Answer:
The tropical western pacific ocean regions experience lower sea levels during strong enso events.
Step-by-step explanation:
El Niño–Southern Oscillation (ENSO) is an intermittently periodical change in drafts and sea surface temperatures across the tropical eastern Pacific Ocean, altering the climate of many of the tropics and subtropics. The warming state of the sea temperature is identified as El Niño and the cooling stage as La Niña.