A suite of early Eocene (~ 55 Ma) climate model boundary conditions

We describe a set of early Eocene (~ 55 Ma) climate model boundary conditions constructed in a self-consistent reference frame and incorporating recent data and methodologies. Given the growing need for uniform experimental design within the Eocene climate modelling community and the challenges face...

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Published in:Geoscientific Model Development
Main Authors: Herold, N., Buzan, J., Seton, M., Goldner, A., Green, J. A. M., Müller, R. D., Markwick, P., Huber, M.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/gmd-7-2077-2014
https://gmd.copernicus.org/articles/7/2077/2014/
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spelling ftcopernicus:oai:publications.copernicus.org:gmd23423 2023-05-15T13:54:27+02:00 A suite of early Eocene (~ 55 Ma) climate model boundary conditions Herold, N. Buzan, J. Seton, M. Goldner, A. Green, J. A. M. Müller, R. D. Markwick, P. Huber, M. 2018-09-27 application/pdf https://doi.org/10.5194/gmd-7-2077-2014 https://gmd.copernicus.org/articles/7/2077/2014/ eng eng doi:10.5194/gmd-7-2077-2014 https://gmd.copernicus.org/articles/7/2077/2014/ eISSN: 1991-9603 Text 2018 ftcopernicus https://doi.org/10.5194/gmd-7-2077-2014 2020-07-20T16:24:57Z We describe a set of early Eocene (~ 55 Ma) climate model boundary conditions constructed in a self-consistent reference frame and incorporating recent data and methodologies. Given the growing need for uniform experimental design within the Eocene climate modelling community and the challenges faced in simulating the prominent features of Eocene climate, we make publicly available our data sets of Eocene topography, bathymetry, tidal dissipation, vegetation, aerosol distributions and river runoff. Major improvements in our boundary conditions over previous efforts include the implementation of the ANTscape palaeotopography of Antarctica, more accurate representations of the Drake Passage and Tasman Gateway, as well as an approximation of sub grid cell topographic variability. Our boundary conditions also include for the first time modelled estimates of Eocene aerosol distributions and tidal dissipation, both consistent with our palaeotopography and palaeobathymetry. The resolution of our data sets is unprecedented and will facilitate high resolution climate simulations. In light of the inherent uncertainties involved in reconstructing global boundary conditions for past time periods these data sets should be considered as one interpretation of the available data and users are encouraged to modify them according to their needs and interpretations. This paper marks the beginning of a process for reconstructing a set of accurate, open-access Eocene boundary conditions for use in climate models. Text Antarc* Antarctica Drake Passage Copernicus Publications: E-Journals Drake Passage Geoscientific Model Development 7 5 2077 2090
institution Open Polar
collection Copernicus Publications: E-Journals
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language English
description We describe a set of early Eocene (~ 55 Ma) climate model boundary conditions constructed in a self-consistent reference frame and incorporating recent data and methodologies. Given the growing need for uniform experimental design within the Eocene climate modelling community and the challenges faced in simulating the prominent features of Eocene climate, we make publicly available our data sets of Eocene topography, bathymetry, tidal dissipation, vegetation, aerosol distributions and river runoff. Major improvements in our boundary conditions over previous efforts include the implementation of the ANTscape palaeotopography of Antarctica, more accurate representations of the Drake Passage and Tasman Gateway, as well as an approximation of sub grid cell topographic variability. Our boundary conditions also include for the first time modelled estimates of Eocene aerosol distributions and tidal dissipation, both consistent with our palaeotopography and palaeobathymetry. The resolution of our data sets is unprecedented and will facilitate high resolution climate simulations. In light of the inherent uncertainties involved in reconstructing global boundary conditions for past time periods these data sets should be considered as one interpretation of the available data and users are encouraged to modify them according to their needs and interpretations. This paper marks the beginning of a process for reconstructing a set of accurate, open-access Eocene boundary conditions for use in climate models.
format Text
author Herold, N.
Buzan, J.
Seton, M.
Goldner, A.
Green, J. A. M.
Müller, R. D.
Markwick, P.
Huber, M.
spellingShingle Herold, N.
Buzan, J.
Seton, M.
Goldner, A.
Green, J. A. M.
Müller, R. D.
Markwick, P.
Huber, M.
A suite of early Eocene (~ 55 Ma) climate model boundary conditions
author_facet Herold, N.
Buzan, J.
Seton, M.
Goldner, A.
Green, J. A. M.
Müller, R. D.
Markwick, P.
Huber, M.
author_sort Herold, N.
title A suite of early Eocene (~ 55 Ma) climate model boundary conditions
title_short A suite of early Eocene (~ 55 Ma) climate model boundary conditions
title_full A suite of early Eocene (~ 55 Ma) climate model boundary conditions
title_fullStr A suite of early Eocene (~ 55 Ma) climate model boundary conditions
title_full_unstemmed A suite of early Eocene (~ 55 Ma) climate model boundary conditions
title_sort suite of early eocene (~ 55 ma) climate model boundary conditions
publishDate 2018
url https://doi.org/10.5194/gmd-7-2077-2014
https://gmd.copernicus.org/articles/7/2077/2014/
geographic Drake Passage
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Antarctica
Drake Passage
genre_facet Antarc*
Antarctica
Drake Passage
op_source eISSN: 1991-9603
op_relation doi:10.5194/gmd-7-2077-2014
https://gmd.copernicus.org/articles/7/2077/2014/
op_doi https://doi.org/10.5194/gmd-7-2077-2014
container_title Geoscientific Model Development
container_volume 7
container_issue 5
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