Goal and products of PAGES LandCover6k 2018-2020: Past Global Land Cover and Land Use for Climate Modelling
- 1Dept of Biology and Environmental Science, Linnaeus University, Kalmar, Sweden (marie-jose.gaillard-lemdahl@lnu.se)
- 2Department of General Education, Mount Royal University, T3E 6K6, Calgary, Canada
- 3School of Geography, Earth and Environmental Sciences, Plymouth University, PL4 8AA, Plymouth, UK
- 4Department of Anthropology, University of Pennsylvania, 19104, Philadelphia, USA
- 5Geography and Environmental Science, University of Reading, RG66UD, Reading, UK
- 6ICREA Department of Humanities, University Pompeu Fabra (UPF), 08002, Barcelona, Spain
- 7Dep. of Environmental Systems Science, ETH, 8092, Zürich, Switzerland
- 8Department of Archaeology, University of Cambridge, CB2 3DZ, Cambridge, UK
- 9Department of Archaeology, University of Glasgow, G12 8QQ, Glasgow, UK
The question of whether prehistoric human impacts on land cover (i.e. anthropogenic land cover change due to land use, LULC) were sufficiently large to have a major impact on regional cli-mates is still a matter of debate. Climate model simulations have shown that LULC datasets can have large regional impacts on climate in recent and prehistoric time (1). But there are major differences between the available LULC scenarios/datasets such as HYDE (History Database of the Global En-vironment) and Kaplan’s KK10 (2), and diagnoses of inferred carbon-cycle impacts show that none of the scenarios are realistic (3). The only way to provide a useful assessment of the potential for LULC changes to affect climate in the past, is to provide more realistic LULC data based on palaeovegetation and archaeological evidence to improve the LULC datasets used in climate modelling(4). We use the REVEALS model to reconstruct LC from pollen data at a regional scale, and archaeological data to map LU types and distribution, and estimate per capita LU. The archaeology-based LU maps and per-capita LU estimates are used to improve LULC datasets. Pollen-based REVEALS LC estimates are then used to evaluate/validate the new, improved LULC datasets. These new datasets will be used to implement past land use in palaeoclimate and carbon cycle model simulations. Such simulations are necessary to assess the impact of LULC changes in the past and understand the effect of ecosys-tem management on future climate. We present results from five years of PAGES LandCover6k activities.
(1) Strandberg G, Kjellström E, Poska A, Wagner S, Gaillard M-J et al. (2014) Regional climate model sim-ulations for Europe at 6 and 0.2 k BP: sensitivity to changes in anthropogenic deforestation. Clim. Past 10, 661–680.
(2) Gaillard M-J, Sugita S, Mazier F et al (2010) Holocene land-cover reconstructions for studies on land cover-climate feedbacks. Clim. Past 6, 483-499.
(3) Stocker B, Yud Z, Massae C, Joos F (2017) Holocene peatland and ice-core data constraints on the tim-ing and magnitude of CO2 emissions from past land use. www.pnas.org/cgi/doi/10.1073/ pnas.1613889114.
(4) Harrison S P, Gaillard M-J, Stocker B D, Vander Linden M, Klein Goldewijk K, Boles O, Braconnot P, Dawson A, Fluet-Chouinard E, Kaplan J O, Kastner T, Pausata F S R, Robinson E, Whitehouse N J, Madella M, and Morrison K D (2019) Development and testing of scenarios for implementing Holocene LULC in Earth Sys-tem Model Experiments, Geosci. Model Dev. Discuss., https://doi.org/10.5194/gmd-2019-125, in review, 2019.
How to cite: Gaillard, M.-J., Dawson, A., Fyfe, R., Githumbi, E., Hammer, E., Harrison, S., Li, F., Madella, M., Morrison, K. D., Stocker, B., Vander Linden, M., and Whitehouse, N. J.: Goal and products of PAGES LandCover6k 2018-2020: Past Global Land Cover and Land Use for Climate Modelling, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11082, https://doi.org/10.5194/egusphere-egu2020-11082, 2020