Top 5 Cosmic Myths
Tue Sep 3, 9:16 AM ET
By Philip Plait, SPACE.com
How much astronomy do you know? I mean, really know. Completely,
self-assuredly, bet-your-bottom-dollar, 100 percent absolutely certain you
know.
Hmmm.wanna bet? On these pages are five astronomy misconceptions that are so
common they're almost canonical. Is one of these lurking in your brain? I
bet at least one is.
Let's find out how much you know that you think you know, but really don't
know.

1 There is no gravity in space
We've all seen videos of astronauts floating weightlessly above the Earth,
and of course you've heard the expression "zero-g." But that's a misnomer.
Gravity gets weaker with distance (in fact, with the square of the
distance), but it never falls all the way to zero. In point of fact, gravity
goes on essentially forever.
You cannot "escape the bounds of gravity" anymore than you can escape the
grasp of the IRS.
Astronauts look like they are experiencing no gravity because they are
orbiting the Earth. What they are really feeling is freefall, since they are
in reality "falling" around the Earth. In effect, they are falling toward
the Earth, but moving sideways enough to continuously miss it. The net
result is they follow the curvature of the Earth, always falling but never
hitting.
At the typical shuttle orbital height of 250 miles (400 kilometers) off the
Earth's surface, the force of gravity is roughly 90 percent what it is here
on the surface. Gravity is still very much in control of the shuttle's (and
astronauts') motion. Inevitably, when they land, they return to its full
effects.
Some things even astronauts cannot escape. They even have to pay their taxes
too.
Next Page: Big Moon Rising

2 The Moon looks bigger on the horizon because the air acts like a lens,
magnifying it

When on the horizon, the Moon appears huge and flat from space, too.
Almost everyone has seen the Moon, red and swollen, looming hugely as it
rises over the horizon. A few hours later, when it's high in the sky, it has
shrunk considerably, looking more "normal." Most people are also aware the
Sun exhibits this behavior, and even constellations do, too.
It's true that the Earth's air is thicker near the horizon. When you look
up, you are looking through the thinnest part of the atmosphere, and the
closer you look toward the horizon, the more air you look through.
However, the air actually compresses the Moon's image, instead of magnifying
it. Have you noticed that the Moon looks noticeably squashed when it's right
on the horizon? That's because the varying thickness of the air near the
horizon distorts the Moon's shape, making it smaller top-to-bottom.
It turns out this effect of the Moon looking larger near the horizon, called
the Moon Illusion, really is an illusion. You can see this for yourself, by
comparing the rising Moon's size with some household object (say, the tip of
a pencil eraser held at arm's length), and then wait a few hours and do it
again. You'll find the size hasn't changed appreciably.
This illusion is convincing, but it's not real.
What's going on here is that your brain is interpreting the sky as being
farther away near the horizon, and closer near the zenith (directly
overhead). This isn't surprising; look at the sky on a cloudy day and the
clouds overhead may be a few kilometers above you, but near the horizon they
might be hundreds of kilometers away. The Moon, when it's on the horizon, is
interpreted by your brain as being farther away. Since it's the same
apparent size as when it's high up, your brain figures it must be physically
bigger. Otherwise, the distance would make it look smaller.
This effect is the well-known Ponzo Illusion. Recent tests have shown pretty
conclusively that this is indeed the cause of the Moon Illusion.
By the way, when it's on the horizon, the Moon is actually a few thousand
miles (kilometers) farther away than when it's overhead. So in reality, it's
actually a bit smaller when it's on the horizon! Our brains may be smart,
but they are very easily fooled.
Next Page: Seasons and the Sun

