IPA: /ˈtrəʊpəˌpɔːz/
KK: /trəˈpəʊpɔːs/
The boundary layer in the atmosphere that separates the troposphere from the stratosphere, with its height changing based on location, being lower at the poles and higher at the equator.
The weather patterns are influenced by the conditions at the tropopause.
Tropopause → It is formed from "tropo-" (from Greek "tropos", meaning turn or change) and "pause" (from Latin "pausa", meaning a stop or break). The word refers to the boundary layer in the atmosphere where the temperature stops decreasing with altitude, marking a change in the atmospheric conditions.
Think of 'tropo-' meaning a 'change' in the atmosphere and 'pause' indicating a 'stop' — the tropopause is where the temperature change stops.
No commonly confused words.