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- W2051176175 abstract "Abstract In the past three decades, the strongest central Pacific (CP) El Nino event was observed in 2009–2010 by satellites. When intensity of this CP El Nino reached its maximum, large diurnal variations of sea surface temperature (SST) were also observed from tropical atmosphere ocean moorings in the central equatorial Pacific. Solar radiation in the equatorial central Pacific is larger than 140 W/m 2 , which leads to the amplitude of diurnal cycle of SST primarily determined by large-scale wind patterns. Intraseasonal westerly wind events (WWEs) can lead to an eastward displacement of the warm pool and also can weaken the trade winds in central Pacific. When the occurrence of equatorial WWEs is more than 20 days in a month, monthly mean wind speed in central equatorial Pacific has high possibility of wind speed less than 3 m/s, thus has pronounced diurnal cycle of SST. The diurnal cycle of SST will rectify daily mean SST. Reduced mixing at the base of the mixed layer and suppression of entrainment due to the accumulated effect of diurnal cycle may lead to warmer SST in the following month. This study suggests the occurrence of more diurnal SST events may contribute to the increasing intensity of the CP El Nino events." @default.
- W2051176175 created "2016-06-24" @default.
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- W2051176175 date "2013-09-01" @default.
- W2051176175 modified "2023-10-17" @default.
- W2051176175 title "Westerly wind events, diurnal cycle and central Pacific El Niño warming" @default.
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- W2051176175 doi "https://doi.org/10.1016/j.dynatmoce.2013.04.002" @default.
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