OW1 data inout
| dc.contributor.org | Earth, Environmental, and Planetary Sciences | en_US |
| dc.creator | Seales, Johnny | en_US |
| dc.creator | Lenardic, Adrian | en_US |
| dc.date.accessioned | 2020-08-20T21:51:20Z | en_US |
| dc.date.available | 2020-08-20T21:51:20Z | en_US |
| dc.date.issued | 8/20/2020 | en_US |
| dc.description.abstract | The parameter inputs and data outputs provided herein were used to establish the hypothesis that changes in deep water cycling lead to a multi-stage cooling of the Earth. | en_US |
| dc.identifier.citation | Seales, Johnny and Lenardic, Adrian (2020): OW1 data inout. [Dataset]. Rice University. https://doi.org/10.25611/rryf-x193 | en_US |
| dc.identifier.doi | https://doi.org/10.25611/rryf-x193 | en_US |
| dc.identifier.uri | https://hdl.handle.net/1911/109245 | en_US |
| dc.language.iso | eng | en_US |
| dc.publisher | Rice University | en_US |
| dc.rights | This dataset is made available under the Creative Commons Attribution 4.0 International (CC BY 4.0) license. | en_US |
| dc.rights.uri | https://creativecommons.org/licenses/by/4.0/ | en_US |
| dc.title | OW1 data inout | en_US |
| dc.title.subtitle | Dataset | en_US |
| dc.type.dcmi | Dataset | en_US |