What Role Does the Barrier Layer Play During Extreme El Niño Events?

Intensive air‐sea interaction and the formation of the salinity barrier layer (BL) in the Pacific has fundamental importance to the El Niño evolution. The structure and formation of the BL in the equatorial Pacific Ocean during moderate and extreme El Niños over the past 30 years are investigated using in situ temperature and salinity data measured by the TAO/TRITON array and the data‐assimilating ECCO2 product. In the western and central Pacific Ocean, the BL is thicker during moderate El Niños compared to extreme El Niños due to a deeper isothermal layer depth compared to the density defined mixed layer depth. Moreover, in the western and central Pacific Ocean, the anomalous zonal eastward current related to the westerly wind event that initiates El Niños is found to be stronger during extreme El Niños, advecting the thicker BLs from west to east. A salinity budget suggests that during both moderate and extreme El Niño events, surface freshwater flux dominates at the equator. During extreme El Niños, the change in the freshwater flux drives a strong surface jet in the far western Pacific at 1°S, 156°E. North of the equator, the surface freshwater flux largely dampens this advective impact. Thus during the different El Niño strengths, the BL distribution, evolution and impact are also different. This suggests that climate models need to better distinguish different types of El Niño events in order to simulate the ENSO dynamics correctly. Plain Language Summary: During the different El Niño scenarios, the barrier layer (BL) distribution, evolution and impact are different. Observations from TAO/TRITON array shows that the BL is thicker during moderate El Niños than during extreme El Niños in the western and central Pacific Ocean. Less heat input leads to a thinner isothermal layer depth during extreme El Niños. Stronger anomalous zonal eastward current during extreme El Niños advects the thicker BLs from west to east, dampens thick BL maintaining in the western and central Pacific Ocean. During extreme El Niños, the diagnosis shows that the change in the freshwater flux further drives a strong eastward surface jet mainly through salinity effect in the far western Pacific, further advect the thick BL to the east. Climate models need to better distinguish the evolution of BL during different types of El Niño events. Key Points: Salinity stratified barrier layers (BLs) are thicker in the western Pacific Ocean during moderate El Niños compared to extreme El NiñosDifferences in the freshwater flux and advection are the main reasons for the discrepancies during the two types of El Niño eventsDuring extreme El Niños, the freshwater flux results in a salinity‐dominated zonal current anomaly advecting BLs eastward [ABSTRACT FROM AUTHOR]