Role of the North Atlantic circulation in the mid-Pleistocene transition

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: Role of the North Atlantic circulation in the mid-Pleistocene transition ; year:2018 ; pages:1-20
Climate of the past discussions ; (2018), 1-20

Creator: Martin-Garcia, Gloria M.
Sierro, Francisco J.
Flores, José A.
Abrantes, Fátima

DOI: 10.5194/cp-2018-30

URN: urn:nbn:de:101:1-2018061312252520404577

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:32 AM CEST

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Associated

Martin-Garcia, Gloria M.
Sierro, Francisco J.
Flores, José A.
Abrantes, Fátima

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Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2

Diverse manifestations of the mid-Pleistocene climate transition

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Mid to late pleistocene variations of marine productivity in and terrigenous input to the southeast Atlantic

Anomalous mid-twentieth century atmospheric circulation change over the South Atlantic compared to the last 6000 years

Glacial Indonesian Throughflow weakening across the Mid-Pleistocene Climatic Transition

Closure of the Bering Strait caused Mid-Pleistocene Transition cooling

Onset of Mid-Pleistocene glaciation in the Eastern Himalayan syntaxis

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Late Pleistocene climate and circulation history of the western equatorial Pacific

Change in the North Atlantic circulation associated with the mid-Pleistocene transition

Mid-pliocene Atlantic Meridional Overturning Circulation not unlike modern

Atmospheric circulation variability in the North-Atlantic-European area since the mid-seventeenth century

Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2

Diverse manifestations of the mid-Pleistocene climate transition

Hochschulschrift

Mid to late pleistocene variations of marine productivity in and terrigenous input to the southeast Atlantic

Anomalous mid-twentieth century atmospheric circulation change over the South Atlantic compared to the last 6000 years

Glacial Indonesian Throughflow weakening across the Mid-Pleistocene Climatic Transition

Closure of the Bering Strait caused Mid-Pleistocene Transition cooling

Onset of Mid-Pleistocene glaciation in the Eastern Himalayan syntaxis

Hochschulschrift

Late Pleistocene climate and circulation history of the western equatorial Pacific

Change in the North Atlantic circulation associated with the mid-Pleistocene transition

Mid-pliocene Atlantic Meridional Overturning Circulation not unlike modern

Atmospheric circulation variability in the North-Atlantic-European area since the mid-seventeenth century

Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2

Diverse manifestations of the mid-Pleistocene climate transition

Hochschulschrift

Mid to late pleistocene variations of marine productivity in and terrigenous input to the southeast Atlantic

Anomalous mid-twentieth century atmospheric circulation change over the South Atlantic compared to the last 6000 years

Glacial Indonesian Throughflow weakening across the Mid-Pleistocene Climatic Transition

Closure of the Bering Strait caused Mid-Pleistocene Transition cooling

Onset of Mid-Pleistocene glaciation in the Eastern Himalayan syntaxis

Hochschulschrift

Late Pleistocene climate and circulation history of the western equatorial Pacific

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Role of the North Atlantic circulation in the mid-Pleistocene transition

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Other Objects (12)

Change in the North Atlantic circulation associated with the mid-Pleistocene transition

Mid-pliocene Atlantic Meridional Overturning Circulation not unlike modern

Atmospheric circulation variability in the North-Atlantic-European area since the mid-seventeenth century

Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2

Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2

Diverse manifestations of the mid-Pleistocene climate transition

Mid to late pleistocene variations of marine productivity in and terrigenous input to the southeast Atlantic

Anomalous mid-twentieth century atmospheric circulation change over the South Atlantic compared to the last 6000 years

Glacial Indonesian Throughflow weakening across the Mid-Pleistocene Climatic Transition

Closure of the Bering Strait caused Mid-Pleistocene Transition cooling

Onset of Mid-Pleistocene glaciation in the Eastern Himalayan syntaxis

Late Pleistocene climate and circulation history of the western equatorial Pacific

Change in the North Atlantic circulation associated with the mid-Pleistocene transition

Mid-pliocene Atlantic Meridional Overturning Circulation not unlike modern

Atmospheric circulation variability in the North-Atlantic-European area since the mid-seventeenth century

Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2

Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2

Diverse manifestations of the mid-Pleistocene climate transition

Mid to late pleistocene variations of marine productivity in and terrigenous input to the southeast Atlantic

Anomalous mid-twentieth century atmospheric circulation change over the South Atlantic compared to the last 6000 years

Glacial Indonesian Throughflow weakening across the Mid-Pleistocene Climatic Transition

Closure of the Bering Strait caused Mid-Pleistocene Transition cooling

Onset of Mid-Pleistocene glaciation in the Eastern Himalayan syntaxis

Late Pleistocene climate and circulation history of the western equatorial Pacific

Change in the North Atlantic circulation associated with the mid-Pleistocene transition

Mid-pliocene Atlantic Meridional Overturning Circulation not unlike modern

Atmospheric circulation variability in the North-Atlantic-European area since the mid-seventeenth century

Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2

Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2

Diverse manifestations of the mid-Pleistocene climate transition

Mid to late pleistocene variations of marine productivity in and terrigenous input to the southeast Atlantic

Anomalous mid-twentieth century atmospheric circulation change over the South Atlantic compared to the last 6000 years

Glacial Indonesian Throughflow weakening across the Mid-Pleistocene Climatic Transition

Closure of the Bering Strait caused Mid-Pleistocene Transition cooling

Onset of Mid-Pleistocene glaciation in the Eastern Himalayan syntaxis

Late Pleistocene climate and circulation history of the western equatorial Pacific

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