• journal_title：Geology
• Contributor：Michael R. Kaplan ; Joerg M. Schaefer ; George H. Denton ; Alice M. Doughty ; David J.A. Barrell ; Trevor J.H. Chinn ; Aaron E. Putnam ; Bjørn G. Andersen ; Andrew Mackintosh ; Robert C. Finkel ; Roseanne Schwartz ; Brian Anderson
• Publisher：Geological Society of America
• Date：2013-08-01
• Format：text/html
• Language：en
• Identifier：10.1130/G34288.1
• journal_abbrev：Geology
• issn：0091-7613
• volume：41
• issue：8
• firstpage：887
• section：Articles

The timing and magnitude of postglacial climatic changes around the globe provide insights into the underlying drivers of natural climate change. Using geomorphologic mapping of moraines, ¹⁰Be surface-exposure dating, snowline reconstructions, and numerical modeling, we quantified glacier behavior during Late Glacial (15–11.5 ka) and Holocene (the past ∼11.5 k.y.) time in the Ben Ohau Range, New Zealand. Glaciers were more extensive during the Antarctic Cold Reversal (ACR), than subsequently, and the margins underwent a punctuated net withdrawal over the Holocene. Numerical modeling experiments that achieve the best fit to the moraines suggest that air temperature during the ACR was between 1.8 °C and 2.6 °C cooler than today, with similar (±20%) prescribed precipitation. After the ACR, a net snowline rise of ∼100 m through the Younger Dryas stadial (12.9–11.7 ka) was succeeded by a further “long-term,” or net, rise of ∼100 m between ∼11 k.y. and ∼500 yr ago. Glacier snowline records in New Zealand show generally coherent Late Glacial and Holocene climate trends. However, the paleoclimate record in the southwest Pacific region shows important differences from that in the Northern Hemisphere.