Oceanic tracer and proxy time scales revisited
Quantifying time-responses of the ocean to tracer input is important to the interpretation of paleodata from sediment cores – because surface-injected tracers do not instantaneously spread throughout the ocean. To obtain insights into the time response, a computationally efficient state-transition m...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2011-01-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/7/27/2011/cp-7-27-2011.pdf |