Synchronous change of atmospheric CO2 and Antarctic temperature during the last deglacial warming.
about
On the causal structure between CO2 and global temperatureClimate change decouples oceanic primary and export productivity and organic carbon burialHydrologic impacts of past shifts of Earth's thermal equator offer insight into those to be produced by fossil fuel CO2Siple Dome ice reveals two modes of millennial CO2 change during the last ice age.North Atlantic forcing of tropical Indian Ocean climate.Precise interpolar phasing of abrupt climate change during the last ice age.Design of a Peripheral Building Block for H-Bonded Dendritic Frameworks and Analysis of the Void Space in the Bulk DendrimersThe early rise and late demise of New Zealand's last glacial maximum.The seasonal sea-ice zone in the glacial Southern Ocean as a carbon sinkDeglacial temperature history of West Antarctica.Synchronous deglacial thermocline and deep-water ventilation in the eastern equatorial Pacific.Nonlinear climate sensitivity and its implications for future greenhouse warming.Centennial-scale changes in the global carbon cycle during the last deglaciation.Onset of deglacial warming in West Antarctica driven by local orbital forcing.Responses of ocean circulation and carbon cycle to changes in the position of the Southern Hemisphere westerlies at Last Glacial Maximum.Permafrost thawing as a possible source of abrupt carbon release at the onset of the Bølling/Allerød.Carbon isotope records reveal precise timing of enhanced Southern Ocean upwelling during the last deglaciation.Mean global ocean temperatures during the last glacial transition.Asynchrony between Antarctic temperature and CO2 associated with obliquity over the past 720,000 years.Model evidence for a seasonal bias in Antarctic ice cores.Stratigraphic and Earth System approaches to defining the AnthropoceneSouthern Hemisphere westerlies as a driver of the early deglacial atmospheric CO2 rise.Consequences of twenty-first-century policy for multi-millennial climate and sea-level changeInterglacials of the last 800,000 yearsLaurentide ice-sheet instability during the last deglaciationPushing the boundaries: Glacial/interglacial variability of intermediate and deep waters in the southwest Pacific over the last 350,000 yearsAnthropogenic and natural causes of climate changeEvolution of the monsoon and dry climate in East Asia during late Cenozoic: A reviewMulticentennial Agulhas leakage variability and links to North Atlantic climate during the past 80,000 yearsSouthern Ocean deep convection as a driver of Antarctic warming eventsAtlantic-Pacific seesaw and its role in outgassing CO2during Heinrich eventsSouthwest Atlantic water mass evolution during the last deglaciationEarth’s Climate SystemTiming of the descent into the last Ice Age determined by the bipolar seesawCausal feedbacks in climate change
P2860
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P2860
Synchronous change of atmospheric CO2 and Antarctic temperature during the last deglacial warming.
description
2013 nî lūn-bûn
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2013 թուականի Մարտին հրատարակուած գիտական յօդուած
@hyw
2013 թվականի մարտին հրատարակված գիտական հոդված
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2013年の論文
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2013年論文
@yue
2013年論文
@zh-hant
2013年論文
@zh-hk
2013年論文
@zh-mo
2013年論文
@zh-tw
2013年论文
@wuu
name
Synchronous change of atmosphe ...... ng the last deglacial warming.
@ast
Synchronous change of atmosphe ...... ng the last deglacial warming.
@en
Synchronous change of atmosphe ...... ng the last deglacial warming.
@nl
type
label
Synchronous change of atmosphe ...... ng the last deglacial warming.
@ast
Synchronous change of atmosphe ...... ng the last deglacial warming.
@en
Synchronous change of atmosphe ...... ng the last deglacial warming.
@nl
prefLabel
Synchronous change of atmosphe ...... ng the last deglacial warming.
@ast
Synchronous change of atmosphe ...... ng the last deglacial warming.
@en
Synchronous change of atmosphe ...... ng the last deglacial warming.
@nl
P2093
P2860
P50
P356
P1433
P1476
Synchronous change of atmosphe ...... ng the last deglacial warming.
@en
P2093
P2860
P304
P356
10.1126/SCIENCE.1226368
P407
P577
2013-03-01T00:00:00Z