Publication Date:
2013-06-08
Description:
Atmospheric deep convection in the west Pacific plays a key role in the global heat and moisture budgets, yet its response to orbital and abrupt climate change events is poorly resolved. Here, we present four absolutely dated, overlapping stalagmite oxygen isotopic records from northern Borneo that span most of the last glacial cycle. The records suggest that northern Borneo's hydroclimate shifted in phase with precessional forcing but was only weakly affected by glacial-interglacial changes in global climate boundary conditions. Regional convection likely decreased during Heinrich events, but other Northern Hemisphere abrupt climate change events are notably absent. The new records suggest that the deep tropical Pacific hydroclimate variability may have played an important role in shaping the global response to the largest abrupt climate change events.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Carolin, Stacy A -- Cobb, Kim M -- Adkins, Jess F -- Clark, Brian -- Conroy, Jessica L -- Lejau, Syria -- Malang, Jenny -- Tuen, Andrew A -- New York, N.Y. -- Science. 2013 Jun 28;340(6140):1564-6. doi: 10.1126/science.1233797. Epub 2013 Jun 6.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA. stacy.carolin@gatech.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23744779" target="_blank"〉PubMed〈/a〉
Keywords:
Atmosphere
;
Borneo
;
*Climate Change
;
Convection
;
*Ice Cover
;
Oxygen Isotopes/analysis
;
Pacific Ocean
;
*Tropical Climate
Print ISSN:
0036-8075
Electronic ISSN:
1095-9203
Topics:
Biology
,
Chemistry and Pharmacology
,
Computer Science
,
Medicine
,
Natural Sciences in General
,
Physics
