Air Masses and Fronts Chapter 16 section 2 S6E4.b – Relate unequal heating of land and water surfaces to form large global wind systems and weather. S6E4.c – Relate how moisture evaporating from the oceans affects the weather patterns and the weather events such as hurricanes. Air Masses Air mass – is a large body of air where temperature and moisture content are similar throughout. Moisture content and temp are determined by the area over which the air mass forms called source regions. Represented on maps by two-letter symbols; first letter – moisture content, second letter - temperature Cold Air Masses (3) Continental polar (cP)- air mass forms over northern Canada, brings extremely cold winter weather to the US, summer brings cool, dry weather. Cold Air Masses Maritime polar (mP) (Forms in 2 places) Forms over the North Pacific Ocean; cool and very wet, brings rain and snow to the Pacific Coast in winter, foggy weather in summer. Forms over the North Atlantic Ocean brings in cool, cloudy weather and precipitation to New England in the winter, cool weather in the summer. Warm Air Masses (4) Maritime tropical (mT) Develops over warm areas in the Pacific Ocean and Atlantic Ocean. Winter they bring mild, often cloudy weather. Summer, hot and humid weather, hurricanes, and thunderstorms. Warm Air Masses Continental tropical (cT) Forms over the deserts of northern Mexico and the southwestern United States; moves northward and brings clear , dry, and hot weather. Air Masses of North America Review 1. 2. What are the major air masses that influence the weather in the United States? What is one source region of a maritime polar air mass? 1. 2. Continental polar, maritime polar, maritime tropical, and continental tropical. The North Pacific and the North Atlantic Oceans. Review 3. Why does the Pacific Coast have cool, wet winters and warm, dry summers? 3. Cool, wet winters are affected by a maritime polar air mass. Summers are affected by a dry continental air mass.