It’s here, it’s there! In the car. Under the china cabinet. On book shelves—and books. Curled into dust bunnies in closet corners. Where on earth does all that dust come from? Short answer? Nearly everywhere!
Wherever it comes from, dust is fine particles of solid matter, heavy enough to see and light enough to be carried by the wind.
What Makes Dust?
Tiny fragments of human skin account for 20-50% of household dust! People are generally aware of dry skin on the scalp and body. Now you know: it doesn’t just disappear! If you sleep on flannel sheets, your bed might look like you have full-body dandruff. (Told to me by a friend!)
Pets also shed skin cells. People who are allergic to cats, dogs, guinea pigs or whatever, are allergic to that pet’s dander. Personally, I have a major anaphylactic response (throat swelling, unable to breathe) to guinea pig dander—even to a room where a guinea pig has been! In Peru, guinea pig meat is a traditional and major source of protein. It turns out, I can eat guinea pig, I just can’t be around them.
Hair is usually seen in strands, but can disintegrate into dust, too.
Dangerous Dust
Smoke and ash often go together. You smell smoke because of the particles coming in contact with your nasal membranes. And as you all know, excessive exposure to smoke or ash can be deadly. But don’t forget volcanic ash!
Those spring days when your vehicle seems to have been powdered in yellow, you can see pollen dust. But even when you can’t see it, airborne pollen can adversely affect breathing.
Bacteria are dust? Yep. Or at least they are in dust. The most common ones are staphylococcus and streptococcus, both common on human skin and relatively prevalent in our everyday lives.
Dust that is small bits of dirt or rock are hazardous to one’s lungs with long or repeated exposure. Think black lung disease for coal miners. Ditto asbestos used in construction. Even plaster or chalk dust.
Wind moves dust in dry places. A small wind gust can swirl debris almost anywhere, such as the driveway or a city street. A strong, well-formed, relatively short-lived whirlwind makes a dust devil. It can be short or tall, like a swirling cone of dust.
Big winds, over expansive areas can form dust storms. This happened long-term in the 1930s across the American and Canadian prairie. The result was called the Dust Bowl, and great damage to the ecology and agriculture.
People with asthma or other breathing problems pay close attention to the daily air quality index, which is affected by all these sources of dust pollution.
Useful Dust
Is there anything good about dust? I mean apart from children being able to write their names on tables, cars, etc.
Beauty, maybe? You can buy sea salt spray for your hair, purported to offer texture, a natural look, and to counter some of the oil on hair to give you an extra day of good style between washes.
Sea spray (aerosol particles of salt crystals from the ocean) is formed mostly by bursting bubbles where the sea meets the air, transferring matter and energy between the ocean and the atmosphere. It’s most obvious when it dries on surfaces.
Then, too, individual dust particles are a major part of rain. Water vapor in clouds condenses (turns to liquid) around invisible dust particles. A “grain” of dust is likely at the center of every raindrop.
In agriculture, dust can enhance soil fertility and improve crop growth. Adding rock dust to fields can also help to capture carbon in the atmosphere, potentially helping to reverse climate change.
In industry, dust can be used in the production of such materials as concrete and ceramics.
Among the benefits of dust is that it reduces the air temperature, as well as reduces the risk of toxic gases in the atmosphere.
Exposing children to dust through gardens and dust in the child’s natural surroundings enhances children’s immunity.
Household dust actually purifies the air by neutralizing ozone that can harm our lungs—because one of the major components of house dust is human skin, which contains the ozone-eliminating component squalene.
Dust is important for survival because it plays a role in a range of physical, chemical, and bio-geological processes, and interacts with the cycles of energy, nitrogen, carbon, and water that are necessary for Earth system functions.
Bottom Line: Like so many things, dust is good for you—in moderation.
According to the wind sock above, the wind when the photo was taken was blowing at about 6 knots (7mph). The sky is clear, the sun is bright, and there are no flying sharks. Unless you live in England or Seattle, this is nothing to write home about.
Even though you can’t actually see it, wind can create some pretty incredible things to write home about. Our ancestors definitely thought the wind was worth writing about, especially when it picked up everything around and sent it flying through the air.
Like snow, there are seemingly endless names for specific types of winds. If you really want to know about the difference between piteraq and bora winds, check out the World Meteorological Organization or National Oceanic and Atmospheric Administration websites. I’ve included some of the most spectacular and most mythological wind events here.
Dust Devils
Suppose you experienced a Dust Devil? A small dust devil, say 18 inches wide and a few yards tall is a sight to behold. A BIG dust devil—say 33 feet wide and 1000 feet tall—can be terrifying!
An extreme dust devil can reach 60 mph and last up to 20 minutes. In the process, it could lift more than 12 tons of dirt, and the friction between wind and surface can create sparks often mistaken for lightning. In fact, dust devils are not associated with storms.
Dust devils have been known to lift roofs and collapse buildings, sometimes killing people. They’ve been reported to fling animals and 10-year-old children about. Inflatable bounce houses are especially vulnerable.
Where do they come from? When hot air at ground level rises quickly and hits a pocket of cool/cold air, it can start to spin, forming a column of air. The spinning, along with friction from the surface, allows the column to move, picking up dust along the way. Dust devils are especially likely in deserts. Usually they cause little damage.
