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- W1481592011 abstract "Orbital forcing of Pleistocene climate has been firmly established since the development of the benthic δO record, a proxy for glacial ice volume, three decades ago. However, our understanding of ice age cycles and the involving feedback remains limited. Prediction based on Milankovitch theory that both ~21kyr and ~41kyr cycles exist in the ice volume record failed to explain Pleistocene benthic δO record which is dominated by ~41kyr periodicity before 0.8 Ma. This failure of Milankovitch theory has inspired new hypotheses to account for the unexplained features of the ice volume record. The variety of these hypotheses indicates the complication of the climate-orbital linkage: instead of simple radiative forcing of high latitudes, internal climate feedbacks might play an important role in the cause of ice age cycles. However, these hypotheses are largely untested to date. Marine proxy records demonstrate tropical climate oscillations in accordance with high-latitude climate changes. Based on these records, tropical region has been recognized as a possible amplifier of the obliquity insolation change. Nevertheless, the pathways through which the high-latitude climate influenced tropical climate condition are not understood." @default.
- W1481592011 created "2016-06-24" @default.
- W1481592011 creator A5019370820 @default.
- W1481592011 date "2008-01-01" @default.
- W1481592011 modified "2023-09-23" @default.
- W1481592011 title "Orbital control and climate feedbacks on ice age cycles during Plio-Pleistocene" @default.
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