Why Our Days Are Getting Longer: Understanding Earth's Tilt and Daylight Changes
WFAAJanuary 15, 20261 min300 views
1 connectionsΒ·2 entities in this videoβThe Science Behind Longer Days
- π The primary reason for longer days and later sunsets is Earth's axial tilt.
- π‘ Since the winter solstice, which occurred just over three weeks ago, the Northern Hemisphere has been tilting away from the sun, resulting in shorter days.
- π As we move away from the solstice, the tilt gradually shifts, causing the days to become progressively longer.
Changes in Sunrise and Sunset Times
- π Sunset times are noticeably later now; for example, a sunset that was at 5:23 PM a month ago is now at 5:43 PM.
- π In one month, the sunset will be around 6:07 PM, indicating a significant increase in evening daylight.
- βοΈ While sunrises are still getting slightly later (e.g., from 7:31 AM to 7:22 AM), they will soon start to occur earlier, with a projected sunrise of 7:15 AM in a month.
Earth's Tilt and Seasonal Changes
- π§ The Earth's tilt is not constant; it changes throughout the year, influencing daylight hours and the apparent position of the sun.
- β‘οΈ During winter, the Northern Hemisphere tilts away from the sun, leading to less daylight and sunrises appearing more from the northeast.
- βοΈ As we approach the vernal equinox, the tilt becomes more diagonal, and sunrises will shift to appear more out of the southeast, moving easterly.
Future Daylight Gains
- β³ We are currently gaining daylight rapidly each day.
- π In the next month, we can expect to gain an additional 45 to 50 minutes of daylight, making the days feel significantly longer.
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Whatβs Discussed
Earth's TiltWinter SolsticeVernal EquinoxSunrise TimesSunset TimesDaylight HoursNorthern HemisphereSeasonsAxial Tilt
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