Journal
FOREST ECOLOGY AND MANAGEMENT
Volume 259, Issue 6, Pages 1190-1199Publisher
ELSEVIER
DOI: 10.1016/j.foreco.2010.01.006
Keywords
Eucalyptus regnans; Acacia dealbata; Acacia melanoxylon; Tree water use; Stand structure; Water management; Climate change
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Funding
- Australian Research Council (ARC)
- Department of Sustainability and Environment of Victoria
- Department of Forest and Ecosystem Science of the University of Melbourne
- Alexander v. Humboldt Foundation
- Deutsche Forschungsgemeinschaft (DFG)
- German Academic Exchange Service (DAAD)
- Landesstiftung Baden-Wurttemberg
- Albert-Ludwigs-University of Freiburg
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We examined water use by maturing Eucalyptus regnans, growing with or without an mid-storey stratum of Acacia spp. (Acacia dealbata or A. melanoxylon), for > 180 consecutive days. Study sites were located in the Upper Yarra catchment area in south-eastern Australia. Depending on their contribution to stand basal area, mid-storey Acacia spp. increased total stand water use by up to 30%. Monthly water use in such stands reached more than 640,000 L ha(-1) (compared to 545,000 L ha(-1) in stands where acacias were absent) in early spring. Water use was curvilinearly related to sapwood area of Acacia spp. and logistically related to sapwood area of E. regnans. Water use of all three species showed a strong relation to daily maximum air temperatures. Distinct and simple relationships provide clear guides to the likely impacts of climate change and forest management on water yield. We compared a traditional up-scaling approach, from individual tree water use to stand water use, to a new approach that incorporates variation in temperature. Development of this approach can lead to greater precision of stand water use estimates - and in turn catchment water yield - undercurrent climate change scenarios, which predict a rise in air temperatures of 0.6-2.5 degrees C by 2050 for the study area. Our temperature-dependent approach suggests that under conditions of non-limiting water availability, stand water use will rise by 2% for every 0.25 degrees C increase in maximum air temperatures during winter, and possibly more than that during summer. (C) 2010 Elsevier B.V. All rights reserved.
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