Hydrologic impacts of past shifts of Earth's thermal equator offer insight into those to be produced by fossil fuel CO2
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Response of the Pacific inter-tropical convergence zone to global cooling and initiation of Antarctic glaciation across the Eocene Oligocene TransitionAnthropogenic aerosols are a potential cause for migration of the summer monsoon rain belt in ChinaThe intertropical convergence zone modulates intense hurricane strikes on the western North Atlantic marginWarming-induced northwestward migration of the East Asian monsoon rain belt from the Last Glacial Maximum to the mid-HoloceneNorthern Hemisphere hydroclimate variability over the past twelve centuries.Tropical cyclone activity enhanced by Sahara greening and reduced dust emissions during the African Humid Period.Human-induced changes in the distribution of rainfall.Northward extent of East Asian monsoon covaries with intensity on orbital and millennial timescales.South American monsoon response to iceberg discharge in the North Atlantic.
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P2860
Hydrologic impacts of past shifts of Earth's thermal equator offer insight into those to be produced by fossil fuel CO2
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2013 nî lūn-bûn
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2013 թուականի Հոկտեմբերին հրատարակուած գիտական յօդուած
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2013 թվականի հոտեմբերին հրատարակված գիտական հոդված
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2013年の論文
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2013年論文
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2013年論文
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2013年論文
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2013年論文
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2013年論文
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2013年论文
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Hydrologic impacts of past shi ...... be produced by fossil fuel CO2
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Hydrologic impacts of past shi ...... be produced by fossil fuel CO2
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Hydrologic impacts of past shi ...... be produced by fossil fuel CO2
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Hydrologic impacts of past shi ...... be produced by fossil fuel CO2
@ast
Hydrologic impacts of past shi ...... be produced by fossil fuel CO2
@en
Hydrologic impacts of past shi ...... be produced by fossil fuel CO2
@nl
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Hydrologic impacts of past shi ...... be produced by fossil fuel CO2
@ast
Hydrologic impacts of past shi ...... be produced by fossil fuel CO2
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Hydrologic impacts of past shi ...... be produced by fossil fuel CO2
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Hydrologic impacts of past shi ...... be produced by fossil fuel CO2
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Wallace S Broecker
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16710-16715
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10.1073/PNAS.1301855110
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2013-09-27T00:00:00Z