Jump to content

Tropical Solstice Shadows


NASA

Recommended Posts

  • Publishers
4 Min Read

Tropical Solstice Shadows

These views, captured from the Sun-facing side of Earth, show the change in Earth’s tilt between the December (left) and June (right) solstices. These images were taken by NASA’s Earth Polychromatic Imaging Camera on the National Oceanic and Atmospheric Administration’s DSCOVR satellite in December 2018 and June 2019.
June 20, 2024, marks the summer solstice — the beginning of astronomical summer — in the Northern Hemisphere.
Credits: NASA/DSCOVR EPIC

Solstices mark the changing of seasons, occur twice a year, and feature the year’s shortest and longest daylight hours – depending on your hemisphere. These extremes in the length of day and night make solstice days more noticeable to many observers than the subtle equality of day and night experienced during equinoxes. Solstices were some of our earliest astronomical observations, celebrated throughout history via many summer and winter celebrations.

Solstices occur twice yearly, and in 2024 they arrive on June 20 at 4:50 PM EDT (20:50 UTC), and December 21 at 4:19 AM EST (9:18 UTC). The June solstice marks the moment when the Sun is at its northernmost position in relation to Earth’s equator, and the December solstice marks its southernmost position. The summer solstice occurs on the day when the Sun reaches its highest point at solar noon for regions outside of the tropics, and those observers experience the longest amount of daylight for the year. Conversely, during the winter solstice, the Sun is at its lowest point at solar noon for the year and observers outside of the tropics experience the least amount of daylight- and the longest night – of the year.

The June solstice marks the beginning of summer for folks in the Northern Hemisphere and winter for Southern Hemisphere folks, and in December the opposite is true, as a result of the tilt of Earth’s axis of rotation. For example, this means that the Northern Hemisphere receives more direct light from the Sun than the Southern Hemisphere during the June solstice. Earth’s tilt is enough that northern polar regions experience 24-hour sunlight during the June solstice, while southern polar regions experience 24-hour night, deep in Earth’s shadow. That same tilt means that the Earth’s polar regions also experience a reversal of light and shadow half a year later in December, with 24 hours of night in the north and 24 hours of daylight in the south. Depending on how close you are to the poles, these extreme lighting conditions can last for many months, their duration deepening the closer you are to the poles.

A man squats on the ground surrounded by people, and only their legs are visible. He is pointing to a spot on a globe of the Earth which is propped above the ground on a small plastic stand. Shadows below everything in the picture are very small.
A presenter from the San Antonio Astronomy Club in Puerto Rico demonstrating some Earth-Sun geometry to a group during a “Zero Shadow Day” event.  As Puerto Rico lies a few degrees south of the Tropic of Cancer, their two zero shadow days arrive just a few weeks before and after the June solstice. Globes are a handy and practical way to help visualize solstices and equinoxes for large outdoor groups, especially outdoors during sunny days!
Credit: Juan Velázquez / San Antonio Astronomy Club

While solstice days are very noticeable to observers in mid to high latitudes, that’s not the case for observers in the tropics – areas of Earth found between the Tropic of Cancer and the Tropic of Capricorn. Instead, individuals experience two “zero shadow” days per year. These days, with the sun directly overhead at solar noon, objects cast a minimal shadow compared to the rest of the year. If you want to see your own shadow at that moment, you have to jump! The exact date for zero shadow days depends on latitude; observers on the Tropic of Cancer (23.5° north of the equator) experience a zero-shadow day on the June solstice, and observers on the Tropic of Capricorn (23.5° south of the equator) get their zero-shadow day on December’s solstice. Observers on the equator experience two zero shadow days, being exactly in between these two lines of latitude; equatorial zero shadow days fall on the March and September equinoxes.

There is some serious science that can be done by carefully observing solstice shadows. In approximately 200 BC, Eratosthenes is said to have observed sunlight shining straight down the shaft of a well during high noon on the solstice, near the modern-day Egyptian city of Aswan. Inspired, he compared measurements of solstice shadows between that location and measurements taken north, in the city of Alexandria. By calculating the difference in the lengths of these shadows, along with the distance between the two cities, Eratosthenes calculated a rough early estimate for the circumference of Earth – and also provided further evidence that the Earth is a sphere!

Are you having difficulty visualizing solstice lighting and geometry? You can build a Suntrack model that helps demonstrate the path the Sun takes through the sky during the seasons. You can find more fun activities and resources like this model on NASA’s Wavelength and Energy activity.

