Deepwater formation in the North Pacific during the Last Glacial Termination.
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Heat Transport Compensation in Atmosphere and Ocean over the Past 22,000 YearsGlobal climate evolution during the last deglaciationPaleoclimate. Synchronization of North Pacific and Greenland climates preceded abrupt deglacial warming.North Pacific deglacial hypoxic events linked to abrupt ocean warming.Abyssal ocean overturning shaped by seafloor distribution.Hydrothermal sediments record changes in deep water oxygen content in the SE PacificSouthern Hemisphere westerlies as a driver of the early deglacial atmospheric CO2 rise.Ice sheet sources of sea level rise and freshwater discharge during the last deglaciationCyclic magnetite dissolution in Pleistocene sediments of the abyssal northwest Pacific Ocean: Evidence for glacial oxygen depletion and carbon trappingThe deglacial transition on the southeastern Alaska Margin: Meltwater input, sea level rise, marine productivity, and sedimentary anoxiaCentennial to millennial climate variability in the far northwestern Pacific (off Kamchatka) and its linkage to the East Asian monsoon and North Atlantic from the Last Glacial Maximum to the early HoloceneDirect ventilation of the North Pacific did not reach the deep ocean during the last deglaciationDeep water formation in the North Pacific and deglacial CO2riseThe Pacific-Atlantic seesaw and the Bering StraitOcean circulation reconstructions fromεNd: A model-based feasibility studyEstimated strength of the Atlantic overturning circulation during the last deglaciationMillennial-scale glacial meltwater pulses and their effect on the spatiotemporal benthicδ18O variabilityPoorly ventilated deep ocean at the Last Glacial Maximum inferred from carbon isotopes: A data-model comparison studyImpact of oceanic circulation changes on atmosphericδ13CO2Toward explaining the Holocene carbon dioxide and carbon isotope records: Results from transient ocean carbon cycle-climate simulationsAtlantic-Pacific seesaw and its role in outgassing CO2during Heinrich eventsCan we use ice sheet reconstructions to constrain meltwater for deglacial simulations?Collapse of the North American ice saddle 14,500 years ago caused widespread cooling and reduced ocean overturning circulationOcean Cooling Pattern at the Last Glacial MaximumGlobal and Arctic climate sensitivity enhanced by changes in North Pacific heat flux
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P2860
Deepwater formation in the North Pacific during the Last Glacial Termination.
description
2010 nî lūn-bûn
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2010年の論文
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2010年学术文章
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2010年学术文章
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2010年学术文章
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2010年学术文章
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2010年学术文章
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2010年學術文章
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2010年學術文章
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name
Deepwater formation in the North Pacific during the Last Glacial Termination.
@en
Deepwater formation in the North Pacific during the Last Glacial Termination.
@nl
type
label
Deepwater formation in the North Pacific during the Last Glacial Termination.
@en
Deepwater formation in the North Pacific during the Last Glacial Termination.
@nl
prefLabel
Deepwater formation in the North Pacific during the Last Glacial Termination.
@en
Deepwater formation in the North Pacific during the Last Glacial Termination.
@nl
P2093
P2860
P50
P356
P1433
P1476
Deepwater formation in the North Pacific during the Last Glacial Termination.
@en
P2093
P2860
P304
P356
10.1126/SCIENCE.1190612
P407
P577
2010-07-01T00:00:00Z