Constraining the North Atlantic circulation between 4.5°S and 39.5°N with transient tracer
[1] A1 ° horizontal resolution North Atlantic general circulation model (GCM) in the latitude band 4.5°S to 39.5°N is compared to, and then combined with, chlorofluorocarbon and tritium transient tracer data. The method of Lagrange multipliers (adjoint) is used. Tracer distribution within the model...
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.389.5052 http://ocean.mit.edu/~cwunsch/papersonline/liandwunsch2003.pdf |