Water has a high specific heat capacity, meaning it absorbs and releases heat slowly. Coastal areas have milder climates than inland areas at the same latitude: cooler summers, warmer winters, and less temperature variation. San Francisco is much cooler in summer than St. Louis at the same latitude because of the Pacific Ocean. Ocean currents also redistribute heat: the Gulf Stream carries warm water to Western Europe, keeping the U.K. and France much warmer than equivalent latitudes in Canada.
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Lesson PreviewLesson 8 of 9 in this unit
4.8 Earth’s Geography and Climate
Part of Earth Systems and Resources in AP® Environmental Science. Read the opening section, then create a free account for the full interactive lesson, practice, and progress tracking.
In this unit
9 lessons
- 4.1Plate TectonicsPreview lesson
- 4.2Soil Formation and ErosionPreview lesson
- 4.3Soil Composition and PropertiesPreview lesson
- 4.4Earth’s AtmospherePreview lesson
- 4.5Global Wind PatternsPreview lesson
- 4.6WatershedsPreview lesson
- 4.7Solar Radiation and Earth’s SeasonsPreview lesson
- 4.8Earth’s Geography and ClimateThis lesson
- 4.9El Niño and La NiñaPreview lesson
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