ANSTO Publications Online >
Conference Publications >
Conference Publications >
Please use this identifier to cite or link to this item:
|Title: ||A fine-resolution reconstruction of climatic variability in southeastern Australia over the last 1500 years.|
|Authors: ||Barr, C|
|Issue Date: ||21-Jul-2011|
|Publisher: ||18th INQUA Congress|
|Citation: ||Barr, C., Tibby, J., Gell, P., Jacobsen, G., Zawaszki, A. (2011). A fine-resolution reconstruction of climatic variability in southeastern Australia over the last 1500 years. 18th International Union for Quaternary Research Congress, 21th-27th July 2011, Berne Switzerland.|
|Abstract: ||High-resolution palaeoclimate records extend knowledge of long- and short-term climatic variability beyond the limit of instrumental data. However, to date, no millennial-length, sub-decadal resolution climate records have been produced from mainland Australia. In part, this is due to the absence of suitable archives of proxies amenable to high-resolution analysis.
Here, we present a study of two crater lakes in western Victoria, southeastern Australia. A diatom-conductivity transfer function was developed specifically for application to oligosaline and mesosaline lakes, such as the two study sites; Lake Elingamite and Lake Surprise. A sub-decadal resolution sampling regime was undertaken and results demonstrate that over the past 1500 years, both lakes responded to a common regional-scale climate signal. Reconstructed conductivity, a proxy for moisture balance, indicates distinct periods of contrasting climates. Both lakes record evidence of a severe, and prolonged, dry phase centered around AD 700, which was more extreme than any subsequent drought. Between ca. AD 900 and 1500, the climate was highly variable, with substantial fluctuations in effective moisture. Thereafter, a period of positive moisture balance is evident from ca. AD 1500-1850, with a marked reduction in the amplitude of variability.
Correlations with studies from further afield suggest that ENSO, and possibly the Indian Ocean Dipole, are the key drivers of the observed shifts in moisture balance. These records constitute the first high-resolution evidence of centennial- and decadal-scale climatic variability over the last 1500 years from mainland Australia. This enables a recent major drought to be viewed in an historical context for the first time and provides insight into past climate regimes across southeastern Australia in general, and western Victoria in particular.Copyright (c) 2011 INQUA 18|
|Appears in Collections:||Conference Publications|
Files in This Item:
There are no files associated with this item.
Items in APO are protected by copyright, with all rights reserved, unless otherwise indicated.