Coupling of the Intertropical Convergence Zone and Southern Hemisphere mid-latitude climate during the early to mid-Holocene
dc.contributor.author | Mariani, M | en_AU |
dc.contributor.author | Fletcher, MS | en_AU |
dc.contributor.author | Drysdale, RN | en_AU |
dc.contributor.author | Saunders, KM | en_AU |
dc.contributor.author | Heijnis, H | en_AU |
dc.contributor.author | Jacobsen, GE | en_AU |
dc.contributor.author | Zawadzki, A | en_AU |
dc.date.accessioned | 2025-02-05T23:59:35Z | en_AU |
dc.date.available | 2025-02-05T23:59:35Z | en_AU |
dc.date.issued | 2017-10-27 | en_AU |
dc.date.statistics | 2025-02-06 | en_AU |
dc.description.abstract | Conceptual models predict a tight coupling between the Intertropical Convergence Zone (ITCZ) and the Southern Westerly Winds (SWW) in response to glacial-interglacial transitions, yet little is known about this relationship under Holocene boundary conditions. Here we present a synthesis of Holocene pollen data from the southwest Pacific mid-latitudes that tracks changes in the SWW. Comparison of our SWW paleoclimate records with data tracking the ITCZ, oceanic circulation, and insolation reveals clearly synchronous and in-phase ITCZ-SWW dynamics between 12 and 5 ka, indicating a tight coupling between the tropics and southern mid-latitudes in response to ocean circulation and insolation. An apparent decoupling of the SWW and ITCZ in the Pacific region after 5 ka is attributable to the overriding influence of the El Niño-Southern Oscillation (ENSO) over the proxy data. © 2017 Geological Society of America | en_AU |
dc.identifier.citation | Mariani, M., Fletcher, M.-S., Drysdale, R. N., Saunders, K. M., Heijnis, H., Jacobsen, G., & Zawadzki, A. (2017). Coupling of the Intertropical Convergence Zone and Southern Hemisphere mid-latitude climate during the early to mid-Holocene. Geology, 45(12), 1083-1086. doi:10.1130/g39705.1 | en_AU |
dc.identifier.issn | 0091-7613 | en_AU |
dc.identifier.issn | 1943-2682 | en_AU |
dc.identifier.issue | 12 | en_AU |
dc.identifier.journaltitle | Geology | en_AU |
dc.identifier.pagination | 1083-1086 | en_AU |
dc.identifier.uri | https://doi.org/10.1130/g39705.1 | en_AU |
dc.identifier.uri | https://apo.ansto.gov.au/handle/10238/15965 | en_AU |
dc.identifier.volume | 45 | en_AU |
dc.language | English | en_AU |
dc.language.iso | en | en_AU |
dc.publisher | Geological Society of America | en_AU |
dc.subject | Pollen | en_AU |
dc.subject | Precipitation | en_AU |
dc.subject | Tasmania | en_AU |
dc.subject | Australia | en_AU |
dc.subject | Sediments | en_AU |
dc.subject | Southern Oscillation | en_AU |
dc.subject | Climatic change | en_AU |
dc.subject | Carbon | en_AU |
dc.subject | Drill cores | en_AU |
dc.subject | Fires | en_AU |
dc.subject | Charcoal | en_AU |
dc.subject | Quaternary Period | en_AU |
dc.subject | Tropical Regions | en_AU |
dc.subject | Southern Hemisphere | en_AU |
dc.subject | Pacific Ocean | en_AU |
dc.subject | Glaciers | en_AU |
dc.subject | Isotopes | en_AU |
dc.subject | Wind | en_AU |
dc.subject | Plants | en_AU |
dc.title | Coupling of the Intertropical Convergence Zone and Southern Hemisphere mid-latitude climate during the early to mid-Holocene | en_AU |
dc.type | Journal Article | en_AU |