Northern Hemisphere forcing of climatic cycles in Antarctica over the past 360,000 years
The Milankovitch theory of climate change proposes that glacial interglacial cycles are driven by changes in summer insolation at high northern latitudes(1). The timing of climate change in the Southern Hemisphere at glacial-interglacial transitions (which are known as terminations) relative to vari...
Main Authors: | , , , , , , , , , , , , , , , , , |
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Format: | Text |
Language: | English |
Published: |
2007
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Subjects: | |
Online Access: | https://www.documentation.ird.fr/hor/fdi:010040778 |