1. Composition of the Earth's Atmosphere
... differences in air's density. There are more molecules of air above a point of having high pressure than above on where low pressure is observed. Warm air is less dense than cool air, because the air molecules are farther apart. Because temperature and altitude determine air pressure, air pressure readings are useful in predicting weather and wind changes, and in estimating altitudes ... the water is now warmer than the air in the land. The warmer air rises, and the cooler air moves off the shore to take its place. This flow of cool air from land to water is called a land breeze. WEATHE...
- Word Count: 3528
- Approx Pages: 14
- Grade Level: High School