African Hydroclimate During the Early Eocene From the DeepMIP Simulations

Charles J. R. Williams; Daniel J. Lunt; Ulrich Salzmann; Tammo Reichgelt; Gordon N. Inglis; David R. Greenwood; Wing‐le Chan; Ayako Abe‐ouchi; Yannick Donnadieu; David K. Hutchinson; Agatha M. Boer; Jean‐baptiste Ladant; Polina A. Morozova; Igor Niezgodzki; Gregor Knorr; Sebastian Steinig; Zhongshi Zhang; Jiang Zhu; Matthew Huber; Bette L. Otto‐bliesner

doi:10.1029/2022PA004419

African Hydroclimate During the Early Eocene From the DeepMIP Simulations

Charles J. R. Williams
, Daniel J. Lunt
, Ulrich Salzmann
, Tammo Reichgelt
, Gordon N. Inglis
, David R. Greenwood
, Wing‐le Chan
, Ayako Abe‐ouchi
, Yannick Donnadieu
, David K. Hutchinson
, Agatha M. Boer
, Jean‐baptiste Ladant
, Polina A. Morozova
, Igor Niezgodzki
, Gregor Knorr
, Sebastian Steinig
, Zhongshi Zhang
, Jiang Zhu
, Matthew Huber
, Bette L. Otto‐bliesner

Research output: Contribution to journal › Article (Academic Journal) › peer-review

16 Citations (Scopus)

219 Downloads (Pure)

Original language	English
Article number	e2022PA004419
Journal	Paleoceanography and Paleoclimatology
Volume	37
Issue number	5
DOIs	https://doi.org/10.1029/2022PA004419
Publication status	Published - 9 May 2022

Bibliographical note

Funding Information:
CJRW acknowledges the financial support of the UK Natural Environment Research Council funded SWEET project (Super‐Warm Early Eocene Temperatures), and that of the European Research Council. WLC and AAO acknowledge funding from JSPS KAKENHI and MEXT KAKENHI, and are grateful to JAMSTEC for use of the Earth Simulator. The numerical simulations performed by DKH and AMB used resources provided by the Swedish National Infrastructure for Computing (SNIC) at the National Supercomputer Centre (NSC), partially funded by the Swedish Research Council. YD and JBL thank GENCI for providing access to the HPC resources of TGCC. PAM thanks Evgeny Volodin and INM RAS for the help with INMCM simulations. GK acknowledges financial support by PACES through the Helmholtz association and the computing center of the Alfred Wegener Institute in Bremerhaven and the DKRZ in Hamburg (Germany) for computational resources, infrastructure, and support. JZ and BLOB acknowledge support from the National Center for Atmospheric Research, which is a major facility sponsored by the National Science Foundation. U.S. acknowledges funding from the Natural Environment Research Council. DRG acknowledges funding from the Natural Sciences and Engineering Council of Canada. GNI acknowledges a GCRF Royal Society Dorothy Hodgkin Fellowship. CJRW was supported by the UK Natural Environment Research Council‐funded SWEET project (Grant no. NE/P01903X/1) and that of the European Research Council under the European Union's Seventh Framework Program (FP/2007‐868 2013) (ERC Grant agreement no. 340923 (TGRES)). WLC and AAO were supported by JSPS KAKENHI (Grant no. 17H06104) and MEXT KAKENHI (Grant no. 17H06323). AMB and DKH were partially funded by the Swedish Research Council through Grant agreement no. 2016‐03912 and 2020‐04791, and DKH also acknowledges the support of FORMAS Grant 2018‐01621 and Australian Research Council Grant DE220100279. The GFDL simulations were performed at NSC, partially funded by the Swedish Research Council through Grant agreement no. 2018‐05973. YD and JBL were supported by GENCI under allocation no. 2019‐A0050102212. PAM was supported by the state assignment project no. АААА‐А19‐119022190173‐2 (FMGE‐2019‐0009). JZ and BLOB were supported by the National Science Foundation under cooperative agreement no. 1852977. U.S. was supported by the Natural Environment Research Council (Grant NE/P019137/1). DRG was supported by the Natural Sciences and Engineering Council of Canada (Grant no. 2016‐04337). GNI was supported by a GCRF Royal Society Dorothy Hodgkin Fellowship (DHF\R1\191178). MH acknowledges support from NSF OPP 1842059.

