A rumbling in the distance, the weather radio going off, the storm siren blowing - all are sure signs a big and nasty thunderstorm is about to move through immediate area. However, for 2009, this has been a rare sight, with only a handful of severe weather warnings issued in late April and May. In past years, we’ve already experienced our share of weather by now. You may recall in May 2008, when we experienced that severe weather blowout just before Memorial Day, with tornadoes and grapefruit sized hail. That event was followed by eight consecutive weekends where a severe thunderstorm warning or a tornado warning was issued for at least one of our 14 counties.
So what’s the deal? That answer boils down to one crucial element in weather - wind. Sure, you need that hot sun during the spring, summer and early fall to help power up those storms. But in the end, you need the right kind of wind to kickoff those nasty thunderstorms.
Wind’s first role is fueling the thunderstorm. Southerly winds usher in crucial moisture from the Gulf of Mexico, while rapidly shifting upper-level winds induce regions of rising and sinking air in the atmosphere. Areas where air is sinking can be especially helpful to severe weather development, as it puts a cap on any lower-level being pulled northward from the gulf. Just like a lid on a boiling pot of water, moisture builds up at the ground, until a little burst of dry air breaks that cap, sending the moisture high into the atmosphere, fueling thunderstorms.
Secondly, not only must the wind bring in moisture, but it must have the right amount of shear. Wind shear is defined as the wind’s change in direction and speed with height in the atmosphere. For example, for optimal severe weather development, the winds just above the ground should be out of the south at around 10-15 miles per hour, while three to four miles above ground, winds should be westerly between 50 to 70 miles per hour. This shift in direction and speed causes tilted updrafts to develop, a critical component of a severe thunderstorm. That’s because tilted updrafts will feed moisture to the thunderstorm for a long duration, unlike vertical updrafts, which are “killed” when rain falls out of the sky. If the winds aloft are too weak, or the winds at the ground are too strong, the updrafts will not be sufficient enough for severe weather development.
So now you know a little about wind and its impact on severe weather development. And speaking of severe storms, keep your eyes to the sky the next few days, as an approaching low will kick up a few thunderstorms that could reach those severe limits. Of course, we’ll be keeping you tuned!
Have a great day, and thank you for reading!
Meteorologist Nick Grunseth
This post was written by ngrunseth on July 8, 2009
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