Articles | Volume 11, issue 21
Biogeosciences, 11, 6159–6171, 2014
https://doi.org/10.5194/bg-11-6159-2014

Special issue: Climate extremes and biogeochemical cycles in the terrestrial...

Biogeosciences, 11, 6159–6171, 2014
https://doi.org/10.5194/bg-11-6159-2014

Research article 13 Nov 2014

Research article | 13 Nov 2014

Disentangling the response of forest and grassland energy exchange to heatwaves under idealized land–atmosphere coupling

C. C. van Heerwaarden and A. J. Teuling

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Cited articles

Bonan, G. B.: Forests and climate change: forcings, feedbacks, and the climate benefits of forest, Science, 320, 1444–1449, 2008.
Brilli, F., Hoertnagl, L., Hammerle, A., Haslwanter, A., Hansel, A., oreto, F., and Wohlfahrt, G.: Leaf and ecosystem response to soil water availability in mountain grasslands, Agric. For. Meteorol., 151, 1731–1740, 2011.
Christidis, N., Stott, P. A., Hegerl, G. C., and Betts, R. A.: The role of land use change in the recent warming of daily extreme temperatures, Geophys. Res. Lett., 40, 589–594, 2013.
Davin, E. L. and de Noblet-Ducoudré: Climatic impact of global-scale deforestation: radiative versus nonradiative processes, J. Climate, 23, 97–112, 2010.
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This study disentangles the response of forest and grassland to heatwaves, to interpret the findings of Teuling et al. (2010), who found systematically higher temperatures over forests than over grasslands in European heatwaves. By means of a study with a simple coupled land–atmosphere model, we show that the increase in stomatal resistance of vegetation under high values of vapor pressure deficit explains most of the differences and that this increase is enhanced by boundary layer feedbacks.
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