Declining silicate concentrations in the Norwegian and Barents Seas

    loading  Checking for direct PDF access through Ovid

Abstract

Since 1990, a decline in silicate concentrations together with increasing salinities has been observed in the Atlantic water of the Norwegian and Barents Seas. This decline in silicate has been found to be related to the relative proportion in which eastern and western source water masses from the northeastern North Atlantic enter the Norwegian Sea.

Related Topics

    loading  Loading Related Articles