An Advective Model of the Ocean Thermocline
نویسندگان
چکیده
منابع مشابه
Thermocline and Zonal Advective Feedbacks Within the Equatorial Ocean Recharge Oscillator Model for ENSO
Through the dynamical coupling between ocean and atmosphere, the vertical advection of anomalous subsurface temperature by the mean upwelling and the zonal advection of mean sea surface temperature (SST) by anomalous current constitute the so-called the thermocline and zonal advective feedbacks that are essential for El Nifio / Southern Oscillation (ENSO) coupled dynamics. In this paper, we dem...
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ژورنال
عنوان ژورنال: Tellus
سال: 1959
ISSN: 0040-2826,2153-3490
DOI: 10.3402/tellusa.v11i3.9316