Explain how latitude, elevation, and distance from the ocean combine to create different climate zones, using California's own varied climates as a case study.
A region's climate is shaped by several factors working together, not just one. Latitude sets the baseline, regions near the equator receive more direct, concentrated sunlight year-round, while regions near the poles receive weaker, more slanted sunlight, but elevation and distance from the ocean matter enormously too. Higher elevations are cooler because the atmosphere is thinner and holds less heat, and places near an ocean tend to have milder, more moderate temperatures than places deep inland, because water heats and cools much more slowly than land.
California is an unusually good place to see all of these factors at once. The coast has a mild, Mediterranean climate moderated by the nearby Pacific Ocean and the cool California Current; the Central Valley, farther from the ocean's moderating effect, has hot, dry summers; the Sierra Nevada mountains are cool and often snowy because of elevation; and the Mojave Desert, blocked from ocean moisture by mountains creating a rain shadow, is hot and extremely dry. One state, four very different climate zones, all explained by the same handful of factors.
Mastery looks like: They can name latitude, elevation, and distance from the ocean as climate factors and explain how each one shapes a specific California region's climate.
Common stumbles: Assuming latitude alone determines climate; not connecting a rain shadow to the mountain that causes it.