Calibrating climate-δ18O regression models for the interpretation of high-resolution speleothem δ18O time series
Providing estimates of past climate changes on interannual–millenial timescales requires suitable regression models between climate and climate proxies. Many proxies appear to show relationships with climate that are timescale dependent. Any proxy‐climate model should be able to replicate the major...
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Veröffentlicht in: | Journal of Geophysical Research: Atmospheres 2008-09, Vol.113 (D17), p.n/a |
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Sprache: | eng |
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