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 statetransition ma...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Article |
| Language: | English |
| Published: |
European Geosciences Union / Copernicus,
2011-10-05T17:24:03Z.
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| Subjects: | |
| Online Access: | Get fulltext |