Land management and land-cover change have impacts of similar magnitude on surface temperature

The direct effects of land-cover change on surface climate are increasingly well understood, but fewer studies have investigated the consequences of the trend towards more intensive land management practices. Now, research investigating the biophysical effects of temperate land-management changes re...

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Published inNature climate change Vol. 4; no. 5; pp. 389 - 393
Main Authors Luyssaert, Sebastiaan, Jammet, Mathilde, Stoy, Paul C., Estel, Stephan, Pongratz, Julia, Ceschia, Eric, Churkina, Galina, Don, Axel, Erb, KarlHeinz, Ferlicoq, Morgan, Gielen, Bert, Grünwald, Thomas, Houghton, Richard A., Klumpp, Katja, Knohl, Alexander, Kolb, Thomas, Kuemmerle, Tobias, Laurila, Tuomas, Lohila, Annalea, Loustau, Denis, McGrath, Matthew J., Meyfroidt, Patrick, Moors, Eddy J., Naudts, Kim, Novick, Kim, Otto, Juliane, Pilegaard, Kim, Pio, Casimiro A., Rambal, Serge, Rebmann, Corinna, Ryder, James, Suyker, Andrew E., Varlagin, Andrej, Wattenbach, Martin, Dolman, A. Johannes
Format Journal Article
LanguageEnglish
Published London Nature Publishing Group UK 01.05.2014
Nature Publishing Group
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Abstract The direct effects of land-cover change on surface climate are increasingly well understood, but fewer studies have investigated the consequences of the trend towards more intensive land management practices. Now, research investigating the biophysical effects of temperate land-management changes reveals a net warming effect of similar magnitude to that driven by changing land cover. Anthropogenic changes to land cover (LCC) remain common, but continuing land scarcity promotes the widespread intensification of land management changes (LMC) to better satisfy societal demand for food, fibre, fuel and shelter 1 . The biophysical effects of LCC on surface climate are largely understood 2 , 3 , 4 , 5 , particularly for the boreal 6 and tropical zones 7 , but fewer studies have investigated the biophysical consequences of LMC; that is, anthropogenic modification without a change in land cover type. Harmonized analysis of ground measurements and remote sensing observations of both LCC and LMC revealed that, in the temperate zone, potential surface cooling from increased albedo is typically offset by warming from decreased sensible heat fluxes, with the net effect being a warming of the surface. Temperature changes from LMC and LCC were of the same magnitude, and averaged 2 K at the vegetation surface and were estimated at 1.7 K in the planetary boundary layer. Given the spatial extent of land management (42–58% of the land surface) this calls for increasing the efforts to integrate land management in Earth System Science to better take into account the human impact on the climate 8 .
AbstractList Anthropogenic changes to land cover (LCC) remain common, but continuing land scarcity promotes the widespread intensification of land management changes (LMC) to better satisfy societal demand for food, fibre, fuel and shelter. The biophysical effects of LCC on surface climate are largely understood, particularly for the boreal and tropical zones, but fewer studies have investigated the biophysical consequences of LMC; that is, anthropogenic modification without a change in land cover type. Harmonized analysis of ground measurements and remote sensing observations of both LCC and LMC revealed that, in the temperate zone, potential surface cooling from increased albedo is typically offset by warming from decreased sensible heat fluxes, with the net effect being a warming of the surface. Temperature changes from LMC and LCC were of the same magnitude, and averaged 2 K at the vegetation surface and were estimated at 1.7 K in the planetary boundary layer. Given the spatial extent of land management (42-58% of the land surface) this calls for increasing the efforts to integrate land management in Earth System Science to better take into account the human impact on the climate.
The direct effects of land-cover change on surface climate are increasingly well understood, but fewer studies have investigated the consequences of the trend towards more intensive land management practices. Now, research investigating the biophysical effects of temperate land-management changes reveals a net warming effect of similar magnitude to that driven by changing land cover. Anthropogenic changes to land cover (LCC) remain common, but continuing land scarcity promotes the widespread intensification of land management changes (LMC) to better satisfy societal demand for food, fibre, fuel and shelter 1 . The biophysical effects of LCC on surface climate are largely understood 2 , 3 , 4 , 5 , particularly for the boreal 6 and tropical zones 7 , but fewer studies have investigated the biophysical consequences of LMC; that is, anthropogenic modification without a change in land cover type. Harmonized analysis of ground measurements and remote sensing observations of both LCC and LMC revealed that, in the temperate zone, potential surface cooling from increased albedo is typically offset by warming from decreased sensible heat fluxes, with the net effect being a warming of the surface. Temperature changes from LMC and LCC were of the same magnitude, and averaged 2 K at the vegetation surface and were estimated at 1.7 K in the planetary boundary layer. Given the spatial extent of land management (42–58% of the land surface) this calls for increasing the efforts to integrate land management in Earth System Science to better take into account the human impact on the climate 8 .
