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A 277 year cool season dam inflow reconstruction for Tasmania, southeastern Australia
Citation
Allen, KJ and Nichols, SC and Evans, R and Allie, S and Carson, G and Ling, F and Cook, ER and Lee, G and Baker, PJ, A 277 year cool season dam inflow reconstruction for Tasmania, southeastern Australia, Water Resources Research, 53, (1) pp. 400-414. ISSN 0043-1397 (2017) [Refereed Article]
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Copyright Statement
Copyright 2016 American Geophysical Union
Abstract
Seasonal variability is a significant source of uncertainty in projected changes to precipitation across southeastern Australia (SEA). While existing instrumental records provide seasonal data for recent decades, most proxy records (e.g., tree rings, corals, speleothems) offer only annual reconstructions of hydroclimate. We present the first cool-season (July–August) reconstruction of dam inflow (Lake Burbury) for western Tasmania in SEA based on tree-ring width (Athrotaxis selaginoides) and mean latewood cell wall thickness (Phyllocladus aspleniifolius) chronologies. The reconstruction, produced using principal component regression, verifies back to 1731 and is moderately skillful, explaining around 23% of the variance. According to the reconstruction, relatively low inflow periods occurred around 1860, the early 1900s and 1970, while relatively high inflows occurred in the 1770s and 1810s. Highest reconstructed inflows occurred in 1816, and lowest in 1909. Comparison with available documentary and instrumental records indicates that the reconstruction better captures high rather than low flow events. There is virtually no correlation between our reconstruction and another for December–January inflow for the same catchment, a result consistent with the relationship between seasonal instrumental data. This suggests that conditions in one season have not generally reflected conditions in the other season over the instrumental record, or for the past 277 years. This illustrates the value of obtaining reconstructions of regional hydroclimatic variability for multiple individual seasons in regions where dry and wet seasons are not strongly defined. The results also indicate that the hydroclimate of the southeastern Australian region cannot be adequately represented by a single regional reconstruction.
Item Details
Item Type: | Refereed Article |
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Keywords: | Tasmania, seasonal variability, precipitation |
Research Division: | Earth Sciences |
Research Group: | Climate change science |
Research Field: | Climatology |
Objective Division: | Expanding Knowledge |
Objective Group: | Expanding knowledge |
Objective Field: | Expanding knowledge in the environmental sciences |
UTAS Author: | Lee, G (Dr Greg Lee) |
ID Code: | 123498 |
Year Published: | 2017 |
Web of Science® Times Cited: | 11 |
Deposited By: | CRC-Antarctic Climate & Ecosystems |
Deposited On: | 2018-01-10 |
Last Modified: | 2018-04-23 |
Downloads: | 61 View Download Statistics |
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