Articles | Volume 11, issue 21
https://doi.org/10.5194/bg-11-6159-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-11-6159-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Disentangling the response of forest and grassland energy exchange to heatwaves under idealized land–atmosphere coupling
C. C. van Heerwaarden
CORRESPONDING AUTHOR
Max Planck Institute for Meteorology, Hamburg, Germany
A. J. Teuling
Hydrology and Quantitative Water Management Group, Wageningen University, Wageningen, the Netherlands
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42 citations as recorded by crossref.
- Strong influence of convective heat transfer efficiency on the cooling benefits of green roof irrigation L. Wang et al. 10.1088/1748-9326/ac18ea
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- Surface-atmosphere energy exchanges and their effects on surface climate and atmospheric boundary layer characteristics in the forest-tundra ecotone in northwestern Canada V. Graveline et al. 10.1016/j.agrformet.2024.109996
- Carbon, water and energy fluxes in agricultural systems of Australia and New Zealand J. Cleverly et al. 10.1016/j.agrformet.2020.107934
- Contrasting Evaporative Responses of Ecosystems to Heatwaves Traced to the Opposing Roles of Vapor Pressure Deficit and Surface Resistance P. Wang et al. 10.1029/2019WR024771
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- Mitigation of drought negative effect on ecosystem productivity by vegetation mixing C. Van den Hoof & F. Lambert 10.1002/2016JG003625
- Land-atmosphere interaction during heat waves diagnosed using vapor pressure deficit dynamics S. Zhang et al. 10.1016/j.jhydrol.2024.132181
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- Soil drought can mitigate deadly heat stress thanks to a reduction of air humidity H. Wouters et al. 10.1126/sciadv.abe6653
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- Examining the evidence for decoupling between photosynthesis and transpiration during heat extremes M. De Kauwe et al. 10.5194/bg-16-903-2019
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- Vegetation-heatwave correlations and contrasting energy exchange responses of different vegetation types to summer heatwaves in the Northern Hemisphere during the 1982–2011 period J. Li et al. 10.1016/j.agrformet.2020.108208
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- Sensitivity of land–atmosphere coupling strength to changing atmospheric temperature and moisture over Europe L. Jach et al. 10.5194/esd-13-109-2022
- Observational evidence for cloud cover enhancement over western European forests A. Teuling et al. 10.1038/ncomms14065
- Examining the link between vegetation leaf area and land–atmosphere exchange of water, energy, and carbon fluxes using FLUXNET data A. Hoek van Dijke et al. 10.5194/bg-17-4443-2020
- Partitioning of Sensible and Latent Heat Fluxes in Different Vegetation Types and Their Spatiotemporal Variations Based on 203 FLUXNET Sites H. Lin et al. 10.1029/2022JD037142
- Grassland albedo as a nature-based climate prospect: the role of growth form and grazing S. McGregor et al. 10.1088/1748-9326/ad8765
- A conceptual model for a generalized canopy parametrization for atmospheric models G. Cheng & K. Schlünzen 10.1002/qj.4420
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- The effect of afforestation on moist heat stress in Loess Plateau, China S. Zhang et al. 10.1016/j.ejrh.2022.101209
- Land Cover Control on the Drivers of Evaporation and Sensible Heat Fluxes: An Observation‐Based Synthesis for the Netherlands F. Jansen et al. 10.1029/2022WR034361
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- Plant water-stress parameterization determines the strength of land–atmosphere coupling M. Combe et al. 10.1016/j.agrformet.2015.11.006
- Atmospheric Aridity and Apparent Soil Moisture Drought in European Forest During Heat Waves E. Lansu et al. 10.1029/2020GL087091
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Latest update: 13 Dec 2024
Short summary
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.
This study disentangles the response of forest and grassland to heatwaves, to interpret the...
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