Spatio-temporal transpiration patterns reflect vegetation structure in complex upland terrain

Daniel Metzen, Gary J. Sheridan, Richard G. Benyon, Paul V. Bolstad, Anne Griebel, Patrick N.J. Lane

Research output: Contribution to journalArticlepeer-review

7 Scopus citations

Abstract

Topography exerts control on eco-hydrologic processes via alteration of energy inputs due to slope angle and orientation. Further, water availability varies with drainage position in response to topographic water redistribution and the catena effect on soil depth and thus soil water storage capacity. Our understanding of the spatio-temporal dynamics and drivers of transpiration patterns in complex terrain is still limited by lacking knowledge of how systematic interactions of energy and moisture patterns shape ecosystem state and water fluxes and adaptation of the vegetation to these patterns. To untangle the effects of slope orientation and hillslope position on forest structure and transpiration patterns, we measured forest structure, sap flux, soil moisture, throughfall and incoming shortwave radiation along two downslope transects in a forested head water catchment in south-east Australia. Our plot locations controlled for three systematically varying drainage position levels (topographic wetness index: 5.0, 6.5 and 8.0) and two levels of energy input (aridity index: 1.2 and 1.8). Vegetation patterns were generally stronger related to drainage position than slope orientation, whereas sap velocity variations were less pronounced. However, in combination with stand sapwood area, consistent spatio-temporal transpiration patterns emerged in relation to landscape position, where slope orientation was the primary and drainage position the secondary controlling factor. On short temporal scales, radiation and vapor pressure deficit were most important in regulating transpiration rates, whereas soil water limitation only occurred on shallow soils during summer. The importance of stand structural parameters increased on longer time scales, indicating optimization of vegetation in response to the long-term hydro-climatic conditions at a given landscape position. Thus, vegetation patterns can be conceptualized as a ‘time-integrated’ predictor variable that captures large fractions of other factors contributing to transpiration patterns.

Original languageEnglish (US)
Article number133551
JournalScience of the Total Environment
Volume694
DOIs
StatePublished - Dec 1 2019

Bibliographical note

Funding Information:
The study was supported by the integrated Forest Ecosystem Research program, which is funded by the Victorian Department of Environment, Land, Water and Planning and by the Melbourne International Research Scholarship and Melbourne International Fee Remission of The University of Melbourne . We thank Philip Noske for assistance with installing and maintaining the field site, Petter Nyman for providing the aridity index rasters, Tom Fairman for helping with species identification and two anonymous reviewers for their suggestions which improved an earlier version of the manuscript.

Publisher Copyright:
© 2019

Keywords

  • Aridity index
  • Eucalyptus
  • Forest structure
  • Sap flow
  • Topography

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