Since gradients exists with every atmospheric phenomenon, including air pressure and SSTs, you can think of the ENSO ONI like the low pressure off of the east coast and the SSTS over the west PAC like the high pressure over the mid west...same type of system. Well, given that this is an el nino, the high ONI is analogous to a deep area of low pressure off of the east coast. But we would want to see lower SSTS over the west PAC to have a really strong SYSTEM, just like we would a strong high pressure over the mid west. But this year, we have a weak high (warm W PAC SSTS), so the gradient isn't there. Its like having the impressive 961mb low (ONI) with a paltry 1000mb high.