(Q59096847)

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Role of orbitally induced changes in tundra area in the onset of glaciation

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Role of orbitally induced changes in tundra area in the onset of glaciation (English)

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2

J. E. Kutzbach

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R. G. Gallimore

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1

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English

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publication date

June 1996

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Nature

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volume

381

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6582

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page(s)

503-505

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https://scigraph.springernature.com/pub.10.1038/381503a0

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Variations in the Earth's Orbit: Pacemaker of the Ice Ages

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Modeling the climatic response to orbital variations

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On the structure and origin of major glaciation cycles 2. The 100,000-year cycle

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Can Milankovitch orbital variations initiate the growth of ice sheets in a general circulation model?

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The Response of Northern Hemisphere Extratropical Climate and Vegetation to Orbitally Induced Changes in Insolation during the Last Interglaciation

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Effects of boreal forest vegetation on global climate

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Feedbacks between climate and boreal forests during the Holocene epoch

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The Laurentide ice sheet through the last glacial cycle: the topology of drift lineations as a key to the dynamic behaviour of former ice sheets

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Ice age paleotopography

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Oxygen isotopes and sea level

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10.1038/381503A0

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1026395887

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(Q59096847)

Role of orbitally induced changes in tundra area in the onset of glaciation

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