Originally posted by Dave Prosper: June 2022

Last Updated by Kat Troche: April 2024

Simplified Summary

The June solstice happens when the Sun is farthest north from the equator, and the December solstice is when it’s farthest south. During the June one, places outside the tropics have the longest day of the year, and during December’s, they have the shortest. In the Northern Hemisphere, June marks the start of summer, while in the Southern Hemisphere, it’s winter, and it’s the opposite in December. This happens because of the axis on which Earth leans. Because of this tilt, places near the North Pole have continuous daylight in June, while places near the South Pole have continuous darkness. In December, it’s the other way around. This goes on for months, depending on how close you are to the poles. People in the tropics, between the Tropic of Cancer and the Tropic of Capricorn, don’t see as big of a change in daylight. Instead, they have two days a year where shadows almost disappear because the Sun is directly overhead at noon. If you want to see your shadow, you have to jump! The exact days depend on where you are. Around 200 BC, Eratosthenes noticed the Sun was directly overhead on the solstice in one place, comparing that to another place where it wasn’t overhead, and was able to calculate Earth’s size and shape.

View the full article

Link to comment
Share on other sites

Join the conversation

You can post now and register later. If you have an account, sign in now to post with your account.
Note: Your post will require moderator approval before it will be visible.

Guest
Reply to this topic...

×   Pasted as rich text.   Paste as plain text instead

  Only 75 emoji are allowed.

×   Your link has been automatically embedded.   Display as a link instead

×   Your previous content has been restored.   Clear editor

×   You cannot paste images directly. Upload or insert images from URL.

  • Similar Topics

    • By European Space Agency
      Video: 00:00:10 Summer officially begins in the Northern Hemisphere today 20 June, marking the longest day of the year. The summer solstice, which is when the Sun reaches the most northerly point in the sky, is set to occur tonight at 21:50 BST/22:50 CEST.
      During the summer solstice, the Northern Hemisphere will experience the longest period of sunlight in a day or the longest day of the year. This is because of Earth’s position in orbit around the Sun and the way the North Pole is tilted towards the Sun during the solstice. 
      The Sun’s rays hit the Northern Hemisphere at their most direct angle, resulting in the most extended period of daylight. Despite the long hours of daylight, it may not necessarily be the hottest day of the year. 
      This animation shows one image per day captured by the Meteosat Second Generation from 20 June 2023 until 19 June 2024 captured at approximately 16:30 BST/17:30 CEST.
      Access the related broadcast quality video material.
      View the full article
    • By NASA
      Patrick Duran (SPoRT/ST11) participated in the annual Tropical Cyclone Operations and Research Forum (TCORF) at the NOAA Aircraft Operations Center in Lakeland, FL 3/5-6/24. TCORF brings together hurricane researchers, forecasters, and aircraft reconnaissance personnel from NOAA, the US Navy, and the US Air Force to discuss recent research results and plans for operational hurricane forecasting and aircraft reconnaissance during the upcoming hurricane season. The forum provided an opportunity to get initial stakeholder feedback from the hurricane aircraft reconnaissance community on real-time situational awareness products currently being developed by SPoRT. These products are designed to be used aboard an aircraft while it’s in the storm to make decisions on whether to modify the flight track and instrument deployments to accommodate a pre-planned research experiment called a “module.” Conversations at the forum also led to an enhanced collaboration with the NOAA Hurricane Research Division that will incorporate SPoRT into a module designed to perform cal/val for NASA’s TROPICS constellation. A new collaboration also was formed with NOAA’s Cooperative Institute for Research in the Atmosphere to better understand the Geostationary Lightning Mapper’s detection efficiency in the hurricane inner core.
      View the full article
    • By European Space Agency
      Tropical forests are clearly critical to Earth’s climate system, but understanding exactly how much carbon they absorb from the atmosphere, store and release is tricky to calculate, not least because measuring and reporting methods vary. With these measurements paramount for nations assessing the action they are taking to combat the climate crisis, new research shows how differences in estimates of carbon flux associated with human activity can be reconciled.
      View the full article
    • By NASA
      After the previous launch target date changed due to weather conditions in New Zealand, NASA and Rocket Lab are now targeting 9 p.m. EDT Sunday, May 7, (1 p.m. Monday, May 8, New Zealand Standard Time), to launch two storm tracking CubeSats into orbitView the full article
    • By NASA
      NASA and Rocket Lab are targeting 9 p.m. EDT, Sunday, April 30 (1 p.m. New Zealand Standard Time, Monday, May 1), to launch two storm tracking CubeSats into orbit.View the full article
  • Check out these Videos

×
×
  • Create New...