Many traditions on the Arabian peninsula include a djinn or afreet/ ifritinside the column of dust
In Brazil, Saci-Pererêis said to live inside the dust devil and grant wishes to anyone who can steal his magic cap
Other Weird Winds
Martian dust devils form the same way as on Earth, but bigger: up to 10 times as high and 50 times as wide, with mini-lightning flashes. Dust devil trails on earth’s deserts usually disappear in a couple of days; on Mars, they remain visible (so I’m told) for weeks.
Gustnadoesare closely related to dust devils, short-lived and ground based, but they have stronger winds (maybe as strong as weak tornadoes) and develop over open plains areas of the U.S. They don’t form funnels and may go unnoticed. Though a gustnado can cause serious damage, it’s not tall enough to register as a tornado.
The actual definition of a tornado is a bit fuzzy, even among the experts. They can’t seem to agree on when one tornado stops and another starts. The swirling wind tunnel has to touch the ground and the clouds at the same time before it counts (that’s why gustnadoes aren’t really tornadoes). Tornado strength is judged by size, wind speed, and distance over the rainbow it can throw a farmhouse.
Snow devils develop when a strong wind hits a solid object (like a mountain), spins downward and lifts up snow, creating a vortex. They usually last only a few minutes, and they are small (seldom more than 30 feet across). Still not something one would want to be out in.
Fire whirls, aka fire devils or fire tornadoes, develop a vortex inside a wildfire. They are whirling columns of fire rising up into the air. They carry ash, debris, and smoke and feed the fire and spread it. Fire whirls have also been reported at volcanos and during earthquakes.
A firestormdevelops when a fire becomes so big and intense that it creates its own storm-force wind systems. Firestorms are most often associated with wildfires and brush fires, but they can also be created when large sections of densely built cities catch fire.
Haboob (هَبوب) is a kind of huge dirt devil found in deserts around the world, including the U.S., associated with thunderstorms. When the rain is released, it causes sand to blow up, making a wall of sand that precedes the storm. Haboobs can be several miles high and 60 miles wide.
Sandstorms(aka dust storms) don’t whirl or spin. It’s essentially a wall of wind that pushes sand in a more-or-less straight line. Entire dunes can be picked up and moved great distances. Sandstorms occur worldwide, wherever deserts are found.
Each spring, areas along the eastern Mediterranean, North Africa, and the Arabian peninsula are hit by a khamsin (خمسين from Arabic word for 50). The khamsin is a 50-day wind that coats everything in sand and dirt. In 2009, remains were found that appear to be those of a Persian army of more than 50,000 that vanished in 525 BCE. A strong wind that blew up from the south is suspected of covering them in suffocating mounds of sand.
A downburst occurs when the downdraft of a thunderstorm hits the ground and forces the air to gust outward and curl backward. As it moves horizontally, the wind can cause extensive damage to everything it passes over. The wind curling backward can cause further damage, creating tornadoes, waterspouts, snow devils, sharknadoes, and fire whirls.
A macrobursthappens when an extremely strong downdraft hits the ground. Horizontal gusts cover an area more than 4 km in diameter. These gusts can be as destructive as a tornado.
Microburstsare smaller in size and shorter in duration. A microburst is less than 4 km across and short-lived, lasting only five to 10 minutes, with maximum windspeeds sometimes exceeding 100 mph.
A derechois a widespread, long-lived wind storm that is associated with a band of rapidly moving showers or thunderstorms. A typical derecho consists of numerous microbursts, downbursts, and downburst clusters. By definition, if the wind damage swath extends more than 240 miles (about 400 kilometers) and includes wind gusts of at least 58 mph (93 km/h) or greater along most of its length, then the event may be classified as a derecho.
Ground blizzards don’t involve any snow falling from the sky, but they are still deadly. Instead, snow that is already on the ground is whipped into whiteout conditions by an extreme cold front. Temperatures plummet, and snow on the ground is picked up by wind gusts up to 60mph. The Arctic cold fronts that cause ground blizzards also cause extreme low temperatures.
Every one of these wind events have been known to kill people! In addition, extremely hot or cold winds can do the same. Though we usually can’t see the air itself, the effects are pretty amazing!
Godly Winds
Deities connected to the wind are often closely related to those of the air. In many traditions, the air and the wind are governed by the same deity. Cultures heavily reliant on changes in the wind, such as seafaring communities or nomadic groups on open plains, tend to have more detailed and powerful wind and air gods.
One of the most famous wind gods in mythology is Aeolus, the Greek god governing all winds, who was closely involved in Odysseus’s voyage home. He is certainly not the only supernatural being in charge of the wind and air.
If that’s not enough to convince you that wind and air hold a prominent position in our collective subconscious, just look at how many modern superheroes (and villains) have the names and powers of wind phenomena.
Cyclone in the DC Universe
Cyclone in the Marvel Universe
Silver Banshee, villain who fights Batman and Supergirl
Wind Dancer of the New Mutants
Dust Devil of the Masters of Disaster
Wind Warrior of Earth Force
Red Tornado of the Justice League
Macroburst from The Incredibles
Firestorm of the Legends of Tomorrow
Bottom line: We tend to think in terms of breezes or stiff winds, but there’s so much more to wind than that!
Stay tuned, coming on Friday: When wind meets water, they create some of the most extreme weather.