Forward modeling of δ 18 O in Andean ice cores
Author:
Affiliation:
1. Department of Atmospheric and Environmental Sciences State University of New York at Albany Albany New York USA
2. Department of Geosciences University of Massachusetts Amherst Amherst Massachusetts USA
Funder
National Science Foundation
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL070150
Reference55 articles.
1. Millennial-length forward models and pseudoproxies of stalagmite δ<sup>18</sup>O: an example from NW Scotland
2. Influence of convective processes on the isotopic composition (δ18O andδD) of precipitation and water vapor in the tropics: 1. Radiative-convective equilibrium and Tropical Ocean–Global Atmosphere–Coupled Ocean-Atmosphere Response Experiment (TOGA-COARE) simulations
3. Low latitude ice cores record Pacific sea surface temperatures
4. Simulating the temperature and precipitation signal in an Alpine ice core
5. Thinning of the Quelccaya Ice Cap over the last thirty years
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