Funding Information:
CJRW acknowledges the financial support of the UK Natural Environment Research Council funded SWEET project (Super-Warm Early Eocene Temperatures), and that of the European Research Council. WLC and AAO acknowledge funding from JSPS KAKENHI and MEXT KAKENHI, and are grateful to JAMSTEC for use of the Earth Simulator. The numerical simulations performed by DKH and AMB used resources provided by the Swedish National Infrastructure for Computing (SNIC) at the National Supercomputer Centre (NSC), partially funded by the Swedish Research Council. YD and JBL thank GENCI for providing access to the HPC resources of TGCC. PAM thanks Evgeny Volodin and INM RAS for the help with INMCM simulations. GK acknowledges financial support by PACES through the Helmholtz association and the computing center of the Alfred Wegener Institute in Bremerhaven and the DKRZ in Hamburg (Germany) for computational resources, infrastructure, and support. JZ and BLOB acknowledge support from the National Center for Atmospheric Research, which is a major facility sponsored by the National Science Foundation. U.S. acknowledges funding from the Natural Environment Research Council. DRG acknowledges funding from the Natural Sciences and Engineering Council of Canada. GNI acknowledges a GCRF Royal Society Dorothy Hodgkin Fellowship. CJRW was supported by the UK Natural Environment Research Council-funded SWEET project (Grant no. NE/P01903X/1) and that of the European Research Council under the European Union's Seventh Framework Program (FP/2007-868 2013) (ERC Grant agreement no. 340923 (TGRES)). WLC and AAO were supported by JSPS KAKENHI (Grant no. 17H06104) and MEXT KAKENHI (Grant no. 17H06323). AMB and DKH were partially funded by the Swedish Research Council through Grant agreement no. 2016-03912 and 2020-04791, and DKH also acknowledges the support of FORMAS Grant 2018-01621 and Australian Research Council Grant DE220100279. The GFDL simulations were performed at NSC, partially funded by the Swedish Research Council through Grant agreement no. 2018-05973. YD and JBL were supported by GENCI under allocation no. 2019-A0050102212. PAM was supported by the state assignment project no. АААА-А19-119022190173-2 (FMGE-2019-0009). JZ and BLOB were supported by the National Science Foundation under cooperative agreement no. 1852977. U.S. was supported by the Natural Environment Research Council (Grant NE/P019137/1). DRG was supported by the Natural Sciences and Engineering Council of Canada (Grant no. 2016-04337). GNI was supported by a GCRF Royal Society Dorothy Hodgkin Fellowship (DHF\R1\191178). MH acknowledges support from NSF OPP 1842059.

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© 2022. The Authors.

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Lunt, D. (Principal Investigator)
1/10/17 → 30/09/23
Project: Research

Cite this

Williams, C. J. R., Lunt, D. J., Salzmann, U., Reichgelt, T., Inglis, G. N., Greenwood, D. R., Chan, W., Abe‐ouchi, A., Donnadieu, Y., Hutchinson, D. K., Boer, A. M., Ladant, J., Morozova, P. A., Niezgodzki, I., Knorr, G., Steinig, S., Zhang, Z., Zhu, J., Huber, M., & Otto‐bliesner, B. L. (2022). African Hydroclimate During the Early Eocene From the DeepMIP Simulations. Paleoceanography and Paleoclimatology, 37(5), Article e2022PA004419. https://doi.org/10.1029/2022PA004419

@article{5831e0a616de487d8420ee9f37c60e1d,

title = "African Hydroclimate During the Early Eocene From the DeepMIP Simulations",

author = "Williams, \{Charles J. R.\} and Lunt, \{Daniel J.\} and Ulrich Salzmann and Tammo Reichgelt and Inglis, \{Gordon N.\} and Greenwood, \{David R.\} and Wing‐le Chan and Ayako Abe‐ouchi and Yannick Donnadieu and Hutchinson, \{David K.\} and Boer, \{Agatha M.\} and Jean‐baptiste Ladant and Morozova, \{Polina A.\} and Igor Niezgodzki and Gregor Knorr and Sebastian Steinig and Zhongshi Zhang and Jiang Zhu and Matthew Huber and Otto‐bliesner, \{Bette L.\}",

