155,000 years of West African monsoon and ocean thermal evolution. - Wikidata - wikimedia - TriplyDB

155,000 years of West African monsoon and ocean thermal evolution.

155,000 years of West African monsoon and ocean thermal evolution.

http://www.wikidata.org/entity/Q34633230

about

Atlantic forcing of persistent drought in West Africa The Expansion of mtDNA Haplogroup L3 within and out of Africa African humid periods triggered the reactivation of a large river system in Western Sahara 60,000 years of interactions between Central and Eastern Africa documented by major African mitochondrial haplogroup L2 West African monsoon dynamics inferred from abrupt fluctuations of Lake Mega-Chad Development of Middle Stone Age innovation linked to rapid climate change Dynamics of green Sahara periods and their role in hominin evolution Global climate evolution during the last deglaciation Wet phases in the Sahara/Sahel region and human migration patterns in North Africa Khoisan hunter-gatherers have been the largest population throughout most of modern-human demographic history Impact of abrupt deglacial climate change on tropical Atlantic subsurface temperatures.Abrupt shifts in Horn of Africa hydroclimate since the Last Glacial Maximum.The Asian monsoon over the past 640,000 years and ice age terminations.Glacial to Holocene changes in trans-Atlantic Saharan dust transport and dust-climate feedbacks.Link between light-triggered Mg-banding and chamber formation in the planktic foraminifera Neogloboquadrina dutertrei.Greening of the Sahara suppressed ENSO activity during the mid-Holocene.Regional and global sea-surface temperatures during the last interglaciation.Intensity of African Humid Periods Estimated from Saharan Dust Fluxes Eastern South African hydroclimate over the past 270,000 years.A global multiproxy database for temperature reconstructions of the Common Era Nonlinear climate sensitivity and its implications for future greenhouse warming.Coherent changes of southeastern equatorial and northern African rainfall during the last deglaciation.Late Pleistocene climate drivers of early human migration.Catastrophic drought in the Afro-Asian monsoon region during Heinrich event 1.Deglacial Tropical Atlantic subsurface warming links ocean circulation variability to the West African Monsoon.Rapid termination of the African Humid Period triggered by northern high-latitude cooling.150,000-year palaeoclimate record from northern Ethiopia supports early, multiple dispersals of modern humans from Africa.Pollen from the Deep-Sea: A Breakthrough in the Mystery of the Ice Ages.Relative impacts of insolation changes, meltwater fluxes and ice sheets on African and Asian monsoons during the Holocene Coherent high- and low-latitude control of the northwest African hydrological balance Non-linear intensification of Sahel rainfall as a possible dynamic response to future warming Extreme events as drivers of early human behaviour in Africa? The case for variability, not catastrophic drought Drivers of ecosystem and climate change in tropical West Africa over the past ∼540 000 years Ba incorporation in benthic foraminifera A 30,000 yr Record of land-ocean interaction in the eastern gulf of Guinea Mechanisms rectifying the annual mean response of tropical Atlantic rainfall to precessional forcing Strong middepth warming and weak radiocarbon imprints in the equatorial Atlantic during Heinrich 1 and Younger Dryas LA-ICP-MS depth profiling perspective on cleaning protocols for elemental analyses in planktic foraminifers Timing of the descent into the last Ice Age determined by the bipolar seesaw The effect of Congo River freshwater discharge on Eastern Equatorial Atlantic climate variability

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155,000 years of West African monsoon and ocean thermal evolution.

http://www.wikidata.org/entity/Q34633230

description

2007 nî lūn-bûn

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2007 թուականի Յունիսին հրատարակուած գիտական յօդուած

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2007 թվականի հունիսին հրատարակված գիտական հոդված

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2007年の論文

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2007年学术文章

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2007年学术文章

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2007年学术文章

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2007年学术文章

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2007年学术文章

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2007年學術文章

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name

155,000 years of West African monsoon and ocean thermal evolution.

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155,000 years of West African monsoon and ocean thermal evolution.

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155,000 years of West African monsoon and ocean thermal evolution.

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155,000 years of West African monsoon and ocean thermal evolution.

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155,000 years of West African monsoon and ocean thermal evolution.

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155,000 years of West African monsoon and ocean thermal evolution.

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155,000 years of West African monsoon and ocean thermal evolution.

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155,000 years of West African monsoon and ocean thermal evolution.

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155,000 years of West African monsoon and ocean thermal evolution.

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SCIENCE.1140461

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155,000 years of West African monsoon and ocean thermal evolution.

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P2093

David W Lea

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Nils Andersen

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Syee Weldeab

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P2860

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

A high-resolution absolute-dated late Pleistocene Monsoon record from Hulu Cave, China.

Synchroneity of tropical and high-latitude Atlantic temperatures over the last glacial termination.

Indian Ocean climate and an absolute chronology over Dansgaard/Oeschger events 9 to 13.

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

Climate impact of late quaternary equatorial pacific sea surface temperature variations

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

Super ENSO and global climate oscillations at millennial time scales.

Timing, duration, and transitions of the last interglacial Asian monsoon.

Coherent high- and low-latitude climate variability during the holocene warm period

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1303-1307

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scholarly article

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10.1126/SCIENCE.1140461

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316

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Ralph Schneider

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2007-06-01T00:00:00Z

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6295244

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17540896

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