Other
Scientific paper
Aug 2003
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30ooce1i&link_type=abstract
Geophysical Research Letters, Volume 30, Issue 15, pp. OCE 1-1, CiteID 1794, DOI 10.1029/2003GL017652
Other
5
Oceanography: Physical: Eddies And Mesoscale Processes, Oceanography: Physical: Western Boundary Currents, Oceanography: Physical: Sea Level Variations
Scientific paper
It has been reported that several eddies frequently exist along the Kuril-Kamchatka Trench (K-K Trench, hereafter), the western boundary of the subarctic North Pacific. Lagged correlation maps of the altimeter-derived sea level anomalies (SLAs) along the trench indicate that the southern eddies on the whole move northeastward along the K-K Trench and the northern eddies, on the other hand, move southwestward. By tracking each anticyclonic eddy, its propagating velocity along the trench is calculated. The time series of the tracked 7 eddies shows similar seasonal variation to those of the first empirical orthogonal function (EOF) of the SLA maps and to those of the Sverdrup transport at 40°N. In addition, when more than two eddies remotely exist in the studied area, they show coherent moving patterns. These results suggest that the eddies in the western boundary region of the subarctic North Pacific are advected by the time-dependent wind-driven current.
Isoguchi Osamu
Kawamura Hiroshi
No associations
LandOfFree
Eddies advected by time-dependent Sverdrup circulation in the western boundary of the subarctic North Pacific does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Eddies advected by time-dependent Sverdrup circulation in the western boundary of the subarctic North Pacific, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Eddies advected by time-dependent Sverdrup circulation in the western boundary of the subarctic North Pacific will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1669703