African hydroclimate during the early Eocene from the DeepMIP simulations

Accepted/In Press date: 26 April 2022

e-pub ahead of print date: 9 May 2022

Published date: 10 May 2022

Additional Information: 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.

Keywords: African precipitation, DeepMIP, arly Eocene, paleoclimate

Local EPrints ID: 457539

URI: http://eprints.soton.ac.uk/id/eprint/457539

DOI: doi:10.1029/2022PA004419

ISSN: 2572-4525

PURE UUID: 966a9c94-8e80-4243-ab54-6eed9d411ce7

ORCID for Gordon Inglis: orcid.org/0000-0002-0032-4668

Date deposited: 10 Jun 2022 16:41

Last modified: 17 Mar 2024 04:00