note = "Funding Information: CJRW acknowledges the financial support of the UK Natural Environment Research Council funded SWEET project (Super‐Warm Early Eocene Temperatures), and that of the European Research Council. WLC and AAO acknowledge funding from JSPS KAKENHI and MEXT KAKENHI, and are grateful to JAMSTEC for use of the Earth Simulator. The numerical simulations performed by DKH and AMB used resources provided by the Swedish National Infrastructure for Computing (SNIC) at the National Supercomputer Centre (NSC), partially funded by the Swedish Research Council. YD and JBL thank GENCI for providing access to the HPC resources of TGCC. PAM thanks Evgeny Volodin and INM RAS for the help with INMCM simulations. GK acknowledges financial support by PACES through the Helmholtz association and the computing center of the Alfred Wegener Institute in Bremerhaven and the DKRZ in Hamburg (Germany) for computational resources, infrastructure, and support. JZ and BLOB acknowledge support from the National Center for Atmospheric Research, which is a major facility sponsored by the National Science Foundation. U.S. acknowledges funding from the Natural Environment Research Council. DRG acknowledges funding from the Natural Sciences and Engineering Council of Canada. GNI acknowledges a GCRF Royal Society Dorothy Hodgkin Fellowship. CJRW was supported by the UK Natural Environment Research Council‐funded SWEET project (Grant no. NE/P01903X/1) and that of the European Research Council under the European Union's Seventh Framework Program (FP/2007‐868 2013) (ERC Grant agreement no. 340923 (TGRES)). WLC and AAO were supported by JSPS KAKENHI (Grant no. 17H06104) and MEXT KAKENHI (Grant no. 17H06323). AMB and DKH were partially funded by the Swedish Research Council through Grant agreement no. 2016‐03912 and 2020‐04791, and DKH also acknowledges the support of FORMAS Grant 2018‐01621 and Australian Research Council Grant DE220100279. The GFDL simulations were performed at NSC, partially funded by the Swedish Research Council through Grant agreement no. 2018‐05973. YD and JBL were supported by GENCI under allocation no. 2019‐A0050102212. PAM was supported by the state assignment project no. АААА‐А19‐119022190173‐2 (FMGE‐2019‐0009). JZ and BLOB were supported by the National Science Foundation under cooperative agreement no. 1852977. U.S. was supported by the Natural Environment Research Council (Grant NE/P019137/1). DRG was supported by the Natural Sciences and Engineering Council of Canada (Grant no. 2016‐04337). GNI was supported by a GCRF Royal Society Dorothy Hodgkin Fellowship (DHF\textbackslash{}R1\textbackslash{}191178). MH acknowledges support from NSF OPP 1842059. Funding Information: CJRW acknowledges the financial support of the UK Natural Environment Research Council funded SWEET project (Super-Warm Early Eocene Temperatures), and that of the European Research Council. WLC and AAO acknowledge funding from JSPS KAKENHI and MEXT KAKENHI, and are grateful to JAMSTEC for use of the Earth Simulator. The numerical simulations performed by DKH and AMB used resources provided by the Swedish National Infrastructure for Computing (SNIC) at the National Supercomputer Centre (NSC), partially funded by the Swedish Research Council. YD and JBL thank GENCI for providing access to the HPC resources of TGCC. PAM thanks Evgeny Volodin and INM RAS for the help with INMCM simulations. GK acknowledges financial support by PACES through the Helmholtz association and the computing center of the Alfred Wegener Institute in Bremerhaven and the DKRZ in Hamburg (Germany) for computational resources, infrastructure, and support. JZ and BLOB acknowledge support from the National Center for Atmospheric Research, which is a major facility sponsored by the National Science Foundation. U.S. acknowledges funding from the Natural Environment Research Council. DRG acknowledges funding from the Natural Sciences and Engineering Council of Canada. GNI acknowledges a GCRF Royal Society Dorothy Hodgkin Fellowship. CJRW was supported by the UK Natural Environment Research Council-funded SWEET project (Grant no. NE/P01903X/1) and that of the European Research Council under the European Union's Seventh Framework Program (FP/2007-868 2013) (ERC Grant agreement no. 340923 (TGRES)). WLC and AAO were supported by JSPS KAKENHI (Grant no. 17H06104) and MEXT KAKENHI (Grant no. 17H06323). AMB and DKH were partially funded by the Swedish Research Council through Grant agreement no. 2016-03912 and 2020-04791, and DKH also acknowledges the support of FORMAS Grant 2018-01621 and Australian Research Council Grant DE220100279. The GFDL simulations were performed at NSC, partially funded by the Swedish Research Council through Grant agreement no. 2018-05973. YD and JBL were supported by GENCI under allocation no. 2019-A0050102212. PAM was supported by the state assignment project no. АААА-А19-119022190173-2 (FMGE-2019-0009). JZ and BLOB were supported by the National Science Foundation under cooperative agreement no. 1852977. U.S. was supported by the Natural Environment Research Council (Grant NE/P019137/1). DRG was supported by the Natural Sciences and Engineering Council of Canada (Grant no. 2016-04337). GNI was supported by a GCRF Royal Society Dorothy Hodgkin Fellowship (DHF\textbackslash{}R1\textbackslash{}191178). MH acknowledges support from NSF OPP 1842059. Publisher Copyright: {\textcopyright} 2022. The Authors.",

