A corrected radiocarbon age of 11,050 +/- 14 years before present for
an advance of the Franz Josef Glacier to the Waiho Loop terminal morai
ne on the western flank of New Zealand's Southern Alps shows that glac
ier advance on a South Pacific island was synchronous with initiation
of the Younger Dryas in the North Atlantic region. Hence, cooling at t
he beginning of the Younger Dryas probably reflects global rather than
regional forcing. The source for Younger Dryas climatic cooling may t
hus lie in the atmosphere rather than in a North Atlantic thermohaline
switch.