Category: Snow

What are the requirements for snow?

There are three main requirements for snow, these are:

1. Moisture

   There must be water vapour in the air for clouds to form. In the UK, surrounded as we are by sea, this is rarely a problem. As water warms up and cools down more slowly than land, the sea around us stays at a pretty constant temperature all year round and is a constant source of water vapour into the air above, through evaporation.

   It can be ‘too cold for snow’ in the centre of large land masses, such as Eurasia, Antarctica or N. America, where the wind has not encountered liquid water from which water can easily evaporate. It’s really ‘too dry for snow’ – but it’s too dry because it is so cold that the rate of evaporation from the lakes and rivers, which may be frozen, is very, very slow. 

2. Cloud

   For clouds to form, the rate of evaporation must be lower than the rate of condensation. Evaporation and condensation are going on all the time, but the rate of evaporation falls as it gets colder. So, clouds can form when the air cools – there are several possible mechanisms for this

• Where warmer air meets colder air at a front, causing it to rise. As the air rises, the air pressure falls and so the air cools (this is known as adiabatic cooling).
• When air from somewhere colder than us (i.e. Arctic maritime of Polar Continental air masses) approaches the UK, is warmed from below as it travels over relatively warm land or sea which causes it to rise and cool. This is the most common source of snow in the UK.
• When air is forced to rise over the coast, hills or mountains and, as it rises, cools. This mechanism can add to, or enhance, the formation of cloud by either of the other mechanisms above.
• If the ground cools overnight, the air in contact with the ground can cool to the temperature at which cloud forms. This is fog and is not likely to produce rain or snow.

3. Temperature

   It has to be cold enough for the cloud droplets to grow as snowflakes and to not melt as they fall through the atmosphere and down to the ground.  To see whether this is the case, forecasters look at the 528dam (=5280m) line. This line shows where the vertical thickness of the bottom half of the atmosphere (by mass) is 5280m i.e. the vertical distance between the 1000mb height (somewhere near the ground) and the 500mb height (somewhere in the middle of the troposphere). As warm air is less dense than cold air, the smaller this distance, the colder the air is.

If we are north of the line (i.e. the thickness is less than 528dam) then any precipitation can fall as snow, and if we are south of the line (i.e. the thickness is greater than 528dam) then we get rain.

If you look at the surface pressure forecast charts on the Met Office website, then if you go more than 24 hours into the future the thickness lines are shown. The 528dam line is shown as a blue dashed line, and the thicker/ warmer 546dam line as a green dashed line.