Areas on the windward side of mountain ranges can expect less precipitation due to the forced rising, expansion, and cooling of moving air masses. This statement is:

The statement is actually not accurate because areas on the windward side of mountain ranges typically receive more precipitation, not less. When moist air masses approach a mountain range, they are forced to rise. As the air rises, it expands and cools, leading to condensation of moisture and precipitation, which is why windward slopes are often lush and green.

Conversely, as this air descends on the leeward side, it warms and tends to dry out, resulting in less precipitation in those areas, commonly leading to what is known as a rain shadow effect. Thus, the correct understanding is that the windward side experiences higher precipitation due to the orographic lift, while the leeward side experiences decreased precipitation. This relationship between mountains and precipitation patterns is fundamental in environmental science and meteorology.