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What causes dew?

Have you ever stepped outside early in the morning and noticed the grass glistening as if it were covered in little jewels? Those sparkling droplets are not rain — they are dew! But where does dew come from? Why does it only appear at certain times? And what does temperature have to do with it?

Let’s dive into the cool and curious world of dew and uncover the science behind those magical morning droplets.

What exactly is dew?

Dew is the water that forms on cool surfaces — like grass, leaves, flowers, and even car roofs — early in the morning or late in the evening. These little drops are not rain or sprayed from a hose. They’re created from moisture in the air that condenses when the temperature drops.

In simple words, dew is tiny water droplets that come from the air and settle on surfaces when temperatures drop enough.

Where does dew come from?

To understand dew, we need to look at something called water vapour.

Water vapour is the gas form of water, and it’s all around us in the air — even if we can’t see it. The air always holds some amount of water vapour. But how much it holds depends on the temperature. Warmer air can hold more vapour. When the air cools, it reaches a point where it can no longer hold all that water. That’s when the water turns back into liquid — forming droplets. This process is called condensation.

So, when a surface (like a blade of grass) gets cooler than the air around it, the water vapour in the air condenses on that surface — creating dew!

What is the dew point?

Now, here’s a cool science word: Dew Point.

The dew point is the temperature at which air becomes fully saturated with water vapour and cannot hold any more. When the surface temperature drops to the dew point, dew begins to form.

Imagine the air is a sponge. If you keep adding water to it (like more vapour), it can soak up quite a bit — but only up to a point. When it’s full, any extra water will drip out. That “dripping” is similar to when the temperature drops to the dew point — the water “drips” out of the air as dew.

Why does dew form at night or early morning?

During the day, the Sun warms up everything — the air, the ground, the leaves. Warm air holds a lot of water vapour, so no dew forms.

But once the Sun goes down, the ground begins to cool. As the surface cools, the air close to the ground also cools. If it cools enough to reach the dew point, the vapour in the air turns into tiny water droplets.

This is why mornings often look “dewy” — it’s the result of nature cooling down overnight.


Where can you see dew?

Dew isn’t picky! It can form on many different surfaces, including:

  • Grass
  • Leaves
  • Car windows
  • Flower petals
  • Spider webs
  • Metal objects like bikes or fences

Basically, if it’s outside and gets cold enough overnight, it could be a home for dew!

How is dew different from rain?

Great question! Rain falls from the sky, and big drops come from clouds. On the other hand, dew doesn’t fall from the sky at all. It forms right where you find it — on cool surfaces close to the ground.

Here’s a simple table to compare:

DewRain
Forms on the ground or objectsFalls from clouds
Happens during cool, clear nightsHappens when clouds get heavy
Comes from water vapour condensingComes from clouds releasing moisture
Light and gentleCan be light or heavy

Does dew help plants?

Yes! Dew is like nature’s gentle morning drink for plants. In dry places where it doesn’t rain much, dew can actually help keep plants alive. It provides a bit of moisture, just enough to keep leaves from drying out completely.

Farmers in some parts of the world even depend on dew for their crops to survive during dry seasons.

Can dew happen anywhere?

Dew can form in many places around the world, but it needs the right conditions:

  • Clear skies
  • Calm winds
  • Cool temperatures
  • Moisture in the air

In deserts, for example, it can get super hot during the day and very cold at night — perfect for dew! Even though deserts are dry, the little moisture in the air can still form dew overnight.

What happens if it’s too cold?

If the temperature drops below 0°C (freezing point), something else happens — frost forms instead of dew! Just like dew, frost forms from moisture in the air. But instead of turning into water droplets, it turns straight into ice crystals.

Frost can make everything look like it’s been sprinkled with sugar or covered in glitter!

Can you make dew yourself?

You sure can try a simple dew experiment at home or in school!

DIY Dew Experiment

What You Need:

  • A clean metal can or glass
  • Ice cubes
  • Water

What to do:

  1. Fill the can or glass with ice cubes.
  2. Add a little water to help it cool quickly.
  3. Wait a few minutes and watch closely.

Soon, you’ll see water droplets forming outside the can. That’s not water leaking through — it’s dew! The cold can cool the air around it, causing the moisture in the air to condense — just like morning dew.

Fun facts about dew!

  • The word “dew” comes from the Old English word dēaw, which means moisture.
  • Animals like frogs and insects sometimes drink dew when there’s no other water around.
  • Some desert beetles in Africa survive by collecting and drinking dew on their backs!
  • In ancient times, people believed dew had magical healing powers.

Dew in stories and sayings

Dew is often used in poetry and stories to symbolise freshness, purity, and new beginnings. Here’s a lovely old saying:

“The early bird catches the worm, but the second mouse gets the cheese — and both get dew on their feet!”

It shows how common and beautiful dew is in the early mornings and gives a smile!

Conclusion:- Dew might seem small, but it’s a big part of nature’s daily rhythm. It helps keep plants healthy, gives animals a drink, and teaches us how air and water work together. Next time you step outside on a cool morning, take a moment to look closely — you might just see the science of dew sparkling all around you!

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