How can you explain the Chinook wind diagram clearly?

The Chinook wind diagram illustrates the process of warm, dry winds descending the leeward side of a mountain range. As moist air rises over the mountains, it cools, causing precipitation on the windward side. When the air descends on the leeward side, it compresses and warms rapidly, resulting in significantly higher temperatures. This phenomenon is often depicted with arrows showing airflow direction and temperature changes, highlighting the contrast between the moist windward side and the dry leeward side.