Research article
13 Jun 2019
Research article
| 13 Jun 2019
Strengths and challenges for transient Mid- to Late Holocene simulations with dynamical vegetation
Pascale Braconnot et al.
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Cited
19 citations as recorded by crossref.
- Millennial-Scale Climate and Human Drivers of Environmental Change and Fire Activity in a Dry, Mixed-Conifer Forest of Northwestern Montana D. McWethy et al. 10.3389/ffgc.2020.00044
- Mid‐Holocene Sahara‐Sahel Precipitation From the Vantage of Present‐Day Climate P. Molnar & B. Rajagopalan 10.1029/2020GL088171
- Climate change in the Indo-Pacific basin from mid- to late Holocene F. Falasca et al. 10.1007/s00382-022-06153-z
- Northwestward shift of the northern boundary of the East Asian summer monsoon during the mid-Holocene caused by orbital forcing and vegetation feedbacks J. Chen et al. 10.1016/j.quascirev.2021.107136
- Abrupt Climate and Weather Changes Across Time Scales G. Lohmann et al. 10.1029/2019PA003782
- Speleothem records of monsoon interannual-interdecadal variability through the Holocene S. Parker et al. 10.1088/2515-7620/ac3eaa
- Feedbacks of soil properties on vegetation during the Green Sahara period W. Chen et al. 10.1016/j.quascirev.2020.106389
- Mid-Holocene to present-day evolution of the Indian monsoon in transient global simulations J. Crétat et al. 10.1007/s00382-020-05418-9
- High-resolution marine data and transient simulations support orbital forcing of ENSO amplitude since the mid-Holocene M. Carré et al. 10.1016/j.quascirev.2021.107125
- Large-scale features and evaluation of the PMIP4-CMIP6 <i>midHolocene</i> simulations C. Brierley et al. 10.5194/cp-16-1847-2020
- African Humid Period Precipitation Sustained by Robust Vegetation, Soil, and Lake Feedbacks D. Chandan & W. Peltier 10.1029/2020GL088728
- Holocene vegetation transitions and their climatic drivers in MPI-ESM1.2 A. Dallmeyer et al. 10.5194/cp-17-2481-2021
- The end of the African humid period as seen by a transient comprehensive Earth system model simulation of the last 8000 years A. Dallmeyer et al. 10.5194/cp-16-117-2020
- Comparison of climate responses to orbital forcing at different latitudes during the Holocene Y. Jing et al. 10.1016/j.quaint.2022.02.004
- Effect of nitrogen limitation and soil biophysics on Holocene greening of the Sahara J. Lee et al. 10.5194/cp-18-313-2022
- Impact of Multiscale Variability on Last 6,000 Years Indian and West African Monsoon Rain P. Braconnot et al. 10.1029/2019GL084797
- Spatiotemporal complexity and time-dependent networks in sea surface temperature from mid- to late Holocene F. Falasca et al. 10.1140/epjp/s13360-020-00403-x
- Spatial patterns of multi–centennial surface air temperature trends in Antarctica over 1–1000 CE: Insights from ice core records and modeling Z. Lyu et al. 10.1016/j.quascirev.2021.107205
- Probing the timescale dependency of local and global variations in surface air temperature from climate simulations and reconstructions of the last millennia B. Ellerhoff & K. Rehfeld 10.1103/PhysRevE.104.064136
19 citations as recorded by crossref.
- Millennial-Scale Climate and Human Drivers of Environmental Change and Fire Activity in a Dry, Mixed-Conifer Forest of Northwestern Montana D. McWethy et al. 10.3389/ffgc.2020.00044
- Mid‐Holocene Sahara‐Sahel Precipitation From the Vantage of Present‐Day Climate P. Molnar & B. Rajagopalan 10.1029/2020GL088171
- Climate change in the Indo-Pacific basin from mid- to late Holocene F. Falasca et al. 10.1007/s00382-022-06153-z
- Northwestward shift of the northern boundary of the East Asian summer monsoon during the mid-Holocene caused by orbital forcing and vegetation feedbacks J. Chen et al. 10.1016/j.quascirev.2021.107136
- Abrupt Climate and Weather Changes Across Time Scales G. Lohmann et al. 10.1029/2019PA003782
- Speleothem records of monsoon interannual-interdecadal variability through the Holocene S. Parker et al. 10.1088/2515-7620/ac3eaa
- Feedbacks of soil properties on vegetation during the Green Sahara period W. Chen et al. 10.1016/j.quascirev.2020.106389
- Mid-Holocene to present-day evolution of the Indian monsoon in transient global simulations J. Crétat et al. 10.1007/s00382-020-05418-9
- High-resolution marine data and transient simulations support orbital forcing of ENSO amplitude since the mid-Holocene M. Carré et al. 10.1016/j.quascirev.2021.107125
- Large-scale features and evaluation of the PMIP4-CMIP6 <i>midHolocene</i> simulations C. Brierley et al. 10.5194/cp-16-1847-2020
- African Humid Period Precipitation Sustained by Robust Vegetation, Soil, and Lake Feedbacks D. Chandan & W. Peltier 10.1029/2020GL088728
- Holocene vegetation transitions and their climatic drivers in MPI-ESM1.2 A. Dallmeyer et al. 10.5194/cp-17-2481-2021
- The end of the African humid period as seen by a transient comprehensive Earth system model simulation of the last 8000 years A. Dallmeyer et al. 10.5194/cp-16-117-2020
- Comparison of climate responses to orbital forcing at different latitudes during the Holocene Y. Jing et al. 10.1016/j.quaint.2022.02.004
- Effect of nitrogen limitation and soil biophysics on Holocene greening of the Sahara J. Lee et al. 10.5194/cp-18-313-2022
- Impact of Multiscale Variability on Last 6,000 Years Indian and West African Monsoon Rain P. Braconnot et al. 10.1029/2019GL084797
- Spatiotemporal complexity and time-dependent networks in sea surface temperature from mid- to late Holocene F. Falasca et al. 10.1140/epjp/s13360-020-00403-x
- Spatial patterns of multi–centennial surface air temperature trends in Antarctica over 1–1000 CE: Insights from ice core records and modeling Z. Lyu et al. 10.1016/j.quascirev.2021.107205
- Probing the timescale dependency of local and global variations in surface air temperature from climate simulations and reconstructions of the last millennia B. Ellerhoff & K. Rehfeld 10.1103/PhysRevE.104.064136
Latest update: 18 May 2022
Short summary
This study discusses a simulation of the last 6000 years realized with a climate model in which the vegetation and carbon cycle are fully interactive. The long-term southward shift in Northern Hemisphere tree line and Afro-Asian monsoon rain are reproduced. The results show substantial change in tree composition with time over Eurasia and the role of trace gases in the recent past. They highlight the limitations due to model setup and multiple preindustrial vegetation states.
This study discusses a simulation of the last 6000 years realized with a climate model in which...