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Past terrestrial hydroclimate sensitivity controlled by Earth system feedbacks
by
Otto-Bliesner, Bette L.
, Contoux, Camille
, Lunt, Daniel J.
, Dowsett, Harry J.
, Lohmann, Gerrit
, Brady, Esther C.
, Peltier, W. Richard
, Chan, Wing-Le
, Feng, Ran
, Hunter, Stephen J.
, Stepanek, Christian
, Haywood, Alan M.
, Bhattacharya, Tripti
, Williams, Charles J. R.
, Abe-Ouchi, Ayako
, Zhang, Qiong
, Tindall, Julia C.
, Kageyama, Masa
, Tan, Ning
, Zhang, Zhongshi
, Guo, Chuncheng
, Li, Xiangyu
, Han, Zixuan
, Chandan, Deepak
in
704/106/413
/ 704/106/694
/ Carbon dioxide
/ Climate change
/ Continental interfaces, environment
/ Earth science
/ Earth, Planet
/ El Nino
/ Equilibrium
/ Feedback
/ Humanities and Social Sciences
/ Hydroclimate
/ Hypotheses
/ Ice Cover
/ Ice sheets
/ Laboratories
/ Land cover
/ multidisciplinary
/ Ocean, Atmosphere
/ Paleoclimate
/ Paleoclimatology
/ Pliocene
/ Precipitation
/ Proxies
/ Radiative forcing
/ Science
/ Science (multidisciplinary)
/ Sciences of the Universe
/ Simulation
/ Surface temperature
/ Tectonics
/ Vegetation
/ Vegetation changes
2022
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Past terrestrial hydroclimate sensitivity controlled by Earth system feedbacks
by
Otto-Bliesner, Bette L.
, Contoux, Camille
, Lunt, Daniel J.
, Dowsett, Harry J.
, Lohmann, Gerrit
, Brady, Esther C.
, Peltier, W. Richard
, Chan, Wing-Le
, Feng, Ran
, Hunter, Stephen J.
, Stepanek, Christian
, Haywood, Alan M.
, Bhattacharya, Tripti
, Williams, Charles J. R.
, Abe-Ouchi, Ayako
, Zhang, Qiong
, Tindall, Julia C.
, Kageyama, Masa
, Tan, Ning
, Zhang, Zhongshi
, Guo, Chuncheng
, Li, Xiangyu
, Han, Zixuan
, Chandan, Deepak
in
704/106/413
/ 704/106/694
/ Carbon dioxide
/ Climate change
/ Continental interfaces, environment
/ Earth science
/ Earth, Planet
/ El Nino
/ Equilibrium
/ Feedback
/ Humanities and Social Sciences
/ Hydroclimate
/ Hypotheses
/ Ice Cover
/ Ice sheets
/ Laboratories
/ Land cover
/ multidisciplinary
/ Ocean, Atmosphere
/ Paleoclimate
/ Paleoclimatology
/ Pliocene
/ Precipitation
/ Proxies
/ Radiative forcing
/ Science
/ Science (multidisciplinary)
/ Sciences of the Universe
/ Simulation
/ Surface temperature
/ Tectonics
/ Vegetation
/ Vegetation changes
2022
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Past terrestrial hydroclimate sensitivity controlled by Earth system feedbacks
by
Otto-Bliesner, Bette L.
, Contoux, Camille
, Lunt, Daniel J.
, Dowsett, Harry J.
, Lohmann, Gerrit
, Brady, Esther C.
, Peltier, W. Richard
, Chan, Wing-Le
, Feng, Ran
, Hunter, Stephen J.
, Stepanek, Christian
, Haywood, Alan M.
, Bhattacharya, Tripti
, Williams, Charles J. R.
, Abe-Ouchi, Ayako
, Zhang, Qiong
, Tindall, Julia C.
, Kageyama, Masa
, Tan, Ning
, Zhang, Zhongshi
, Guo, Chuncheng
, Li, Xiangyu
, Han, Zixuan
, Chandan, Deepak
in
704/106/413
/ 704/106/694
/ Carbon dioxide
/ Climate change
/ Continental interfaces, environment
/ Earth science
/ Earth, Planet
/ El Nino
/ Equilibrium
/ Feedback
/ Humanities and Social Sciences
/ Hydroclimate
/ Hypotheses
/ Ice Cover
/ Ice sheets
/ Laboratories
/ Land cover
/ multidisciplinary
/ Ocean, Atmosphere
/ Paleoclimate
/ Paleoclimatology
/ Pliocene
/ Precipitation
/ Proxies
/ Radiative forcing
/ Science
/ Science (multidisciplinary)
/ Sciences of the Universe
/ Simulation
/ Surface temperature
/ Tectonics
/ Vegetation
/ Vegetation changes
2022
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Past terrestrial hydroclimate sensitivity controlled by Earth system feedbacks
Journal Article
Past terrestrial hydroclimate sensitivity controlled by Earth system feedbacks
2022
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Overview
Despite tectonic conditions and atmospheric
CO
2
levels (
pCO
2
) similar to those of present-day, geological reconstructions from the mid-Pliocene (3.3-3.0 Ma) document high lake levels in the Sahel and mesic conditions in subtropical Eurasia, suggesting drastic reorganizations of subtropical terrestrial hydroclimate during this interval. Here, using a compilation of proxy data and multi-model paleoclimate simulations, we show that the mid-Pliocene hydroclimate state is not driven by direct
CO
2
radiative forcing but by a loss of northern high-latitude ice sheets and continental greening. These ice sheet and vegetation changes are long-term Earth system feedbacks to elevated
pCO
2
. Further, the moist conditions in the Sahel and subtropical Eurasia during the mid-Pliocene are a product of enhanced tropospheric humidity and a stationary wave response to the surface warming pattern, which varies strongly with land cover changes. These findings highlight the potential for amplified terrestrial hydroclimate responses over long timescales to a sustained
CO
2
forcing.
In contrast to future projections, paleoclimate records often find wetter subtropics in tandem with elevated CO
2
. Here, a compilation of proxies and simulations are used to reveal the climate dynamics and feedbacks responsible for generating wet subtropics during the mid-Pliocene.
Publisher
Nature Publishing Group UK,Nature Publishing Group,Nature Portfolio
Subject
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