Abstract
The magnitude of tropical cooling during the Last Glacial Maximum (LGM) has been the subject of uncertainty for over 25 years. We use principles of meta-analysis as an objective approach to reconcile estimates from different proxies. This approach treats each observation as a random estimate of the true mean and weights estimates by their reported precision. We assigned global uncertainties to proxies and derived a new regional standard deviation for temperatures calculated from the Sr/Ca ratio in tropical corals (σ = 1.4°C). Using a Bayesian spatial interpolation scheme, we estimate a mean cooling of LGM tropical sea surface temperatures of -2.7 ± 0.5°C (±σ) and surface air temperatures of -5.4 ± 0.3°C (±σ).
| Original language | English |
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| Pages (from-to) | 1-4 |
| Number of pages | 4 |
| Journal | Geophysical Research Letters |
| Volume | 32 |
| Issue number | 5 |
| DOIs | |
| State | Published - Mar 16 2005 |