East Antarctic cooling induced by decadal changes in Madden-Julian oscillation during austral summer.

RESULTS Changes in Antarctic SAT during austral summer Over the recent three decades of 1979–2014, the DJF mean SAT showed a profound decreasing trend at most of the stations along the East Antarctic coast (30°W to 150°E), in contrast with an increasing trend at some stations on the western coast of Antarctica ( Fig. 1A ).

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