Local summer insolation and greenhouse gas forcing drove warming and glacier retreat in New Zealand during the Holocene
Geological climate archives from the Holocene Epoch provide baseline information concerning natural climate variability. Temperate mountain glacier extent is sensitive to summer air temperature, thus geological records of past glacier length changes are a useful proxy for this climatic variable. Here we present a new cosmogenic 10Be chronology of glacier length changes at Dart Glacier in the Southern Alps, New Zealand. Prominent moraines deposited 321 ± 44 yr ago (n = 11) and 7.8 ± 0.3 ka (n =...[Show more]
|Collections||ANU Research Publications|
|Source:||Quaternary Science Reviews|
|1-s2.0-S0277379121002754-main.pdf||7.05 MB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.