1. Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement, CNRS – Aix Marseille Université, 13545 Aix en Provence, France
2. Centre de Recherches Pétrographiques et Géochimiques, CNRS, 54501 Vandoeuvre-lès-Nancy, France
3. Laboratoire de Géodynamique des Chaînes Alpines, CNRS – Université Joseph Fourier, 38400 Grenoble, France
4. Institut de Recherche Pour le Développement, Great Ice, Laboratoire de Glaciologie et Géophysique de l'Environnement, 38402 Grenoble, France
5. Present addresses: Geological and Planetary Science Division, California Institute of Technology, MC 100-23, 1200 E. California Boulevard, Pasadena, California 91125, USA (P.-H.B.); Centre de Recherches Pétrographiques et Géochimiques, CNRS, 54501 Vandoeuvre-lès-Nancy, France (J.L.).

Correspondence to: P.-H. Blard^1,2,5 Correspondence and requests for materials should be addressed to P.-H.B. (Email: blard@gps.caltech.edu or Email: phb26@yahoo.fr).

The magnitude of atmospheric cooling during the Last Glacial Maximum and the timing of the transition into the current interglacial period remain poorly constrained in tropical regions, partly because of a lack of suitable climate records¹. Glacial moraines provide a method of reconstructing past temperatures, but they are relatively rare in the tropics. Here we present a reconstruction of atmospheric temperatures in the central Pacific during the last deglaciation on the basis of cosmogenic ³He ages of moraines and numerical modelling of the ice cap on Mauna Kea volcano, Hawaii—the only highland in the central Pacific on which moraines that formed during the last glacial period are preserved². Our reconstruction indicates that the Last Glacial Maximum occurred between 19,000 and 16,000 years ago in this region and that temperatures at high elevations were about 7 °C lower than today during this interval. Glacial retreat began about 16,000 years ago, but temperatures were still about 6.5 °C lower than today until 15,000 years ago. When combined with estimates of sea surface temperatures in the central Pacific Ocean³, our reconstruction indicates that the lapse rate during the Last Glacial Maximum was higher than at present, which is consistent with the proposal that the atmosphere was drier at that time^{1, 4}. Furthermore, the persistence of full glacial conditions until 15,000 years ago is consistent with the relatively late and abrupt transition to warmer temperatures in Greenland⁵, indicating that there may have been an atmospheric teleconnection between the central Pacific and North Atlantic regions during the last deglaciation.

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