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Relationship between sea level and climate forcing by CO(2) on geological timescales
On 10(3)- to 10(6)-year timescales, global sea level is determined largely by the volume of ice stored on land, which in turn largely reflects the thermal state of the Earth system. Here we use observations from five well-studied time slices covering the last 40 My to identify a well-defined and cle...
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| Hlavní autoři: | , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
National Academy of Sciences
2013
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3557064/ https://ncbi.nlm.nih.gov/pubmed/23292932 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1216073110 |
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