fv7 - solar radiation
AP Environmental Science: Unit 4 – Earth Systems & Resources
Topic: 4.7 Solar Radiation and Earth's Seasons
Main Source of Energy
Solar Radiation
The sun is the primary energy source for Earth.
Affects seasonal changes in light and temperature.
Seasonal Changes
Length of Daylight
Varies with seasons; longer days in summer, shorter in winter.
Sun's Angle
In winter, the sun's angle is less favorable, resulting in longer nights and less solar radiation.
In summer, the sun's angle is more direct, leading to shorter nights and more solar radiation.
Latitude's Role
Solar Radiation Reception
At the equator (0° latitude), solar radiation hits directly, resulting in higher intensity.
Higher and lower latitudes experience curvature, spreading solar radiation over a larger area, leading to lower intensity.
Earth's Tilt and Orbit
Seasons and Temperature
Earth's tilt towards the sun results in longer days and higher temperatures.
Tilt away from the sun leads to longer nights and cooler temperatures.
Equinoxes
Occur during spring and fall when the tilt changes, marking transitions between seasons.
Day and night lengths are approximately equal.
Key Terms
Biomes
Large ecological communities with distinct climate, vegetation, and animal species.
Equinoxes
Two points in Earth's orbit when day and night are nearly equal, marking the start of spring and autumn.
Solstices
Points in the year when the sun reaches its highest or lowest point, resulting in the longest and shortest days.
Summer Solstice: Around June 21, marks the start of summer.
Winter Solstice: Around December 21, marks the start of winter.
Effects of Earth's Curvature
Distribution of Solar Radiation
Solar radiation is not evenly distributed due to Earth's curvature.
Lower latitudes receive more intense solar radiation.
Higher latitudes receive less intense solar radiation due to the oblique angle of sunlight.
Summary
Understanding solar radiation and its effects on Earth's seasons is crucial for comprehending climate patterns and ecological systems. The interplay between Earth's tilt, orbit, and latitude significantly influences temperature and daylight variations throughout