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In terms of observational analysis and numerical simulations,study is performed of thesynergistic effects of the tropical Indian Ocean and Pacific SSTA on the atmosphere in northern win-ter.It turns out that the SSTA features show in-phase variation for the Indian Ocean and the central/eastern Pacific at low latitudes and anti-phase change compared with that in the neighborhood of thewestern Pacific“warming pool”.When negative SSTA in the western Pacific and positive SSTA inthe central/eastern Pacific and the Indian Ocean are available,the 500 hPa height anomaly exhibits awave train of a positive-negative-positive anomaly following a great-circle path emanating from thesubtropical western Pacific via the NW portion to North America,with enhanced westerly jet overmidlatitude East Asia and the NW Pacific,and v.v.The comparison to the results from the numeri-cal modeling of the tropical western Pacific SSTA reveals the importance of the synergistic effects ofthe oceans on atmospheric circulations.
In terms of observational analysis and numerical simulations, study is performed of thesynergistic effects of the tropical Indian Ocean and Pacific SSTA on the atmosphere in northern win-ter. Turn turns that the SSTA features show in-phase variation for the Indian Ocean and the central / eastern Pacific at low latitudes and anti-phase change compared with that in the neighborhood of the western Pacific “warming pool” .When negative SSTA in the western Pacific and positive SSTA inthe central / eastern Pacific and the Indian Ocean are available, the 500 hPa height anomaly exhibits awave train of a positive-negative-positive anomaly following a great-circle path emanating from the western western Pacific via the NW portion to North America, with enhanced westerly jet overmidlatitude East Asia and the NW Pacific, and vvThe comparison to the results from the numeri-cal modeling of the tropical western Pacific SSTA reveals the importance of the synergistic effects of the oceans on atmospheric circulations.