Academic Journal

Examining the evidence for decoupling between photosynthesis and transpiration during heat extremes

Bibliographic Details
Title: Examining the evidence for decoupling between photosynthesis and transpiration during heat extremes
Authors: M. G. De Kauwe, B. E. Medlyn, A. J. Pitman, J. E. Drake, A. Ukkola, A. Griebel, E. Pendall, S. Prober, M. Roderick
Source: Biogeosciences, Vol 16, Pp 903-916 (2019)
Publisher Information: Copernicus Publications, 2019.
Publication Year: 2019
Collection: LCC:Ecology
LCC:Life
LCC:Geology
Subject Terms: Ecology, QH540-549.5, Life, QH501-531, Geology, QE1-996.5
Description: Recent experimental evidence suggests that during heat extremes, wooded ecosystems may decouple photosynthesis and transpiration, reducing photosynthesis to near zero but increasing transpiration into the boundary layer. This feedback may act to dampen, rather than amplify, heat extremes in wooded ecosystems. We examined eddy covariance databases (OzFlux and FLUXNET2015) to identify whether there was field-based evidence to support these experimental findings. We focused on two types of heat extremes: (i) the 3 days leading up to a temperature extreme, defined as including a daily maximum temperature >37 ∘C (similar to the widely used TXx metric), and (ii) heatwaves, defined as 3 or more consecutive days above 35 ∘C. When focusing on (i), we found some evidence of reduced photosynthesis and sustained or increased latent heat fluxes at seven Australian evergreen wooded flux sites. However, when considering the role of vapour pressure deficit and focusing on (ii), we were unable to conclusively disentangle the decoupling between photosynthesis and latent heat flux from the effect of increasing the vapour pressure deficit. Outside of Australia, the Tier-1 FLUXNET2015 database provided limited scope to tackle this issue as it does not sample sufficient high temperature events with which to probe the physiological response of trees to extreme heat. Thus, further work is required to determine whether this photosynthetic decoupling occurs widely, ideally by matching experimental species with those found at eddy covariance tower sites. Such measurements would allow this decoupling mechanism to be probed experimentally and at the ecosystem scale. Transpiration during heatwaves remains a key issue to resolve, as no land surface model includes a decoupling mechanism, and any potential dampening of the land–atmosphere amplification is thus not included in climate model projections.
Document Type: article
File Description: electronic resource
Language: English
ISSN: 1726-4170
1726-4189
Relation: https://www.biogeosciences.net/16/903/2019/bg-16-903-2019.pdf; https://doaj.org/toc/1726-4170; https://doaj.org/toc/1726-4189
DOI: 10.5194/bg-16-903-2019
Access URL: https://doaj.org/article/8ee3aa2c6e1f4ff5b1d55ce805f7cdcb
Accession Number: edsdoj.8ee3aa2c6e1f4ff5b1d55ce805f7cdcb
Database: Directory of Open Access Journals
Description
ISSN:17264170
17264189
DOI:10.5194/bg-16-903-2019