year = "2022",

month = may,

day = "9",

doi = "10.1029/2022PA004419",

language = "English",

volume = "37",

journal = "Paleoceanography and Paleoclimatology",

issn = "2572-4517",

publisher = "John Wiley and Sons Inc",

number = "5",

}

Williams, CJR , Lunt, DJ, Salzmann, U, Reichgelt, T, Inglis, GN, Greenwood, DR, Chan, W, Abe‐ouchi, A, Donnadieu, Y, Hutchinson, DK, Boer, AM, Ladant, J, Morozova, PA, Niezgodzki, I, Knorr, G, Steinig, S, Zhang, Z, Zhu, J, Huber, M & Otto‐bliesner, BL 2022, 'African Hydroclimate During the Early Eocene From the DeepMIP Simulations', Paleoceanography and Paleoclimatology, vol. 37, no. 5, e2022PA004419. https://doi.org/10.1029/2022PA004419

TY - JOUR

T1 - African Hydroclimate During the Early Eocene From the DeepMIP Simulations

AU - Williams, Charles J. R.

AU - Lunt, Daniel J.

AU - Salzmann, Ulrich

AU - Reichgelt, Tammo

AU - Inglis, Gordon N.

AU - Greenwood, David R.

AU - Chan, Wing‐le

AU - Abe‐ouchi, Ayako

AU - Donnadieu, Yannick

AU - Hutchinson, David K.

AU - Boer, Agatha M.

AU - Ladant, Jean‐baptiste

AU - Morozova, Polina A.

AU - Niezgodzki, Igor

AU - Knorr, Gregor

AU - Steinig, Sebastian

AU - Zhang, Zhongshi

AU - Zhu, Jiang

AU - Huber, Matthew

AU - Otto‐bliesner, Bette L.

