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   <subfield code="a">Global eastward propagation signals associated with the 4-5-year ENSO cycle</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[S.-Y. Simon Wang, Xianan Jiang, Boniface Fosu]</subfield>
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   <subfield code="a">Longitude-time evolution of sea surface temperature anomalies (SSTA) reveals a slow southeastward propagation from the western North Pacific (WNP) around 20°N to the Niño-3.4 region in the equatorial Central Pacific. The propagation is manifested as a narrow, southwest-northeast oriented SSTA band across the subtropical North Pacific, and its journey takes about 2-3years. The propagating SSTA appears to engage the initiation of the El Niño-Southern Oscillation (ENSO). The anomalies of surface winds, sea level pressure, outgoing longwave radiation, and velocity potential all exhibit a concurrent and distinct eastward propagation, one that appears to be circumglobaland is coupled with the predominant 4-5year frequency of the ENSO cycle. It is suggested that the previously found warming/cooling in the Indian Ocean induced by El Niño/La Niña, the progressive SSTA and wind anomalies across the Indian Ocean towards the WNP, and the predominant 4-5-year frequency of the North Pacific Oscillation collectively contribute to the reported SSTA propagation . The findings implicate that monitoring the SSTA propagation from the WNP towards the tropical central Pacific could be useful in tracking the ENSO development.</subfield>
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