Greenland temperature response to climate forcing during the last deglaciation. - Wikidata - wikimedia - TriplyDB

Greenland temperature response to climate forcing during the last deglaciation.

Greenland temperature response to climate forcing during the last deglaciation.

http://www.wikidata.org/entity/Q30847691

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Climate. Greenland deglaciation puzzles.Precise interpolar phasing of abrupt climate change during the last ice age.Abrupt Bølling warming and ice saddle collapse contributions to the Meltwater Pulse 1a rapid sea level rise.Volcanic influence on centennial to millennial Holocene Greenland temperature change Human-induced changes in the distribution of rainfall.Deglacial temperature history of West Antarctica.Rapid measurement of perchlorate in polar ice cores down to sub-ng L(-1) levels without pre-concentration.Synchronous centennial abrupt events in the ocean and atmosphere during the last deglaciation.Asynchronous warming and δ18O evolution of deep Atlantic water masses during the last deglaciation.First identification and characterization of Borrobol-type tephra in the Greenland ice cores: new deposits and improved age estimates.Warm summers during the Younger Dryas cold reversal.Instability of the Northeast Greenland Ice Stream over the last 45,000 years.Southern Hemisphere westerlies as a driver of the early deglacial atmospheric CO2 rise.Interglacials of the last 800,000 years Vegetation dynamics during last 35,000 years at a cold desert locale: preferential loss of forbs with increased aridity The spatial extent and dynamics of the Antarctic Cold Reversal Spatial and temporal oxygen isotope variability in northern Greenland – implications for a new climate record over the past millennium Revision of the EPICA Dome C CO2 record from 800 to 600 kyr before present Destabilization of glacial climate by the radiative impact of Atlantic Meridional Overturning Circulation disruptions Collapse of the North American ice saddle 14,500 years ago caused widespread cooling and reduced ocean overturning circulation A 5500-year oxygen isotope record of high arctic environmental change from southern Spitsbergen Global and Arctic climate sensitivity enhanced by changes in North Pacific heat flux

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Greenland temperature response to climate forcing during the last deglaciation.

http://www.wikidata.org/entity/Q30847691

description

2014 nî lūn-bûn

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2014 թուականի Սեպտեմբերին հրատարակուած գիտական յօդուած

@hyw

2014 թվականի սեպտեմբերին հրատարակված գիտական հոդված

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2014年の論文

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2014年論文

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2014年論文

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2014年論文

@zh-hk

2014年論文

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2014年論文

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2014年论文

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name

Greenland temperature response to climate forcing during the last deglaciation.

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Greenland temperature response to climate forcing during the last deglaciation.

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type

label

Greenland temperature response to climate forcing during the last deglaciation.

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Greenland temperature response to climate forcing during the last deglaciation.

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Greenland temperature response to climate forcing during the last deglaciation.

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Greenland temperature response to climate forcing during the last deglaciation.

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SCIENCE.1254961

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Greenland temperature response to climate forcing during the last deglaciation.

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P2093

Anders E Carlson

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

Benoit S Lecavalier

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

Edward J Brook

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

James W C White

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

Philippe Kindler

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

Zhengyu Liu

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

P2860

Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core

Making sense of palaeoclimate sensitivity

Global climate evolution during the last deglaciation

Large Arctic Temperature Change at the Wisconsin-Holocene Glacial Transition

GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACE

Sea ice as the glacial cycles’ Climate switch: role of seasonal and orbital forcing

Abrupt climate change at the end of the last glacial period inferred from trapped air in polar Ice

The role of the thermohaline circulation in abrupt climate change.

Southern Ocean origin for the resumption of Atlantic thermohaline circulation during deglaciation.

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

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1177-1180

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scholarly article

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10.1126/SCIENCE.1254961

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6201

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P478

345

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Valérie Masson-Delmotte

Markus Leuenberger

Bo Møllesøe Vinther

Vasileios Gkinis

Jeffrey P Severinghaus

Bette Otto-Bliesner

Christo Buizert

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2014-09-01T00:00:00Z

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265375912

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25190795

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