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  • ...al depths of 4000 m or more. However, continents are typically surrounded by continental “shelf” above which the depth of the sea is typically 0-200 ...[Geostrophic flow]]). That is, transport across depth contours is enabled by (i) time scales of a day or less, or (ii) space scales of a few kilometres
    34 KB (5,146 words) - 22:11, 20 June 2024