Ideas and perspectives: Tree–atmosphere interaction responds to water-related stem variations

Journal Article (2018)
Author(s)

T.H.M. Van Emmerik (TU Delft - Water Resources)

Susan Steele-Dunne (TU Delft - Water Resources)

Pierre Gentine (Columbia University)

Rafael S. Oliveira (University of Campinas)

Paulo R.L. Bittencourt (University of Campinas)

Fernanda de V. Barros (University of Campinas)

NC van de Giesen (TU Delft - Water Resources)

Research Group
Water Resources
Copyright
© 2018 T.H.M. van Emmerik, S.C. Steele-Dunne, Pierre Gentine, Rafael S. Oliveira, Paulo R.L. Bittencourt, Fernanda de V. Barros, N.C. van de Giesen
DOI related publication
https://doi.org/10.5194/bg-2018-289
More Info
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Publication Year
2018
Language
English
Copyright
© 2018 T.H.M. van Emmerik, S.C. Steele-Dunne, Pierre Gentine, Rafael S. Oliveira, Paulo R.L. Bittencourt, Fernanda de V. Barros, N.C. van de Giesen
Research Group
Water Resources
Issue number
21
Volume number
15
Pages (from-to)
6439-6449
Reuse Rights

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Abstract

Land–atmosphere interactions depend on momentum transfer from the atmosphere to the canopy, which in turn depends on the tree drag coefficient. It is known that the drag coefficient, and thus tree–atmosphere momentum transfer, can vary strongly within a canopy. Yet, only few measurements are available to study the variation of tree–atmosphere momentum transfer in time and space, and in response to tree water deficit. In this paper we use accelerometers to estimate tree–atmosphere momentum transfer for 19 individual trees of 7 different species in the Brazilian Amazon. The 5-month monitoring period included the transition from wet to dry months. Here, we demonstrate that, under field conditions, tree–atmosphere momentum transfer can vary considerably in time and space (up to a factor of 2.5). Increased water-related stem variations during the dry months are related to observed changes in tree–atmosphere momentum transfer, which is hypothesized to be caused by tree-water-deficit-induced changes in tree mass.