There are three different ways of turning moist air into cloud, so that it rains or snows.
Rain - and other forms of precipitation - occur when warm moist air cools and condensation occurs.
Since warm air can hold more water than cool air, when the warmer air is cooled the moisture condenses to liquid - and it rains.
The video and text below explain how rain forms and the different types of rain that we get in the UK
Frontal rain occurs when two air masses meet. When a warm air mass meets a cold air mass, they don't mix as they have different densities (a bit like oil and water). Instead, the warm less dense air is pushed up over the cold dense air creating the 'front'. As a result, much like when air is forced up over mountains, the warm less dense air cools, and the water vapour condenses into water and falls as raindrops. This type of rain can happen anywhere in the UK.
Orographic rain is rainfall produced as a result of clouds formed from the topography - or shape - of the land. Where there is high ground moist air is forced upwards producing cloud and potentially, precipitation.
Mountainous areas close to prevailing westerly winds are most likely to experience this type of rainfall. The geography of the UK means that this type of rainfall is most common in the north and west of the UK where warm moist air from the Atlantic cools as it is forced upwards over high altitudes.
Convective rain is produced by convective cloud. Convective cloud is formed in vertical motions that result from instability of the atmosphere. One way that the atmosphere can become unstable is by heating from the sun. The ground warms up, causing moisture in the ground to evaporate and rise, and the hot ground also heats the air above it. As the water vapour rises, it cools and condenses into clouds and eventually rain.
When you heat the air from below like this, much like in a boiling kettle, you tend to get "bubbles" of rising air, known as updraughts. These are much smaller than the large-scale lifting of air that occurs at fronts and over mountain ranges. This tends to give us smaller areas of rain, with clear spells in between, commonly referred to in the UK as "sunshine and showers".
This type of rainfall is most common in the south and east of the UK, where it is typically warmer. This area is also prone to very heavy showers and thunderstorms, this is because the warmer air can hold more water.
Sometimes, you can get all three types of rain at once, and this can lead to severe flooding.
Under certain conditions, rain can fall from the sky without ever reaching the ground. It happens when rain falling from a cloud evaporates or sublimes as it approaches the earth's surface.
This creates what is known as Virga clouds, a tail or wisp extending from a cloud in a downwards direction and are generally seen to extend from Cirrocumulus, Altocumulus, Altostratus, Nimbostratus, Stratocumulus, Cumulus or Cumulonimbus clouds.
Perhaps you've been caught in the rain and wondered if its better to run as fast as you can to get out of the rain, or whether running into the rain will make you wetter than walking?
Recent research has suggested there is no easy answer affected by factors as varied as the individual's height-to-breadth ratio, wind direction and the size of the raindrops.
Professor Bocci who conducted the research in the Journal of European Physics did though offer the overall conclusion that "in general, the best thing is to run, as fast as you can - not always, but in general."
When raindrops fall on dusty or clay soils, they trap tiny air bubbles on the surface which then shoot upward - as in a glass of Champagne - and burst out of the drop throwing aerosols of scent into the air where they are then distributed by wind.
This is what is responsible for the familiar smell of rain and is called 'Petrichor'.
While raindrops are usually represented in the shape of a teardrop, in reality they are not.
When they first form high up in the atmosphere, they form a spherical shape as the water molecules bind together held by surface tension.
As they begin to fall their shape changes as they hit other raindrops, while air resistance causes the bottom of the drop to flatten and curve resembling the shape of a jelly bean.
Its difficult to give an exact figure as the height at which raindrops fall and their size vary widely, but given that raindrops fall at an average speed of around 14 mph and assuming a cloud base height of around 2,500 feet, a raindrop would take just over 2 minutes to reach the ground.
Larger raindrops can fall as fast as 20 mph, while the smallest raindrops can take up to 7 minutes to fall.
The title of wettest place in the world goes to Mawsynram in the Maghalaya State of India. It receives an astounding average of 11,971 mm rainfall each year. For comparison, the UK's average annual rainfall is 1154 mm.
The reason for its torrential downpours is its proximity to the Bay of Bengal and its situation 1400 m high in the Garo Hills, to the south of the Himalayas. The southwesterly monsoons pile in with moist winds which are caught against the mountains creating huge amounts of rainfall on the village.
Villagers weave "knups" out of bamboo which form a shell-like structure to shelter from the downpours.
The wettest day recorded in Britain was the 5th December 2015 when Honister Pass in Cumbria recorded 341.4 mm of rain in a single day (0000-2359).
The heavy rainfall was the result of Storm Desmond which brought widespread heavy rain and storm force winds to areas of Scotland and northern England.
The same rainfall event also saw the highest accumulations ever recorded in Britain for a 2-day period (405 mm) recorded nearby in Thirlmere.