wind stress curl changes is a delayed process and would retard the existing cyclonic circulation. We would expect this influence to manifest itself with large reversals in PC1 of the geostrophic velocity like the variations in the curl PC1 or NAO with a 3- to 5-year delay. Figure 5C shows that there...
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.69.3434 http://ni.cs.tu-berlin.de/journalclub/papers/IkegayaYuste_2004_Science.pdf |