocene, Younger Dryas, and Last Glacial Maximum (en) Deepwater circulation on Blake Outer Ridge (western North Atlantic) during the Holocene, Younger Dryas, and Last Glacial Maximum (nl)
author	wds:Q57532748-4E4980CC-4C49-4D08-8D0E-F038C4C7D8AD
author	Ian R. Hall
title	wds:Q57532748-466588BE-A34F-4581-A340-65684CB89D36
title	Deepwater circulation on Blake Outer Ridge (western North Atlantic) during the Holocene, Younger Dryas, and Last Glacial Maximum (en)
instance of	wds:Q57532748-B2DC0A2F-78DF-431D-AC1F-48772D2D017E
instance of	scholarly article
main subject	wds:Q57532748-25BC46B0-390A-4298-8181-9B242CCD5E3A wds:Q57532748-C6E958AC-ECC5-42D8-BBE1-2C5DC2CE870E
main subject	Younger Dryas last glacial maximum
published in	wds:Q57532748-15B8E808-2023-4D10-A463-D2E1FF6AD17C

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