N1 - Funding Information: CJRW acknowledges the financial support of the UK Natural Environment Research Council funded SWEET project (Super‐Warm Early Eocene Temperatures), and that of the European Research Council. WLC and AAO acknowledge funding from JSPS KAKENHI and MEXT KAKENHI, and are grateful to JAMSTEC for use of the Earth Simulator. The numerical simulations performed by DKH and AMB used resources provided by the Swedish National Infrastructure for Computing (SNIC) at the National Supercomputer Centre (NSC), partially funded by the Swedish Research Council. YD and JBL thank GENCI for providing access to the HPC resources of TGCC. PAM thanks Evgeny Volodin and INM RAS for the help with INMCM simulations. GK acknowledges financial support by PACES through the Helmholtz association and the computing center of the Alfred Wegener Institute in Bremerhaven and the DKRZ in Hamburg (Germany) for computational resources, infrastructure, and support. JZ and BLOB acknowledge support from the National Center for Atmospheric Research, which is a major facility sponsored by the National Science Foundation. U.S. acknowledges funding from the Natural Environment Research Council. DRG acknowledges funding from the Natural Sciences and Engineering Council of Canada. GNI acknowledges a GCRF Royal Society Dorothy Hodgkin Fellowship. CJRW was supported by the UK Natural Environment Research Council‐funded SWEET project (Grant no. NE/P01903X/1) and that of the European Research Council under the European Union's Seventh Framework Program (FP/2007‐868 2013) (ERC Grant agreement no. 340923 (TGRES)). WLC and AAO were supported by JSPS KAKENHI (Grant no. 17H06104) and MEXT KAKENHI (Grant no. 17H06323). AMB and DKH were partially funded by the Swedish Research Council through Grant agreement no. 2016‐03912 and 2020‐04791, and DKH also acknowledges the support of FORMAS Grant 2018‐01621 and Australian Research Council Grant DE220100279. The GFDL simulations were performed at NSC, partially funded by the Swedish Research Council through Grant agreement no. 2018‐05973. YD and JBL were supported by GENCI under allocation no. 2019‐A0050102212. PAM was supported by the state assignment project no. АААА‐А19‐119022190173‐2 (FMGE‐2019‐0009). JZ and BLOB were supported by the National Science Foundation under cooperative agreement no. 1852977. U.S. was supported by the Natural Environment Research Council (Grant NE/P019137/1). DRG was supported by the Natural Sciences and Engineering Council of Canada (Grant no. 2016‐04337). GNI was supported by a GCRF Royal Society Dorothy Hodgkin Fellowship (DHF\R1\191178). MH acknowledges support from NSF OPP 1842059. Funding Information: CJRW acknowledges the financial support of the UK Natural Environment Research Council funded SWEET project (Super-Warm Early Eocene Temperatures), and that of the European Research Council. WLC and AAO acknowledge funding from JSPS KAKENHI and MEXT KAKENHI, and are grateful to JAMSTEC for use of the Earth Simulator. The numerical simulations performed by DKH and AMB used resources provided by the Swedish National Infrastructure for Computing (SNIC) at the National Supercomputer Centre (NSC), partially funded by the Swedish Research Council. YD and JBL thank GENCI for providing access to the HPC resources of TGCC. PAM thanks Evgeny Volodin and INM RAS for the help with INMCM simulations. GK acknowledges financial support by PACES through the Helmholtz association and the computing center of the Alfred Wegener Institute in Bremerhaven and the DKRZ in Hamburg (Germany) for computational resources, infrastructure, and support. JZ and BLOB acknowledge support from the National Center for Atmospheric Research, which is a major facility sponsored by the National Science Foundation. U.S. acknowledges funding from the Natural Environment Research Council. DRG acknowledges funding from the Natural Sciences and Engineering Council of Canada. GNI acknowledges a GCRF Royal Society Dorothy Hodgkin Fellowship. CJRW was supported by the UK Natural Environment Research Council-funded SWEET project (Grant no. NE/P01903X/1) and that of the European Research Council under the European Union's Seventh Framework Program (FP/2007-868 2013) (ERC Grant agreement no. 340923 (TGRES)). WLC and AAO were supported by JSPS KAKENHI (Grant no. 17H06104) and MEXT KAKENHI (Grant no. 17H06323). AMB and DKH were partially funded by the Swedish Research Council through Grant agreement no. 2016-03912 and 2020-04791, and DKH also acknowledges the support of FORMAS Grant 2018-01621 and Australian Research Council Grant DE220100279. The GFDL simulations were performed at NSC, partially funded by the Swedish Research Council through Grant agreement no. 2018-05973. YD and JBL were supported by GENCI under allocation no. 2019-A0050102212. PAM was supported by the state assignment project no. АААА-А19-119022190173-2 (FMGE-2019-0009). JZ and BLOB were supported by the National Science Foundation under cooperative agreement no. 1852977. U.S. was supported by the Natural Environment Research Council (Grant NE/P019137/1). DRG was supported by the Natural Sciences and Engineering Council of Canada (Grant no. 2016-04337). GNI was supported by a GCRF Royal Society Dorothy Hodgkin Fellowship (DHF\R1\191178). MH acknowledges support from NSF OPP 1842059. Publisher Copyright: © 2022. The Authors.

PY - 2022/5/9

Y1 - 2022/5/9

U2 - 10.1029/2022PA004419

DO - 10.1029/2022PA004419

M3 - Article (Academic Journal)

C2 - 35915854

SN - 2572-4517

VL - 37

JO - Paleoceanography and Paleoclimatology

JF - Paleoceanography and Paleoclimatology

IS - 5

M1 - e2022PA004419

ER -

African Hydroclimate During the Early Eocene From the DeepMIP Simulations

Bibliographical note

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SWEET NERC Large Grant

Cite this