Anthropogenic changes to land cover (LCC) remain common, but continuing land scarcity promotes the widespread intensification of land management changes (LMC) to better satisfy societal demand for food, fibre, fuel and shelter1. The biophysical effects of LCC on surface climate are largely understood2, 3, 4, 5, particularly for the boreal6 and tropical zones7, but fewer studies have investigated the biophysical consequences of LMC; that is, anthropogenic modification without a change in land cover type. Harmonized analysis of ground measurements and remote sensing observations of both LCC and LMC revealed that, in the temperate zone, potential surface cooling from increased albedo is typically offset by warming from decreased sensible heat fluxes, with the net effect being a warming of the surface. Temperature changes from LMC and LCC were of the same magnitude, and averaged 2 K at the vegetation surface and were estimated at 1.7 K in the planetary boundary layer. Given the spatial extent of land management (42–58% of the land surface) this calls for increasing the efforts to integrate land management in Earth System Science to better take into account the human impact on the climate
Author Ryder, James
Klumpp, Katja
Laurila, Tuomas
Wattenbach, Martin
Erb, KarlHeinz
Gielen, Bert
Rebmann, Corinna
Houghton, Richard A.
McGrath, Matthew J.
Estel, Stephan
Kuemmerle, Tobias
Jammet, Mathilde
Lohila, Annalea
Pilegaard, Kim
Stoy, Paul C.
Knohl, Alexander
Otto, Juliane
Pio, Casimiro A.
Rambal, Serge
Meyfroidt, Patrick
Don, Axel
Dolman, A. Johannes
Luyssaert, Sebastiaan
Ferlicoq, Morgan
Varlagin, Andrej
Suyker, Andrew E.
Ceschia, Eric
Churkina, Galina
Grünwald, Thomas
Pongratz, Julia
Naudts, Kim
Kolb, Thomas
Loustau, Denis
Novick, Kim
Moors, Eddy J.
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  givenname: Sebastiaan
  surname: Luyssaert
  fullname: Luyssaert, Sebastiaan
  email: Sebastiaan.Luyssaert@lsce.ipsl.fr
  organization: Laboratoire des Sciences du Climat et l’Environnement (LSCE)
– sequence: 2
  givenname: Mathilde
  surname: Jammet
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  givenname: Paul C.
  surname: Stoy
  fullname: Stoy, Paul C.
  organization: Department of Land Resources and Environmental Sciences, Montana State University, Bozeman Montana 59717, USA
– sequence: 4
  givenname: Stephan
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  fullname: Estel, Stephan
  organization: Geography Department, Humboldt-Universität zu Berlin
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– sequence: 7
  givenname: Galina
  surname: Churkina
  fullname: Churkina, Galina
  organization: Geography Department, Humboldt-Universität zu Berlin
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  givenname: Axel
  surname: Don
  fullname: Don, Axel
  organization: Johann Heinrich von Thünen Institute, Institute of Agricultural Climate Research
– sequence: 9
  givenname: KarlHeinz
  surname: Erb
  fullname: Erb, KarlHeinz
  organization: Institute of Social Ecology Vienna (SEC) Alpen-Adria University Klagenfurt-Vienna-Graz
– sequence: 10
  givenname: Morgan
  surname: Ferlicoq
  fullname: Ferlicoq, Morgan
  organization: Max Planck Institute for Meteorology
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  givenname: Bert
  surname: Gielen
  fullname: Gielen, Bert
  organization: Department of Biology, Research Group on Plant and Vegetation Ecology, Universiteitsplein 1
– sequence: 12
  givenname: Thomas
  surname: Grünwald
  fullname: Grünwald, Thomas
  organization: Department of Meteorology, Institute of Hydrology and Meteorology, Technische Universität Dresden
– sequence: 13
  givenname: Richard A.
  surname: Houghton
  fullname: Houghton, Richard A.
  organization: Woods Hole Research Center, Falmouth Massachusetts 02540, USA
– sequence: 14
  givenname: Katja
  surname: Klumpp
  fullname: Klumpp, Katja
  organization: INRA, Grassland Ecosystem Research (UREP)
– sequence: 15
  givenname: Alexander
  surname: Knohl
  fullname: Knohl, Alexander
  organization: Georg-August University of Göttingen, Büsgenweg 2 37077 Göttingen, Germany
– sequence: 16
  givenname: Thomas
  surname: Kolb
  fullname: Kolb, Thomas
  organization: School of Forestry, Northern Arizona University, Flagstaff Arizona 86011, USA
– sequence: 17
  givenname: Tobias
  surname: Kuemmerle
  fullname: Kuemmerle, Tobias
  organization: Department of Land Resources and Environmental Sciences, Montana State University, Bozeman Montana 59717, USA, Germany and Earth System Analysis, Potsdam Institute for Climate Impact Research
– sequence: 18
  givenname: Tuomas
  surname: Laurila
  fullname: Laurila, Tuomas
  organization: Finnish Meteorological Institute, Climate Change Research, PO Box 503 FI-00101 Helsinki, Finland
– sequence: 19
  givenname: Annalea
  surname: Lohila
  fullname: Lohila, Annalea
  organization: Finnish Meteorological Institute, Climate Change Research, PO Box 503 FI-00101 Helsinki, Finland
– sequence: 20
  givenname: Denis
  surname: Loustau
  fullname: Loustau, Denis
  organization: INRA, unité EPHYSE
– sequence: 21
  givenname: Matthew J.
