Research article
26 Oct 2017
Research article
| 26 Oct 2017
Quantifying the influence of the terrestrial biosphere on glacial–interglacial climate dynamics
Taraka Davies-Barnard et al.
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Cited
13 citations as recorded by crossref.
- Deglacial carbon cycle changes observed in a compilation of 127 benthic <i>δ</i><sup>13</sup>C time series (20–6 ka) C. Peterson & L. Lisiecki 10.5194/cp-14-1229-2018
- Spatio-temporal climate change contributes to latitudinal diversity gradients E. Saupe et al. 10.1038/s41559-019-0962-7
- Projected climatic changes lead to biome changes in areas of previously constant biome B. Huntley et al. 10.1111/jbi.14213
- Low terrestrial carbon storage at the Last Glacial Maximum: constraints from multi-proxy data A. Jeltsch-Thömmes et al. 10.5194/cp-15-849-2019
- Global vegetation patterns of the past 140,000 years J. Allen et al. 10.1111/jbi.13930
- Non‐random latitudinal gradients in range size and niche breadth predicted by spatial patterns of climate E. Saupe et al. 10.1111/geb.12904
- Variable C∕P composition of organic production and its effect on ocean carbon storage in glacial-like model simulations M. Ödalen et al. 10.5194/bg-17-2219-2020
- Ice-sheet modulation of deglacial North American monsoon intensification T. Bhattacharya et al. 10.1038/s41561-018-0220-7
- Response of an Afro-Palearctic bird migrant to glaciation cycles K. Thorup et al. 10.1073/pnas.2023836118
- Thermal niches of planktonic foraminifera are static throughout glacial–interglacial climate change G. Antell et al. 10.1073/pnas.2017105118
- A statistics-based reconstruction of high-resolution global terrestrial climate for the last 800,000 years M. Krapp et al. 10.1038/s41597-021-01009-3
- Complexities in interpreting chironomid-based temperature reconstructions over the Holocene from a lake in Western Ireland M. McKeown et al. 10.1016/j.quascirev.2019.105908
- Identifying Global‐Scale Patterns of Vegetation Change During the Last Deglaciation From Paleoclimate Networks M. Adam et al. 10.1029/2021PA004265
13 citations as recorded by crossref.
- Deglacial carbon cycle changes observed in a compilation of 127 benthic <i>δ</i><sup>13</sup>C time series (20–6 ka) C. Peterson & L. Lisiecki 10.5194/cp-14-1229-2018
- Spatio-temporal climate change contributes to latitudinal diversity gradients E. Saupe et al. 10.1038/s41559-019-0962-7
- Projected climatic changes lead to biome changes in areas of previously constant biome B. Huntley et al. 10.1111/jbi.14213
- Low terrestrial carbon storage at the Last Glacial Maximum: constraints from multi-proxy data A. Jeltsch-Thömmes et al. 10.5194/cp-15-849-2019
- Global vegetation patterns of the past 140,000 years J. Allen et al. 10.1111/jbi.13930
- Non‐random latitudinal gradients in range size and niche breadth predicted by spatial patterns of climate E. Saupe et al. 10.1111/geb.12904
- Variable C∕P composition of organic production and its effect on ocean carbon storage in glacial-like model simulations M. Ödalen et al. 10.5194/bg-17-2219-2020
- Ice-sheet modulation of deglacial North American monsoon intensification T. Bhattacharya et al. 10.1038/s41561-018-0220-7
- Response of an Afro-Palearctic bird migrant to glaciation cycles K. Thorup et al. 10.1073/pnas.2023836118
- Thermal niches of planktonic foraminifera are static throughout glacial–interglacial climate change G. Antell et al. 10.1073/pnas.2017105118
- A statistics-based reconstruction of high-resolution global terrestrial climate for the last 800,000 years M. Krapp et al. 10.1038/s41597-021-01009-3
- Complexities in interpreting chironomid-based temperature reconstructions over the Holocene from a lake in Western Ireland M. McKeown et al. 10.1016/j.quascirev.2019.105908
- Identifying Global‐Scale Patterns of Vegetation Change During the Last Deglaciation From Paleoclimate Networks M. Adam et al. 10.1029/2021PA004265
Latest update: 27 May 2022
Short summary
We present the first model analysis using a fully coupled dynamic atmosphere–ocean–vegetation GCM over the last 120 kyr that quantifies the net effect of vegetation on climate. This analysis shows that over the whole period the biogeophysical effect (albedo, evapotranspiration) is dominant, and that the biogeochemical impacts may have a lower possible range than typically estimated. This emphasises the temporal reliance of the balance between biogeophysical and biogeochemical effects.
We present the first model analysis using a fully coupled dynamic atmosphere–ocean–vegetation...