About: North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature

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scientific article published in Nature

Attributes	Values
rdf:type	Item
description	artículu científicu (ast) wetenschappelijk artikel (nl) article publié dans la revue scientifique Nature (fr) নেচারে প্রকাশিত বৈজ্ঞানিক প্রবন্ধ (bn) scientific article published in Nature (en) im November 1987 veröffentlichter wissenschaftlicher Artikel (de) наукова стаття, опублікована в Nature в листопаді 1987 (uk)
publication date	wds:Q56444055-AFCFF2AE-E846-40C5-A487-047273B626F5
publication date	1987-11-01 00:00:00Z (xsd:dateTime)
language of work or name	wds:Q56444055-FBC4E566-5504-4640-8010-37F49DCA4A93
language of work or name	English
exact match	wds:Q56444055-B5487BDE-0907-4B66-AEDA-E7F42F2C4E9A
exact match	https://scigraph.springernature.com/pub.10.1038/330035a0
author name string	wds:Q56444055-F20BD948-5622-411E-B826-CD18F441F19C
author name string	Lloyd Keigwin
rdfs:label	North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature (en) North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature (nl)
skos:prefLabel	North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature (en) North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature (nl)
name	North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature (en) North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature (nl)
author	wds:Q56444055-383F9E19-E4B8-47B7-B6E4-93197B5808C9
author	Edward A. Boyle
title	wds:Q56444055-62B2F0B3-6068-4195-A9B7-9218C205B321
title	North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature (en)
page(s)	wds:Q56444055-9D51A423-8D49-49A5-B119-64C012E0C963
page(s)	35-40
instance of	wds:Q56444055-A87E4C4E-B7B5-49E8-80AE-4FF2D2120A57
instance of	scholarly article
main subject	wds:Q56444055-7F4D87B8-B701-44E7-80EE-50B57A79D2A4
main subject	thermohaline circulation
published in	wds:Q56444055-0D122082-3EE9-46E9-AD92-4B2BB5BE62F2
published in	Nature
issue	wds:Q56444055-BC1CD038-1089-4612-87A3-DDB83A8AFCEE
volume	wds:Q56444055-7784633B-4C5F-42E6-BEC4-C7D45C707438
issue	6143
volume	330
DOI	wds:Q56444055-8ECB11C7-0101-4BE3-A03E-8E67EB4B21C5
DOI	http://dx.doi.org/10.1038/330035A0
DOI	10.1038/330035A0
ResearchGate publication ID	wds:Q56444055-E3772E57-6845-4D4F-98BC-F6A6CD3A211D
ResearchGate publication ID	230888927
ADS bibcode	wds:Q56444055-29FD9439-9CA3-4DEF-A147-42F796856D20
ADS bibcode	1987Natur.330...35B
Dimensions Publication ID	wds:Q56444055-028B19C0-1E37-4D94-A769-8A50E4C3CF60
Dimensions Publication ID	1049557202
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q56444055
is cites work of	Bifurcations of the Atlantic thermohaline circulation in response to changes in the hydrological cycle The role of the deep ocean in North Atlantic climate change between 70 and 130 kyr ago Atlantic overturning responses to Late Pleistocene climate forcings. A 20,000-year record of ocean circulation and climate change from the Santa Barbara basin The oceanic salt pump: Does it contribute to the glacial-interglacial difference in atmospheric CO2 content? The distribution of radiocarbon in the glacial ocean Deglacial meltwater discharge, North Atlantic Deep Circulation, and abrupt climate change Western North Atlantic evidence for millennial-scale changes in ocean circulation and climate Characteristics of the deep ocean carbon system during the past 150,000 years: SigmaCO2 distributions, deep water flow patterns, and abrupt climate change Sudden changes in North Atlantic circulation during the last deglaciation The δ13C in benthic foraminiferal tests ofFontbotia wuellerstorfi(Schwager) Relative to the δ13C of dissolved inorganic carbon in Southern Ocean Deep Water: Implications for glacial ocean circulation models A deep hydrological front between intermediate and deep-wafpr , masses in the glacial Indian Ocean Evidence for two-step deglaciation and its impact on North Atlantic deep-water circulation Late Quaternary paleoproductivity and deep water circulation in the eastern South Atlantic Ocean: Evidence from benthic foraminifera Barium content of benthic foraminifera controlled by bottom-water composition A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation A 0.5-million-year record of millennial-scale climate variability in the north atlantic A geostrophic transport estimate for the Florida Current from the oxygen isotope composition of benthic foraminifera Weaker Gulf Stream in the Florida Straits during the Last Glacial Maximum Effect of the formation of the Isthmus of Panama on Atlantic Ocean thermohaline circulation Variability of the North Atlantic thermohaline circulation during the last interglacial period Strong and deep Atlantic meridional overturning circulation during the last glacial cycle Global climate evolution during the last deglaciation A 210,000-year record of barium variability in the deep northwest Atlantic Ocean Rapid transitions of the ocean's deep circulation induced by changes in surface water fluxes Reduced North Atlantic Deep Water flux to the glacial Southern Ocean inferred from neodymium isotope ratios Coupled ocean-atmosphere model response to freshwater input: Comparison to Younger Dryas Event Effects of glacial meltwater in the GISS coupled atmosphereocean model: 1. North Atlantic Deep Water response Inherently unstable climate behaviour due to weak thermohaline ocean circulation Influence of ocean heat transport on the climate of the Last Glacial Maximum Transient simulation of last deglaciation with a new mechanism for Bolling-Allerod warming Routing of meltwater from the Laurentide Ice Sheet during the Younger Dryas cold episode Late Pleistocene Climate in the Central American Lowlands Simulated influence of carbon dioxide, orbital forcing and ice sheets on the climate of the Last Glacial Maximum Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes Deepwater formation in the North Pacific during the Last Glacial Termination Ice sheet sources of sea level rise and freshwater discharge during the last deglaciation Evidence from the high-latitude North Atlantic for variations in Antarctic Intermediate water flow during the last deglaciation Deglacial diatom productivity and surface ocean properties over the Bermuda Rise, northeast Sargasso Sea Eolian sediment responses to late Quaternary climate changes: temporal and spatial patterns in the Sahara The salinity contrast between the Atlantic and Pacific oceans during glacial time Sudden end of an interglacial Reconstructing past planktic foraminiferal habitats using stable isotope data: a case history for Mediterranean sapropel S5 Modeling North American Freshwater Runoff through the Last Glacial Cycle Vertical oceanic nutrient fractionation and glacial/interglacial CO2 cycles Reversed flow of Atlantic deep water during the Last Glacial Maximum Intermediate water links to Deep Western Boundary Current variability in the subtropical NW Atlantic during marine isotope stages 5 and 4 Rapid termination of the African Humid Period triggered by northern high-latitude cooling. Synchronous deglacial overturning and water mass source changes. Atmospheric bridge, oceanic tunnel, and global climatic teleconnections The Younger Dryas Cool Episode in the Gulf of Mexico Water mass exchange between the North Atlantic and the Norwegian Sea during the past 28,000 years

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