Abstract
Surface temperature gradients, used in identifying the principal hydrological fronts of the southwestern Atlantic Ocean, were computed from charts of ocean surface temperature plotted with the use of satellite information for the period 1988–1997. An analysis is made of the seasonal variability of ocean temperature gradients in the frontal zone, as well as changes in its geographical position. The year-to-year variability of the position of the Subantarctic Front is examined.
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