Articles | Volume 10, issue 6
https://doi.org/10.5194/bg-10-3593-2013
© Author(s) 2013. 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-10-3593-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Impact of CO2 and climate on Last Glacial maximum vegetation – a factor separation
M. Claussen
Max Planck Institute for Meteorology, Hamburg, Germany
K. Selent
Max Planck Institute for Meteorology, Hamburg, Germany
Meteorological Institute, University of Hamburg, Germany
now at: Deutsches Klimarechenzentrum DKRZ, Hamburg, Germany
V. Brovkin
Max Planck Institute for Meteorology, Hamburg, Germany
T. Raddatz
Max Planck Institute for Meteorology, Hamburg, Germany
V. Gayler
Max Planck Institute for Meteorology, Hamburg, Germany
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23 citations as recorded by crossref.
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- Vegetation over the last glacial maximum at Girraween Lagoon, monsoonal northern Australia C. Rowe et al. 10.1017/qua.2020.50
- Glacial Amazonia at the canopy-scale: Using a biophysical model to understand forest robustness H. Sato & S. Cowling 10.1016/j.quascirev.2017.06.027
- Earth system model simulations show different feedback strengths of the terrestrial carbon cycle under glacial and interglacial conditions M. Adloff et al. 10.5194/esd-9-413-2018
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- Simulating effects of changing climate andCO2emissions on soil carbon pools at the Hubbard Brook experimental forest A. Dib et al. 10.1111/gcb.12436
- Model-Based Analyses Suggest Pleistocene Refugia over Ancient Divergence as Main Diversification Driver for a Neotropical Open-Habitat Treefrog F. Brusquetti et al. 10.1007/s11692-023-09614-3
- Palaeohydrology of lowland rivers in the Murray-Darling Basin, Australia P. Hesse et al. 10.1016/j.quascirev.2018.09.035
- Sunlit, controlled‐environment chambers are essential for comparing plant responses to various climates L. Allen et al. 10.1002/agj2.20428
- Beringia and the global dispersal of modern humans J. Hoffecker et al. 10.1002/evan.21478
- On the mechanisms of warming the mid-Pliocene and the inference of a hierarchy of climate sensitivities with relevance to the understanding of climate futures D. Chandan & W. Peltier 10.5194/cp-14-825-2018
- Assessing the effects of climate change on the distribution of Daphne mucronata in Iran F. Tarnian et al. 10.1007/s10661-021-09311-8
- Identifying Global‐Scale Patterns of Vegetation Change During the Last Deglaciation From Paleoclimate Networks M. Adam et al. 10.1029/2021PA004265
- Tropical vegetation productivity and atmospheric methane over the last 40,000 years from model simulations and stalagmites in Sulawesi, Indonesia C. Krause et al. 10.1017/qua.2023.75
- Environmental selection during the last ice age on the mother-to-infant transmission of vitamin D and fatty acids through breast milk L. Hlusko et al. 10.1073/pnas.1711788115
- Quantifying regional vegetation changes in China during three contrasting temperature intervals since the last glacial maximum Q. Li et al. 10.1016/j.jseaes.2018.10.013
- Closing the energy balance using a canopy heat capacity and storage concept – a physically based approach for the land component JSBACHv3.11 M. Heidkamp et al. 10.5194/gmd-11-3465-2018
- Geographic variation in genetic and demographic performance: new insights from an old biogeographical paradigm S. Pironon et al. 10.1111/brv.12313
- Climate and CO 2 effects on the vegetation of southern tropical Africa over the last 37,000 years V. Khon et al. 10.1016/j.epsl.2014.06.043
- Modulation of ice ages via precession and dust-albedo feedbacks R. Ellis & M. Palmer 10.1016/j.gsf.2016.04.004
- Dry corridors opened by fire and low CO2 in Amazonian rainforest during the Last Glacial Maximum H. Sato et al. 10.1038/s41561-021-00777-2
23 citations as recorded by crossref.
- The impact of standard and hard‐coded parameters on the hydrologic fluxes in the Noah‐MP land surface model M. Cuntz et al. 10.1002/2016JD025097
- Global vegetation distribution driving factors in two Dynamic Global Vegetation Models of contrasting complexities H. Li et al. 10.1016/j.gloplacha.2019.05.009
- Vegetation over the last glacial maximum at Girraween Lagoon, monsoonal northern Australia C. Rowe et al. 10.1017/qua.2020.50
- Glacial Amazonia at the canopy-scale: Using a biophysical model to understand forest robustness H. Sato & S. Cowling 10.1016/j.quascirev.2017.06.027
- Earth system model simulations show different feedback strengths of the terrestrial carbon cycle under glacial and interglacial conditions M. Adloff et al. 10.5194/esd-9-413-2018
- Genomic imputation of ancient Asian populations contrasts local adaptation in pre- and post-agricultural Japan N. Cooke et al. 10.1016/j.isci.2024.110050
- Hydroclimatic changes in the Core Monsoon Zone of India since the Last Glacial Maximum: An overview of the palynological data and correlation with the marine and continental records M. Quamar et al. 10.1016/j.palaeo.2023.111844
- Simulating effects of changing climate andCO2emissions on soil carbon pools at the Hubbard Brook experimental forest A. Dib et al. 10.1111/gcb.12436
- Model-Based Analyses Suggest Pleistocene Refugia over Ancient Divergence as Main Diversification Driver for a Neotropical Open-Habitat Treefrog F. Brusquetti et al. 10.1007/s11692-023-09614-3
- Palaeohydrology of lowland rivers in the Murray-Darling Basin, Australia P. Hesse et al. 10.1016/j.quascirev.2018.09.035
- Sunlit, controlled‐environment chambers are essential for comparing plant responses to various climates L. Allen et al. 10.1002/agj2.20428
- Beringia and the global dispersal of modern humans J. Hoffecker et al. 10.1002/evan.21478
- On the mechanisms of warming the mid-Pliocene and the inference of a hierarchy of climate sensitivities with relevance to the understanding of climate futures D. Chandan & W. Peltier 10.5194/cp-14-825-2018
- Assessing the effects of climate change on the distribution of Daphne mucronata in Iran F. Tarnian et al. 10.1007/s10661-021-09311-8
- Identifying Global‐Scale Patterns of Vegetation Change During the Last Deglaciation From Paleoclimate Networks M. Adam et al. 10.1029/2021PA004265
- Tropical vegetation productivity and atmospheric methane over the last 40,000 years from model simulations and stalagmites in Sulawesi, Indonesia C. Krause et al. 10.1017/qua.2023.75
- Environmental selection during the last ice age on the mother-to-infant transmission of vitamin D and fatty acids through breast milk L. Hlusko et al. 10.1073/pnas.1711788115
- Quantifying regional vegetation changes in China during three contrasting temperature intervals since the last glacial maximum Q. Li et al. 10.1016/j.jseaes.2018.10.013
- Closing the energy balance using a canopy heat capacity and storage concept – a physically based approach for the land component JSBACHv3.11 M. Heidkamp et al. 10.5194/gmd-11-3465-2018
- Geographic variation in genetic and demographic performance: new insights from an old biogeographical paradigm S. Pironon et al. 10.1111/brv.12313
- Climate and CO 2 effects on the vegetation of southern tropical Africa over the last 37,000 years V. Khon et al. 10.1016/j.epsl.2014.06.043
- Modulation of ice ages via precession and dust-albedo feedbacks R. Ellis & M. Palmer 10.1016/j.gsf.2016.04.004
- Dry corridors opened by fire and low CO2 in Amazonian rainforest during the Last Glacial Maximum H. Sato et al. 10.1038/s41561-021-00777-2
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