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Quote: Hi Danny.. The kind of Storm Relative Helicity in question is a measure consisting of two parameters: 1) Stream line shear with height. 2) Directional shear with height. 1)...is the increase in wind velocity ascending through the layer in question. 2)...is the change in wind direction asceding in altitude. The calculations are performed at 1km and 3km layers above ground level. The units suggest this in being m/ss. The larger the SRH, the greater the chance for tornado development. SRH Value Tornado Potential 150-299 weak 300-449 moderate >450 strong Simpler "Helicity" is just a measure of rotation in a storm's updraft... You can bet that a huge SRH value will be codependent. |