{"refrec":{"BRefID":241865,"RR":"<b>Goodwin, I.D.; Browning, S.A.; Anderson, A.J.</b> (2014). Climate windows for Polynesian voyaging to New Zealand and Easter Island. <i>Proc. Natl. Acad. Sci. U.S.A. 11(41)</i>: 14716-14721. <a href=\"https://dx.doi.org/10.1073/pnas.1408918111\" target=\"_blank\">https://dx.doi.org/10.1073/pnas.1408918111</a>","BEntID":233564,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Proc. Natl. Acad. Sci. U.S.A. 11(41)</i>: 14716-14721. <a href=\"https://dx.doi.org/10.1073/pnas.1408918111\" target=\"_blank\">https://dx.doi.org/10.1073/pnas.1408918111</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Goodwin, I.D.; Browning, S.A.; Anderson, A.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Goodwin, I.D. <i>et al.</i>","Englishabstract":"South Pacific migration routes used in East Polynesian colonization (A.D. 800-1500) have been assumed to be commonly upwind, when based on an understanding of modern climate patterns. Instead, our novel paleowind field reconstructions at bidecadal resolution show that migration routes lay downwind from East Polynesia during known times of initial colonization of New Zealand and Easter Island. 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