We have constructed two models which can be used together to estimate the isotopic composition of the oceans, given a time series of global temperature and glacial ice volume. In this way - ('climate' as input to the models, isotope 'data' as output) - we can evaluate various interpretations of the actual data in terms of climate changes. -from Authors
CITATION STYLE
Covey, C., & Schneider, S. H. (1984). Models for reconstructing temperature and ice volume from oxygen isotope data. Milankovitch and Climate. Proc. NATO Workshop, Palisades, 1982. Vol. 2, 699–705. https://doi.org/10.1007/978-94-017-4841-4_15
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