  surname: McGrath
  fullname: McGrath, Matthew J.
  organization: Laboratoire des Sciences du Climat et l’Environnement (LSCE)
– sequence: 22
  givenname: Patrick
  surname: Meyfroidt
  fullname: Meyfroidt, Patrick
  organization: F.R.S.-FNRS and Georges Lemaître Center for Earth and Climate, Earth and Life Institute, Université catholique de Louvain
– sequence: 23
  givenname: Eddy J.
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  fullname: Moors, Eddy J.
  organization: Alterra, PO Box 47 6700 AA Wageningen, The Netherlands
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  givenname: Kim
  surname: Naudts
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  organization: Laboratoire des Sciences du Climat et l’Environnement (LSCE)
– sequence: 25
  givenname: Kim
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  organization: USDA Forest Service – Southern Research Station, Coweeta Hydrologic Laboratory, Otto North Carolina 28763, USA
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  givenname: Juliane
  surname: Otto
  fullname: Otto, Juliane
  organization: Laboratoire des Sciences du Climat et l’Environnement (LSCE)
– sequence: 27
  givenname: Kim
  surname: Pilegaard
  fullname: Pilegaard, Kim
  organization: Department of Chemical and Biochemical Engineering, Center for Ecosystems and Environmental Sustainability, Technical University of Denmark, DTU Risø Campus PO Box 49 4000 Roskilde, Denmark
– sequence: 28
  givenname: Casimiro A.
  surname: Pio
  fullname: Pio, Casimiro A.
  organization: CESAM and Department of Environment, University of Aveiro, Campus de Santiago
– sequence: 29
  givenname: Serge
  surname: Rambal
  fullname: Rambal, Serge
  organization: CEFE CNRS
– sequence: 30
  givenname: Corinna
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  fullname: Rebmann, Corinna
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  givenname: James
  surname: Ryder
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  givenname: Andrew E.
  surname: Suyker
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  organization: School of Natural Resources, 32 L.W. Chase Hall, PO Box 830728, University of Nebraska-Lincoln, Lincoln
– sequence: 33
  givenname: Andrej
  surname: Varlagin
  fullname: Varlagin, Andrej
  organization: A.N. Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences Leninsky pr., 33
– sequence: 34
  givenname: Martin
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  fullname: Wattenbach, Martin
  organization: Helmholtz Centre Potsdam, section 5.4 Hydrology, GFZ German Research Center For Geosciences
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  givenname: A. Johannes
  surname: Dolman
  fullname: Dolman, A. Johannes
  organization: Department of Earth Sciences, Earth and Climate cluster, VU University Amsterdam, Boelelaan 1085 1081 HV Amsterdam, The Netherlands
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https://hal.inrae.fr/hal-02641525$$DView record in HAL
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Issue 5
Keywords Ground based measurement
Space remote sensing
climate warming
Satellite observation
Surface temperature
exploitation
Atmospheric temperature
Human activity
global change
Observation data
Effect on climate
land cover
climate change
Anthropogenic factor
climate change; energy; carbon
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Snippet The direct effects of land-cover change on surface climate are increasingly well understood, but fewer studies have investigated the consequences of the trend...
Anthropogenic changes to land cover (LCC) remain common, but continuing land scarcity promotes the widespread intensification of land management changes (LMC)...
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SubjectTerms 631/158/47
704/106/47
Albedo
Anthropogenic factors
Boundary layers
carbon
Climate Change
Climate Change/Climate Change Impacts
Climatology. Bioclimatology. Climate change
earth
Earth, ocean, space
energy
Environment
Environmental Law/Policy/Ecojustice
Environmental Sciences
Environmental studies
Exact sciences and technology
External geophysics
feedbacks
forests
Global Changes
Human-environment relationship
Humanities and Social Sciences
Land management
letter
Meteorology
Remote sensing
Sensible heat
Surface temperature
vegetation
Title Land management and land-cover change have impacts of similar magnitude on surface temperature
URI https://link.springer.com/article/10.1038/nclimate2196
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Volume 4
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