Cumulo-fractus clouds |
|||||
FTLComm - Tisdale - Wednesday, May 16, 2007 | |||||
Water vapour rising into the cool atmosphere forms visible clouds and the most common of these are fair weather cumulus clouds like those seen below. But when we get a huge weather system of rising wet air a number of things can develop and one of the most difficult of these is the formation of a cumulo-stratus layer with embedded towering cumulus above. Systems like this are not visible from the ground and the combined effects of multiple cells can produce some difficult conditions. |
|||||
That's where the cumulo-fractus clouds come in handy. These small fragments of clouds form beneath the stratus layer and are a clear indication of rain approaching. When you spot a few of them you can surmise a shower is approaching but when you see a lot of them and they are particularily diffuse you can expect serious storms to accompany the showers and if the temperatures are in the mid twenties you can assume that the towering CBs above will be powerful and there is always the chance of hail and sometimes tornados. | |||||
|