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Wednesday 03 Apr 2019The North Pacific pacemaker effect on historical ENSO and its mechanisms

Dillon Amaya -

H170 10:30-11:30

Recent studies have indicated that North Pacific sea surface temperature (SST) variability can significantly modulate the evolution of the El Niņo-Southern Oscillation (ENSO), but there has been little effort to put these extratropical-tropical interactions into the context of historical ENSO events. To quantify the role of the North Pacific in pacing the timing and magnitude of observed ENSO events, we use a fully-coupled climate model to produce the first ensemble of North Pacific Ocean-Global Atmosphere (nPOGA) SST pacemaker simulations. In nPOGA, SSTanomalies in the North Pacific (>15 ?N) are restored back to observations, but are free to evolvethroughout the rest of the globe. We find that North Pacific SST variability has significantly influenced the observed trajectory of historical ENSO, accounting for approximately 15% of the total variance in boreal fall and winter. The interaction between the North and tropical Pacific is the result of two physical pathways: 1. A Wind-Evaporation-SST propagating mechanism in boreal spring, and 2. A convective response associated with the Seasonal Footprinting Mechanism in boreal fall. The latter accounts for 25% of the observed zonal wind variability around the equatorial dateline. On an event-by-event basis, nPOGA most closely reproduces the 2014-2015 El Niņo and the 2015-2016 El Niņo. In particular, we show that the 2015 Pacific Meridional Mode event increased wind forcing along the equator by 20%, potentially contributing to the extreme nature of the 2015-2016 El Niņo. Our results illustrate the significant role of extratropical noise in pacing the initiation and magnitude of ENSO events and may improve the predictability of ENSO on seasonal timescales.

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