

FOLLOWUS
1. Institute of Oceanology Chinese Academy of Sciences
2. Key Laboratory of Ocean Circulation and Waves Chinese Academy of Sciences
网络首发:2012-11-15,
纸质出版:2012
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A time-dependent baroclinic model on NEC bifurcation[J]. 海洋湖沼学报(英文), 2012,30(1):186-191.
Wang, F., Hu, D. A time-dependent baroclinic model on NEC bifurcation., Chin. J. Ocean. Limnol. 30, 186–191 (2012). https://doi.org/10.1007/s00343-012-1213-9
A time-dependent baroclinic model on NEC bifurcation[J]. 海洋湖沼学报(英文), 2012,30(1):186-191. DOI: 10.1007/s00343-012-1213-9.
Wang, F., Hu, D. A time-dependent baroclinic model on NEC bifurcation., Chin. J. Ocean. Limnol. 30, 186–191 (2012). https://doi.org/10.1007/s00343-012-1213-9 DOI:
As it is well-known
the North Equatorial Current (NEC) bifurcates into the Kuroshio flowing northward and the equatorward Mindanao Current
which is well depicted by Munk’s theory in 1950 in terms of its climatology. However
Munk’s theory is unable to tell the NEC bifurcation variability with time. In the present paper
a time-dependent baroclinic model forced by wind
in which temporal and baroclinic terms are added to Munk’s equation
is proposed to examine the seasonal variability of the NEC bifurcation latitude. An analytical solution is obtained
with which the seasonal variability can be well described: NEC bifurcation reaches its northernmost position in December and its southernmost position in June with a range of about 1° in latitude
consistent with previous results with observations. The present solution will degenerate to Munk’s one in the case of steady and barotropic state.
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