3 Seasons are caused by the Earth's distance from the Sun
On a cold winter's evening, you can huddle near a fire for warmth. If you
get too close it can burn you, and if you are too far away it can hardly
warm you at all. Clearly, the amount of warmth you get from something hot
depends on its distance.
And hey, the Earth's orbit is an ellipse! So sometimes it's closer to the
Sun, sometimes farther away. This must be why we have seasons, right?
Wrong. If you do the math, you'll find that the Earth should only be a few
degrees warmer when it is at perihelion (closest to the Sun) than when it's
at aphelion (farthest from the Sun). Yet the difference between summer and
winter in most locations is a lot more than just a few degrees.
Even worse, when it's summer in the Northern Hemisphere, it's winter in the
south, and vice-versa. So clearly it can't be the distance to the Sun that
makes the difference.
The real reason for the seasons is the tilt of the Earth. Ever notice that a
globe of the Earth is always tilted? That's because the Earth's spin axis
(the line connecting the north and south poles) is tilted to the plane of
the Earth's orbit around the Sun. The amount of the tilt is about 23.5
degrees.
In the summer, the Earth's axis is pointed toward the Sun (well, not exactly
at the Sun, but in that direction). When that happens, the Sun gets higher
in the sky. Its light is more concentrated, and it heats the ground more
efficiently. Also, days are longer, giving it more time to heat things up.
Summers are hot.
In the winter, when the Earth's axis is directed away from the Sun, the Sun
is lower in the sky. The light hits the ground slanted, spreading it out.
That makes it heat things a lot less efficiently. Days are also shorter,
giving it less time to heat things up. Winters are cold.
That's why the opposite hemispheres have opposite seasons, too. When the
Northern Hemisphere of the Earth is tipped toward the Sun, the southern one
is tipped away, and vice-versa.
Sometimes, good science just depends on your slant on things.
Next Page: Rubbed the Wrong Way

4 Meteors are heated by friction as they pass through the atmosphere
This one makes sense, which is why it's so pernicious. But it's still wrong.
Meteoroids are tiny bits of dust, rock, ice or metal that have the
unfortunate luck of having their orbits intersect the Earth's. When they
pass through our atmosphere, they are heated so ferociously that they glow
(and at this point are called meteors), and are visible for hundreds of
miles.
However, it is not friction that heats them. Think of it this way: a space
shuttle's tiles are extremely delicate; they crumble easily in your hand. If
they were heated by friction as the shuttle de-orbits and enters the
atmosphere at Mach 25, the tiles would disintegrate. That's not a very good
design characteristic.
In reality, it isn't friction, but ram pressure that heats the meteoroid.
When a gas is compressed it gets hot, like when a bicycle pump is vigorously
used to inflate a tire. A meteoroid, moving at 33,500 mph (15 kilometers a
second) or more compresses the air in front of it violently. The air itself
gets very hot, which is what heats the meteoroid. That's the fact, not
friction.
Next Page: More on this Hot Topic

5 Meteors are still very hot when they hit the ground

You'd expect that something heated up so much that it glows would still be
hot a couple of minutes later. Actually, the situation is a bit more
complicated.
The super-hot air in front of the meteoroid is not actually in contact with
the particle. (A particle can still be referred to as a meteoroid as it
races through the atmosphere, while "meteor" is meant to describe the whole
glowing phenomenon.)
The meteoroid's quick motion sets up a shock wave in the air, like from a
supersonic airplane. The shocked air sits in front of the meteoroid, a few
centimeters away (depending on the meteoroid's size) in what's called a
standoff shock. Between the shocked air and the surface of the meteoroid is
a relatively slow-moving pocket of air.
The surface of the meteoroid melts from the heat of the compressed gas in
front of it, and the air flowing over it blows off the melted portion in a
process called ablation. The meteoroid's high velocity provides the energy
for all this heat and light, which rob it of speed. When it falls below the
speed of sound, the shock wave vanishes, the heating and ablation stop, and
the meteoroid then falls rather slowly, perhaps at a couple of hundred mph
(or a few hundred kilometers per hour).
It's still pretty high up in the atmosphere at this point, and takes several
minutes to fall to the ground. Remember, this tiny bit of rock spent a long
time in space, and the core is pretty cold. Also, the hottest parts were
melted and blown off. Even more, the air up there is cold, which chills the
rock as well.
All of these things together mean that not only is the rock not hot when it
hits the ground, it can actually be very cold. Some meteorites (what a
meteoroid is called after it impacts) have actually been found covered in
frost!


Philip Plait is the author of "Bad Astronomy" (Wiley & Sons, 2002). For more
about these and other astronomy misconceptions, you can buy his book or
visit his Bad Astronomy website.



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