I have a little shadow that goes in and out with me,
And what can be the use of him is more than I can see....
- My Shadow, Robert Louis Stevenson

Me and My Shadow
- Mills Brothers


Does anybody really know what time it is?
Use a sundial to measure Solar Time. Use RealPlayer to hear the exact Standard Time from the US Naval Observatory Master Clock Voice Announcer.

Most days, Solar Time is slightly different from Standard Time (up to 16 min. fast or slow). This time difference is known as the Equation of Time.

Are You Clock-wise?
Ever wonder why is clockwise Clockwise? As it turns out, for objects in the Northern Hemisphere, shadows cast by the Sun move in a clockwise direction. In fact, the word hour means "the day" or "Sun's path." For details, see the How Sundials Work Web page.

Longitude is...
...equivalent to time, and vice versa. If you know the time difference between two locations, then you can use the rate of the Earth's rotation (15° per hour or 1° per 4 minutes) to calculate the difference in longitude between the two places.

For example, Solar Noon occurs eight minutes later in Wash., D.C. than it does on the Standard Time Meridian for the Eastern Time Zone (75°W); how many degrees of longitude separate the two locations?

8 min. x 1°/4 min. = 2°

Therefore, the longitude of Wash., D.C. is 77°W. Simple, huh? Well, it wasn't always so easy! Read The Illustrated Longitude, the story of clockmaker John Harrison, who solved the problem that Newton and Galileo failed to conquer--how to determine longitude at sea.

Long story short, sundials must be corrected for longitude (as well as the Equation of Time) so that Solar Time reads the same as Standard Time.

Did You Know...
...that Earth is eight light-minutes from the Sun? Huh? That's right. At the speed of light (186,000 miles per second, or 300,000 km/sec), it takes nearly eight minutes for sunlight to reach the Earth. The Earth is connected to the Sun, but it is a long-distance connection!

I'm Being Followed...
...by a moonshadow.
- Moonshadow, Cat Stevens

The Moon, especially the Full Moon, is bright enough to cast shadows at night. So, how bright does an astronomical object have to be to cast shadows? Good question! In fact, the question may be impossible to answer, since there are so many factors involved. However it is possible to quantify the brightness or magnitude of a light source. Oddly, negative magnitudes are brighter than positive ones. The Sky & Telescope magnitude Web page lists the following magnitudes for the Sun, Moon, brightest planet, and brightest star (in the night sky):

  • Sun = -26.7m
  • Full Moon = -12.5m
  • Venus = -4.4m
  • Sirius = -1.5m

"Night is a shadow world. The only shadows we see at night are cast by the moonlight, or by artificial light, but night itself is a shadow."
- Soul of the Sky, an essay by Diane Ackerman

The "Morning
Chorus"


During the pre-dawn twilight, have you ever noticed that birds wake up and sing all at once? Ornithologists call this phenomenon the "Morning Chorus." Plan to wake up early tomorrow to see the sunrise and listen to the symphony of nature--a delightful way to feel more connected to the natural world!

28 MAR 2002
Click here to access real-time sunspot imagery...
Today's sunspot
number is

179 /
Sunspot No. Trend
(past 24 hours)
/ Increasing
-- Steady
\ Decreasing

Credits: Real-time image courtesy SOHO; sunspot number courtesy NOAA.

Updated: 27 MAR 2002
ARCHIVES

Today's Predicted
UV Index is

5
Valid for Wash., DC during
the Solar Noon hour on

28 MAR 2002
UV Index courtesy NOAA.

Today's Observed
UV Index is

4.5
Sandburg Planetarium
28 MAR 2002, 01:00 p.m.
Sunny (Clear Skies)
(Sun Transit: 12:14 p.m.)

UV Index Solarmeter
courtesy EPA
SunWise School Program

Sandburg Center for Sky Awareness
A Fairfax County Public Schools Planetarium

Me and My Shadow
Making the Sun-Earth Connection

On a sunny day, drive a stake into the ground and observe how its shadow changes throughout the day or year--a simple yet profound way to demonstrate the interconnection between the Sun and Earth! The following Web resources may help you to more fully comprehend the deeper meaning of these simple observations.

The Analemma

    Ever notice the odd-looking figure eight that appears on many globes? It's called an analemma. See the analemma for Washington, D.C. (can you tell when the maximum altitude of the midday Sun occurs during the year?), then visit the Analemma Web site to learn more about, well, analemmas (including an explanation of how the analemma is derived from the stake you drove into the ground).

