title: Varied response of western Pacific hydrology to climate forcings over the last glacial period.
abstract: 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.
authors.affiliation: School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA. stacy.carolin@gatech.edu
authors.forename: Stacy A
authors.initials: SA
authors.lastname: Carolin
authors.forename: Kim M
authors.initials: KM
authors.lastname: Cobb
authors.forename: Jess F
authors.initials: JF
authors.lastname: Adkins
authors.forename: Brian
authors.initials: B
authors.lastname: Clark
authors.forename: Jessica L
authors.initials: JL
authors.lastname: Conroy
authors.forename: Syria
authors.initials: S
authors.lastname: Lejau
authors.forename: Jenny
authors.initials: J
authors.lastname: Malang
authors.forename: Andrew A
authors.initials: AA
authors.lastname: Tuen
mesh_terms: D001272:Atmosphere; D001893:Borneo; D057231:Climate Change; D018481:Convection; D046448:Ice Cover; D010103:Oxygen Isotopes / Q000032:analysis; D010140:Pacific Ocean; D014329:Tropical Climate
chemical_list: D010103:Oxygen Isotopes