Letter from Stephanie: Day & Night Cycles
Dear Fellow Explorers,
I've never wintered over in Antarctica, when it is dark all of the time. I work in the Antarctic summer, between January and March, when there is plenty of daylight–twenty-four hours a day! That's right, in September, the Sun rises, and then doesn't set again until March.
With that much daylight, we can work pretty much all the time, and we want to work as much as we can. It's not just that we love our work, though we certainly do; we only get into the field for a short time each year, so we want to make the most of it. We run shifts around the clock, each of us working for eight to twelve hours; it doesn't matter which shift each of us gets, because it is always light outside. We sleep less in Antarctica than we usually do–the constant sunlight can make sleeping difficult, and most members of the team work longer hours than they would at home. But we have developed a few tricks to help us sleep–we can cover our portholes with aluminum foil, wear sleep "goggles" or bury ourselves in the blankets!
Unless you live at one of the poles, you probably don't have to take such drastic measures to get to sleep at night; most places on Earth experience daily changes in light, with a period of dark followed by a period of light every day. Why then does Antarctica have six whole months of darkness in the winter and six whole months of lightness in the summer?
In most places on Earth, there are daily changes in light–light all day and darkness all night. These daily changes occur because Earth rotates on its axis, spinning once around in roughly twenty-four hours–slow enough so that we don't get dizzy. For part of that time, the period we call daytime, a given place on Earth, such as your town, faces the Sun. For the remainder of the twenty-four-hour rotation, the period we call nighttime, Earth has turned, and that same area is on the side of Earth facing away from the Sun.
So why do we have changes in daylight over the course of the year?
You've probably noticed that these annual changes in light patterns are tied to the seasons, with a longer daytime period in the summer and a shorter daytime period in the winter. To figure out how daylight is connected to seasons, then, we have to first consider how seasons work.
There are two reasons that we have seasons.
- First, Earth's axis is tilted.
- Second, Earth revolves around the Sun once every 365 days.
Our Earth follows an elliptical path on its journey around the Sun. An ellipse is a slightly flattened circle; this means that there are two extreme points on the orbit, one closest to the Sun and one farthest. (The perihelion is the point where the Earth is closest to the Sun; the aphelion is the point where the Earth is farthest from the Sun.)
You might think seasons are caused by Earth's changing distance from the Sun, with the closest, hottest point being summer and the farthest, coldest being winter. Not so! In fact, winter in the Northern Hemisphere occurs at the perihelion, when the Earth is closest to the Sun.
It's not the Earth's distance from the Sun that causes seasons, then. So what does?
The actual reason for seasons has to do with the tilted angle of the Earth's axis. No matter how close or far the Earth is to the Sun, it always maintains the same angle on its axis; in other words, it's always tilted the same way. This means that for part of the path around the Sun, the Southern Hemisphere is tilted toward the Sun, and for part of the path, it is tilted away from the Sun. When it is tilted toward the Sun, the Southern Hemisphere receives a greater amount of sunlight; this occurs in the Antarctic summer. When it is tilted away from the Sun, the Southern Hemisphere receives less sunlight; this occurs in the Antarctic winter.
The seasons occur at opposite times in the hemispheres; when the Southern Hemisphere is tilted toward the Sun, the Northern Hemisphere has to be tilted away from the Sun. Antarctica, in the very bottom of the Southern Hemisphere, gets more sunlight and warmth, experiencing summer, when the North Pole is receiving less light and warmth and experiencing winter. Eventually (about six months later), the North Pole is exposed to the incoming light and warmth of summer, and the South Pole is in the darkness of winter. The amount of sunlight recevied, then, creates the season; an area of the globe is experiencing summer when it is receiving more sunlight for longer periods.
This is all very nice, you might be saying.... but WHY does Antarctica have such extremely long periods of light and dark?! Why does the Sun rise only once when the Antarctica summer begins and then set only once when the Antarctica winter begins? Why does the summer day and winter night last for almost six months each?
Look again at the drawings of the seasons. During the Southern Hemisphere summer, the Earth is tilted in a way that exposes most of the Southern polar region to the sun's rays all the time. Even though Earth is rotating daily on its axis, the bottom of the Earth is always tilted toward the Sun. Six months later, at the other end of Earth's yearly revolution around the Sun, the tilt of the Earth's axis causes the Southern Hemisphere to tilt away from the Sun all the time. Now, even though the Earth is rotating daily on its axis, the bottom of the Earth is always tilted away from the Sun. At this time, the South Pole gets no sunlight, while the North Pole soaks up twenty-four hours a day of sunlight.
At latitudes greater than 66º33', the position of the Arctic and Antarctic circles on our globe, days of constant darkness or light can occur. (The South Pole is at 90ºS.) Much of Antarctica lies between 66º33' and 90ºS. As you get farther from the Pole, there are increasing (but still very short) periods of sunlight during winter and darkness during summer. Only the Antarctic Peninsula, sticking out north of ~66ºS, does not experience twenty-four-hour days in summer or twenty-four-hour nights in winter. (This might help explain why flowering plants are found only on the Peninsula.) But even at the Peninsula, the lengths of summer days and winter nights are vastly exaggerated compared to what most of us experience at home in lower latitudes.
Well, time for me to go back on watch. The air is cold, the seas are calm, and the Sun is bright–and it's almost midnight! Looks like it will be a pleasant work day!
More About This Resource...
This online letter is part of a series written by a glacial geologist working in Antarctica. In her "letters home," Stephanie Shipp shares her work and discoveries. Specifically, this letter discusses:
- how the Sun never sets in Antarctica during the summer months, January to March, the time when Shipp does her field research,
- why the Earth's tilted axis and the planet's orbit around the Sun create our seasons, and
- how Antarctica's location creates 24-hour-long periods of light and dark.
Less than 1 period
Supplement a study of Antarctica or astronomy with an activity drawn from this essay about day and night cycles.
- Ask students if they know why the Sun never sets during Antarctica's summer or rises during its winter.
- Send students to this online article, or print copies of the essay for them to read.
- Have them write a one-page reaction to the article, comparing their original answers to what they learned in the essay.