Global atmospheric teleconnections during Dansgaard–Oeschger events

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Rapid global ocean-atmosphere response to Southern Ocean freshening during the last glacial.Abrupt transitions in time series with uncertainties.Improved methodologies for continuous-flow analysis of stable water isotopes in ice cores

P2860

Q41196934-63AB3CBE-00BC-495C-A6A4-306742443CBC Q48314155-7FE4BD4F-D579-407D-A50D-9F1C3EE4614F Q57885106-FE76FB10-1FC0-4949-AEEB-C8A646F3F79F

P2860

Global atmospheric teleconnections during Dansgaard–Oeschger events

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http://www.wikidata.org/entity/Q58114246

description

im Dezember 2016 veröffentlichter wissenschaftlicher Artikel

@de

wetenschappelijk artikel

@nl

наукова стаття, опублікована в грудні 2016

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name

Global atmospheric teleconnections during Dansgaard–Oeschger events

@en

Global atmospheric teleconnections during Dansgaard–Oeschger events

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type

Item

label

Global atmospheric teleconnections during Dansgaard–Oeschger events

@en

Global atmospheric teleconnections during Dansgaard–Oeschger events

@nl

prefLabel

Global atmospheric teleconnections during Dansgaard–Oeschger events

@en

Global atmospheric teleconnections during Dansgaard–Oeschger events

@nl

P1476

Global atmospheric teleconnections during Dansgaard–Oeschger events

@en

P2093

Bradley R. Markle

http://www.w3.org/2001/XMLSchema#string

Cecilia M. Bitz

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James W. C. White

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Joel B. Pedro

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Qinghua Ding

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Spruce W. Schoenemann

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T. J. Fudge

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Todd Sowers

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Tyler R. Jones

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P2860

An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka

Precise interpolar phasing of abrupt climate change during the last ice age.

GRIP deuterium excess reveals rapid and orbital-scale changes in Greenland moisture origin.

High-resolution Greenland ice core data show abrupt climate change happens in few years.

Wet periods in northeastern Brazil over the past 210 kyr linked to distant climate anomalies.

High-resolution record of Northern Hemisphere climate extending into the last interglacial period

A new greenland deep ice core.

Onset of deglacial warming in West Antarctica driven by local orbital forcing.

Rapid changes in the hydrologic cycle of the tropical Atlantic during the last glacial.

Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2.

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ngeo2848

P304

36-40

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P31

scholarly article

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10.1038/NGEO2848

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P407

English

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http://www.w3.org/2001/XMLSchema#string

P478

http://www.w3.org/2001/XMLSchema#string

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E. J. Steig

Christo Buizert

P577

2016-12-12T00:00:00Z

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Global atmospheric teleconnections during Dansgaard–Oeschger events

about

P2860

P2860

Global atmospheric teleconnections during Dansgaard–Oeschger events

description

name

type

label

prefLabel

P1433

P1476

P2093

P2860

P2888

P304

P31

P356

P407

P433

P478

P50

P577

P356

P1433

P1476

P2093

P2860

P2888

P304

P31

P356

P407

P433

P478

P50

P577