In the 1990s, highly positive J / w values (more than +25 μmol kg −1 km −1 ) with an increasing trend were found for CW, and negative J / w values (less than −10 μmol kg −1 km −1 ) with a decreasing trend were found for DW, indicating increased (decreased) convective supply of DO to CW (DW).
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Re-initiation of bottom water formation in the East Sea (Japan Sea) in a warming world.
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