SRH is calculated by integrating the cross product of the horizontal wind vector and its derivative with respect to height over a specified layer of the atmosphere. The units are typically expressed in meters squared per second cubed (mΒ²/sΒ³).
V_h(z) = Horizontal wind vector at height z
z_1, z_2 = Lower and upper bounds of the integration layer
What is storm-relative helicity?
How is SRH calculated?
What are the units for storm-relative helicity?
Why is SRH important in meteorology?
Can storm-relative helicity be used for any other purposes besides predicting tornadoes?
How does the layer of atmosphere affect SRH calculations?
What data is needed to calculate storm-relative helicity?
Results are for informational purposes only and do not constitute professional advice.