Sun Calculators

    Explore the daily and annual cycles of change in the apparent path of the Sun across the sky. Great Circle Studio's Solar Calculator will calculate the Sun's altitude and azimuth for a user-specified location, date & time, and data interval. A variety of output modes are available. Use this information to predict how the length of your shadow would change daily and annually (at the same time each day) by visiting the SCSA Shadow Length Calculator.

    How can you determine the height of objects too tall to measure directly? Using shadows, of course! Use the SCSA Object Height Calculator to calculate the height of tall shadow-casters, e.g., buildings, flagpoles, utility poles, trees, etc.

    The Solar Noon Calendar calculates tables showing either the exact time of Solar Noon for your location for each day of the year, or the Standard Time Correction (the amount you have to add to, or to subtract from, solar time on your sundial to get the time shown on your watch).

    The NASA J-Track Web page shows where the Sun is currently directly overhead (see small Sun icon, correctly oriented with respect to latitude and longitude).

You Can Make a Sundial!

Equatorial Sundials and the Equinoxes

    Although horizontal sundials are more familiar to most people, experience has shown that an equatorial sundial is better suited for making the connection between the Earth's rotation and solar time-keeping (see Are You Clock-wise? sidebar, left), as well as the connection between the Earth's revolution around the Sun and the annual cycle of change in the Sun's apparent path across the sky.

    Theoretically, the gnomon (or style) of a properly oriented equatorial sundial will not cast a shadow on the dial plate during the Equinoxes. Because the dial plate of an equatorial sundial is parallel to the Earth's Equator, the Sun is directly over the edge of the dial plate on the Equinoxes, when the Sun is at the zenith along the Equator. From the March Equinox to the September Equinox, when the Sun is at the zenith in the Northern Hemisphere (between 0° and 23.5°N lat.), the gnomon shadow falls on the upper dial face; from the September Equinox to the March Equinox, when the Sun is at the zenith in the Southern Hemisphere (between 0° and 23.5°S lat.), the gnomon shadow falls on the lower dial face.

    Put a little theory into practice--assemble a simple equatorial sundial (courtesy NASA Liftoff to Space Exploration) and empirically observe where the gnomon shadow falls as the seasons change. Gain valuable insight by checking the NASA J-Track Web page to see where the Sun is currently directly overhead (see small Sun icon, which is correctly oriented with respect to latitude and longitude).

    Editor's Note: From the March Equinox to the September Equinox, use the Northern Hemisphere equatorial sundial template. From the September Equinox to the March Equinox, use the Southern Hemisphere template. Be sure to fold the Southern Hemisphere template so that the dial face and gnomon point downward rather than upward (as directed).

Me and My Shadow - A Rule-of-Thumb for Safe Sun Exposure

    The Sun is a star that radiates energy at all wavelengths of the electromagnetic spectrum; some wavelengths of solar radiation are hazardous to plants and animals. Visit the EPA Stay Healthy in the Sun Web site for information about the health risks posed by ultraviolet (UV) radiation, as well as the steps people can take to protect themselves from overexposure to the Sun.

    An easy way to tell how much ultraviolet (UV) radiation exposure you are getting is to look for your shadow:

    • If your shadow is taller than you are (in the early morning and late afternoon), then your UV exposure is likely to be low.
    • If your shadow is shorter than you are (around midday), then you are being exposed to high levels of UV radiation. Seek shade and protect your skin and eyes.

    The Ultraviolet Index (UV Index) overview includes a link to EPA's new SunWise School Program regarding Sun safety. The National Oceanic and Atmospheric Administration (NOAA) produces a daily UV Index U.S. map (showing predicted exposure levels).

Light & Shadow - Suggested Activities for Grade K-6


Sunspots and the Solar Cycle

    What is "The Solar Cycle?" In a regular cycle, the Sun undergoes a period of great activity called the "solar maximum" (predicted to occur during 2000-2001), followed by a period of quiet called the "solar minimum." One way scientists track solar activity is by observing sunspots. Sunspots are relatively cool areas that appear as dark blemishes on the face of the Sun. During solar maximum there are many sunspots; during solar minimum there are few. See sidebar (left) for today's sunspot number.

    For more information about sunspots, Solar Maximum, and the Sun-Earth Connection, visit the SCSA Themes Web page. For classroom teachers, a couple of suggested sunspot-related activities...


Sun-Earth Day, Astronomy Week/Day, Sky Awareness Week, and Space Day


Sun-Earth-Moon Day 2001 | Sun "Block Party" 2000 | SCSA Home | www.wsanford.com