Sunday marks the summer solstice in the Northern Hemisphere, the longest day of the year and the start of astronomical summer. This event occurs when the Earth’s tilt positions the Northern Hemisphere closest to the sun, resulting in the longest daylight hours. Conversely, the Southern Hemisphere experiences its shortest day, signaling the beginning of winter. The term “solstice” is derived from Latin, meaning the sun’s “pause” or “stop,” as it reaches its highest point in the sky before beginning its retreat, leading to shorter days until December. Throughout history, solstices have been celebrated with festivals and monuments like Stonehenge. The Earth’s orbit and tilt cause varying sunlight distribution, creating distinct seasons. While astronomical seasons are based on Earth’s position relative to the sun, meteorological seasons are defined by temperature cycles, starting on the first of March, June, September, and December.
QUESTION: How might understanding the science behind solstices and equinoxes change the way we perceive and celebrate these events?
