Final answer:
A maritime polar (mp) air mass that formed over the North Pacific Ocean would experience a decrease in moisture as it moved inland over the western coast of North America due to the rain shadow effect caused by the western mountain ranges.
Step-by-step explanation:
As a maritime polar (mp) air mass moves inland over the western coast of North America, it undergoes certain modifications in terms of moisture content. The air mass, which formed over the North Pacific Ocean, carries a significant amount of moisture due to its origin. However, as it encounters the western mountain ranges such as the Cascades and the Sierra Nevada, it experiences the rain shadow effect. This effect leads to the blocking of moisture and creates a semi-arid condition in the leeward side of the mountains, resulting in less precipitation.