Disappearance of the last tropical glaciers in the Western Pacific Warm Pool (Papua, Indonesia) appears imminent

• Published in: Proceedings of the National Academy of Sciences
• Main Authors: Permana, Donaldi S., Thompson, Lonnie G., Mosley-Thompson, Ellen, Davis, Mary E., Lin, Ping-Nan, Nicolas, Julien P., Bolzan, John F., Bird, Broxton W., Mikhalenko, Vladimir N., Gabrielli, Paolo, Zagorodnov, Victor, Mountain, Keith R., Schotterer, Ulrich, Hanggoro, Wido, Habibie, Muhammad N., Kaize, Yohanes, Gunawan, Dodo, Setyadi, Gesang, Susanto, Raden D., Fernández, Alfonso, Mark, Bryan G.
• Other Authors: Earth Sciences, School of Science
• Format: Article in Journal/Newspaper
• Language: English
• Published: National Academy of Sciences 2019
• Subjects: glacier retreat; tropical ice cores; Papua Indonesia; climate change; ENSO; Jaya; Pacific; ice core
• Online Access: https://hdl.handle.net/1805/24245

The glaciers near Puncak Jaya in Papua, Indonesia, the highest peak between the Himalayas and the Andes, are the last remaining tropical glaciers in the West Pacific Warm Pool (WPWP). Here, we report the recent, rapid retreat of the glaciers near Puncak Jaya by quantifying the loss of ice coverage and reduction of ice thickness over the last 8 y. Photographs and measurements of a 30-m accumulation stake anchored to bedrock on the summit of one of these glaciers document a rapid pace in the loss of ice cover and a ∼5.4-fold increase in the thinning rate, which was augmented by the strong 2015–2016 El Niño. At the current rate of ice loss, these glaciers will likely disappear within the next decade. To further understand the mechanisms driving the observed retreat of these glaciers, 2 ∼32-m-long ice cores to bedrock recovered in mid-2010 are used to reconstruct the tropical Pacific climate variability over approximately the past half-century on a quasi-interannual timescale. The ice core oxygen isotopic ratios show a significant positive linear trend since 1964 CE (0.018 ± 0.008‰ per year; P < 0.03) and also suggest that the glaciers’ retreat is augmented by El Niño–Southern Oscillation processes, such as convection and warming of the atmosphere and sea surface. These Papua glaciers provide the only tropical records of ice core-derived climate variability for the WPWP.