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The monthly average tropical SST temperature anomaly dynamic could be adequately reproduced by only three factors - ENSO variability (Nino 3.4 index), volcanic aerosols in stratosphere and two climate shifts in 1925/1926 and 1987/1988 years.
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And according to our hypothesis there should be two upward shifts in somewhere in 1925/1926 and 1987/1988.