| Gulf
Stream path analysis |
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| § | Isotherms
typical of Gulf Stream |
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| signature
at different depths are |
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| used
to obtain frontal location. |
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| § | Nearest
neighbor connected |
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| component theory is used to |
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| ascertain
to continuity of the front |
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| § | Frontal
location derived from |
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| every
3 day model output are |
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| averaged
to obtain mean frontal |
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| position |
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| Depth |
| Isotherm |
| 5m |
| 18 oC |
| 50m |
| 17 oC |
| 100m |
| 16 oC |
| 200m |
| 15 oC |
| 400m |
| 12 oC |