The four-day conference, CMMP 2004, will take place from Sunday 4th to Wednesday 7th April 2004 at the University of Warwick, UK. Highlights include a presentation on Monday 5th April by Chris Westbrook and Professor Robin Ball from the University of Warwick who will be revealing progress towards developing a computer simulation of snowflake formation within clouds.

The aim of the project - which is in collaboration with Dr Paul Field at the Met Office, who originally suggested the study - is to increase the accuracy of weather forecasting by allowing more information to be extracted from radar and satellite measurements of clouds.

When the temperature in a cloud is low enough, any water will usually form ice crystals. These can have many different shapes including rods with hexagonal sides and rosettes (which consist of three or more rods growing outwards from a central point), as well as the more familiar six-armed ice 'stars'.

As the ice crystals move through clouds they bump into each other and stick together. Eventually the crystal clusters become so large that they are heavy enough to fall out of the cloud as 'snowflakes' (where any individual snowflake will consist of a cluster of ice crystals of one particular shape). So far the Warwick team have investigated the clustering together of both rods and rosettes in cold, high altitude ice clouds known as cirrus clouds.

"We compute what would happen if you just randomly distribute these clusters in space then track what collisions will occur as they fall under gravity" explains Professor Ball. From these calculations, which assume the crystals stick together on contact, the Warwick team has obtained predictions of the shapes and the distribution of different sizes of ice clusters in cirrus clouds.

These agree well with much of the experimental data obtained from various instruments including cloud particle imagers - special cameras which use a laser beam to illuminate the particles being photographed - by the National Center for Atmospheric Research in the USA.

The theoretical simulation does not however shed any light on why the ice crystals stick together. This process is occurring even at temperatures as low as -40�C, where it is too cold for the accepted higher temperature method - of a thin liquid layer on the surface of the crystals freezing on contact and joining them together - to work.

"We are already in a position to develop better interpretation of standard radar and satellite imaging techniques, but to firmly predict the size and concentration of ice crystal clusters - and hence reveal how intense the rain or snowfall will be - we need to know how the clustering starts.

So we are now contemplating a direct attack on the question of what the sticking mechanism is" says Professor Ball, who acknowledges that modelling behaviour like this at a molecular level will be challenging due to the vast amounts of computing power needed.

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