Articles | Volume 10, issue 3
https://doi.org/10.5194/esd-10-473-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esd-10-473-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Different response of surface temperature and air temperature to deforestation in climate models
Johannes Winckler
Max Planck Institute for Meteorology, Hamburg, Germany
International Max Planck Research School on Earth System Modeling, Hamburg, Germany
Christian H. Reick
Max Planck Institute for Meteorology, Hamburg, Germany
Sebastiaan Luyssaert
Faculty of Science, Vrije Universiteit Amsterdam, Amsterdam, the Netherlands
Alessandro Cescatti
Institute for Environment and Sustainability, Joint Research Centre, European Commission, Ispra, Italy
Paul C. Stoy
Department of Land Resources and Environmental Sciences, Montana State University, Bozeman, MT, USA
Quentin Lejeune
Institute for Atmospheric and Climate Science, ETH-Zürich, Zurich, Switzerland
currently at: Climate Analytics, Berlin, Germany
Thomas Raddatz
Max Planck Institute for Meteorology, Hamburg, Germany
Andreas Chlond
Max Planck Institute for Meteorology, Hamburg, Germany
Marvin Heidkamp
Max Planck Institute for Meteorology, Hamburg, Germany
International Max Planck Research School on Earth System Modeling, Hamburg, Germany
Julia Pongratz
CORRESPONDING AUTHOR
Max Planck Institute for Meteorology, Hamburg, Germany
Ludwig-Maximilians-Universität München, Munich, Germany
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40 citations as recorded by crossref.
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- Importance of Surface Roughness for the Local Biogeophysical Effects of Deforestation J. Winckler et al. 10.1029/2018JD030127
- Reforestation and surface cooling in temperate zones: Mechanisms and implications Q. Zhang et al. 10.1111/gcb.15069
- Initial Land Use/Cover Distribution Substantially Affects Global Carbon and Local Temperature Projections in the Integrated Earth System Model A. Di Vittorio et al. 10.1029/2019GB006383
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- Effects of land use and anthropogenic aerosol emissions in the Roman Empire A. Gilgen et al. 10.5194/cp-15-1885-2019
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- A modelling study on quantifying the impact of urbanization and regional effects on the wintertime surface temperature over a rapidly-growing tropical city G. Nandini et al. 10.1007/s43762-022-00067-6
- Land Use Effects on Climate: Current State, Recent Progress, and Emerging Topics J. Pongratz et al. 10.1007/s40641-021-00178-y
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- An assessment of potential climate impact during 1948–2010 using historical land use land cover change maps N. Chilukoti & Y. Xue 10.1002/joc.6621
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- The biogeophysical effects of idealized land cover and land management changes in Earth system models S. De Hertog et al. 10.5194/esd-14-629-2023
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- Relationships between current climate and deforestation on citrus productivity in Northeastern Pará (Eastern Amazon) T. Dias & E. Souza 10.26848/rbgf.v17.2.p1375-1395
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- The biophysical climate mitigation potential of boreal peatlands during the growing season M. Helbig et al. 10.1088/1748-9326/abab34
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- Geotechnologies applied in the analysis of land use and land cover (LULC) transition in a hydrographic basin in the Brazilian Cerrado W. Alves et al. 10.1016/j.rsase.2021.100495
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- Biomass heat storage dampens diurnal temperature variations in forests R. Meier et al. 10.1088/1748-9326/ab2b4e
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Latest update: 20 Nov 2024
Short summary
For local living conditions, it matters whether deforestation influences the surface temperature, temperature at 2 m, or the temperature higher up in the atmosphere. Here, simulations with a climate model show that at a location of deforestation, surface temperature generally changes more strongly than atmospheric temperature. Comparison across climate models shows that both for summer and winter the surface temperature response exceeds the air temperature response locally by a factor of 2.
For local living conditions, it matters whether deforestation influences the surface...
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