Huascaran δ18Oas an indicator of tropical climate during the Last Glacial Maximum

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Huascaran δO as an indicator of tropical climate during the Last Glacial Maximum

The interpretation of the isotopic composition of Andes tropical mountain glaciers is reconsidered using a simple Rayleigh distillation model. It is shown that Andes snowline depression and Huascaran ice core δO are consistent with a 3C drop in sea surface temperature during the Last Glacial Maximum, accompanied by an increase from 40% at present to 60% during the LGM in the annual mean proport...

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Quantifying the Effects of Lower Sea Level on Tropical Pacific Climate during the Last Glacial Maximum

ACKNOWLEDGEMENTS First and foremost, I wish to thank my research advisor and co-advisor, Dr. Kim Cobb and Dr. Emanuele DiLorenzo. They have put a tremendous number of hours into this project while teaching me that conducting research is challenging, tiring, but more importantly, fun and inspiring. I also wish to thank Dr. Yen, both who introduced me to the world of academia. Working in both of ...

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The Last Glacial Maximum.

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ژورنال

عنوان ژورنال: Geophysical Research Letters

سال: 1999

ISSN: 0094-8276

DOI: 10.1029/1999gl900183