espere Environmental Science Published for Everyobody Round the Earth
Printer friendly version of this page
Home    Contact    Encyclopaedia    Mobility    International    PDF    magazine    - ? -   
Clouds and Particles
1. Clouds
- Water in the atmosphere
- Formation of clouds
- Cloud types
* Worksheet 1
* Worksheet 2
* Worksheet 3
* Worksheet 4
2. Particles
3. Sun and clouds
clouds and particles

Clouds & Particles


Formation of clouds

A cloud is composed of millions of little droplets of water or ice crystals, when temperature is very low, suspended in the air.  Clouds can form when water vapor becomes liquid, i.e. when humid air is cooled the water vapour condenses onto tiny particles.  We now look at the major ways in which clouds form.



formation of clouds by convection process.

1. Formation of clouds by convection process.
Author: J. Gourdeau.



On Earth, the density of air depends on its temperature.  This means that warm air rises and cold air sinks because warm air is less dense than cold air.  This movement of warm air upwards is known as convection.  Convection is one of the processes that allows clouds to form. The Sun warms the surface of the Earth.  This warmth heats the humid air at the ground and, as a result, the air becomes less dense and begins to rise.  As the air rises, it cools.  Clouds are formed when the humid air cools below a critical temperature: the water then condenses onto tiny suspended particles and forms water droplets in the air.


Topography (mountains) 

Clouds also form over mountains or hills.  These clouds are called orographic clouds.  The air is forced to rise over the mountain and, as it rises, it cools.  If the air cools to its saturation point, the water vapour condenses and the water contained within the air becomes visible as a cloud.


clouds over mountains
2. Source: NOAA
clouds over mountains
3. Source: NASA

The Foehn effect

When air rises over the mountains, it cools and becomes saturated with water vapour. Condensation occurs and the water vapour becomes liquid. This liquid water stays as clouds or falls as rain as the air continues to rise.  When this air descends on the other side of the mountain it contains less water so it is warmer and dryer.  The difference in temperature from one side of a mountain to the other is known as the Foehn effect.

When different air masses meet

It's not only mountains which force air to rise.  When warm air meets a mass of heavier cold air, the warm air is forced to rise.  The boundary between warm and colder air is called a front. As the warm air rises it cools and as it cools clouds may form.


cold front-rising warm air
4. Cold front.   A: cold air; B: warm air.  Here cold air moves towards a warm air mass and forces the warm air to rise.  Author: J. Gourdeau.
warm front-rising cold air
5. Warm front.  A: cold air; B: warm air.  Here warm air moves towards a mass of cold air and rises.  Author: J. Gourdeau.

Horizontal motion

Sometimes winds bring warm and moist air into a region. If the warm moist air moves over a much colder surface, it is cooled and the moisture it contains will condense and form fog. This process occurs frequently at the coast.


Fog over a lake

6. Fog over a lake. Source: Ph. Osset

About this page
author: Dr. Justine Gourdeau - LaMP, Clermont-Ferrand, France
scientific reviewer: Prof. A. Flossman - LaMP, Clermont-Ferrand, France
published: 2003-03-12



last updated 21.02.2006 12:14:54 | © ESPERE-ENC 2003 - 2013