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- W2249667022 abstract "The complex thermohaline structure observed in the Western Mediterranean after the severe winter of 2004-05 is still present in the summer of 2009 at the Balearic Islands. The processes that caused the anomaly are now well identified, as well as the different newly formed water masses. The evolution of the anomaly during the period involves a progressive homogenization of the deep waters masking the layered structure. The final product is a warmer and saltier water type that apparently has incorporated deep waters formed in subsequent winters but not from other intense cascading episodes. On the other hand, Levantine Intermediate waters observed at the north of the Balearic Channels does not present robust trends since mid-90`s." @default.
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- W2249667022 date "2010-01-01" @default.
- W2249667022 modified "2023-09-23" @default.
- W2249667022 title "Evolution of the Western Mediterranean thermohaline Anomaly as observed nearby Balearic Islands (2005-2009)" @default.
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