Transient simulation of last deglaciation with a new mechanism for Bolling-Allerod warming.
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Hot topics in biodiversity and climate change researchArctic climate tipping pointsPredicting and mitigating future biodiversity loss using long-term ecological proxiesDownscaled and debiased climate simulations for North America from 21,000 years ago to 2100ADValidation of climate model-inferred regional temperature change for late-glacial EuropeFennoscandian freshwater control on Greenland hydroclimate shifts at the onset of the Younger DryasHeat Transport Compensation in Atmosphere and Ocean over the Past 22,000 YearsRegional paleofire regimes affected by non-uniform climate, vegetation and human driversClimate change on the Tibetan Plateau in response to shifting atmospheric circulation since the LGMSpace can substitute for time in predicting climate-change effects on biodiversityGlobal climate evolution during the last deglaciationIce-shelf collapse from subsurface warming as a trigger for Heinrich eventsImpact of abrupt deglacial climate change on tropical Atlantic subsurface temperatures.Palaeoceanography: motivations and challenges for the future.Model systems for a no-analog future: species associations and climates during the last deglaciation.Abrupt glacial climate shifts controlled by ice sheet changes.Greenland temperature response to climate forcing during the last deglaciation.Ocean surface temperature variability: large model-data differences at decadal and longer periods.Evolution and forcing mechanisms of El Niño over the past 21,000 years.Icebergs not the trigger for North Atlantic cold events.Linking environmental filtering and disequilibrium to biogeography with a community climate framework.Past and future evolution of Abies alba forests in Europe - comparison of a dynamic vegetation model with palaeo data and observations.Gradual onset and recovery of the Younger Dryas abrupt climate event in the tropics.Abrupt Bølling warming and ice saddle collapse contributions to the Meltwater Pulse 1a rapid sea level rise.Rainfall regimes of the Green Sahara.Holocene peatland and ice-core data constraints on the timing and magnitude of CO2 emissions from past land use.The last glacial termination.Climate change. What drives climate flip-flops?Coupling of equatorial Atlantic surface stratification to glacial shifts in the tropical rainbelt.Reconstruction of the South Atlantic Subtropical Dipole index for the past 12,000 years from surface temperature proxyPleistocene range dynamics and episodic rarity in an extinct bird.The Holocene temperature conundrum.Regional and global sea-surface temperatures during the last interglaciation.Role of the Bering Strait on the hysteresis of the ocean conveyor belt circulation and glacial climate stability.Regional and global forcing of glacier retreat during the last deglaciation.Younger Dryas cooling and the Greenland climate response to CO2.Centennial-scale Holocene climate variations amplified by Antarctic Ice Sheet discharge.Correlation and anti-correlation of the East Asian summer and winter monsoons during the last 21,000 years.Equatorial Pacific forcing of western Amazonian precipitation during Heinrich Stadial 1.Timing and nature of AMOC recovery across Termination 2 and magnitude of deglacial CO2 change.
P2860
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P2860
Transient simulation of last deglaciation with a new mechanism for Bolling-Allerod warming.
description
2009 nî lūn-bûn
@nan
2009年の論文
@ja
2009年論文
@yue
2009年論文
@zh-hant
2009年論文
@zh-hk
2009年論文
@zh-mo
2009年論文
@zh-tw
2009年论文
@wuu
2009年论文
@zh
2009年论文
@zh-cn
name
Transient simulation of last d ...... m for Bolling-Allerod warming.
@en
type
label
Transient simulation of last d ...... m for Bolling-Allerod warming.
@en
prefLabel
Transient simulation of last d ...... m for Bolling-Allerod warming.
@en
P2093
P2860
P356
P1433
P1476
Transient simulation of last d ...... m for Bolling-Allerod warming.
@en
P2093
A E Carlson
B L Otto-Bliesner
D Erickson
J Kutzbach
J Lynch-Stieglitz
P2860
P304
P356
10.1126/SCIENCE.1171041
P407
P577
2009-07-01T00:00:00Z