Mike Krzywonski
I've seen meso icons on GRL3 & Baron appear on storms that weren't even severe-warned. How accurate are these icons?
I've seen meso icons on GRL3 & Baron appear on storms that weren't even severe-warned. How accurate are these icons?
I've seen meso icons on GRL3 & Baron appear on storms that weren't even severe-warned. How accurate are these icons?
Remember the presence of a meso isn't enough to force a warning for either SVR or TOR no matter how "strong." The conditions specific to those warnings have to be met. If there's no wall cloud or rotation in a wall cloud (or, God forbid, a tornado on the ground), no 3/4 inch hail, and no 60+ gusts or the recognized radar prediction/detection thereof, there's probably no warranting of an SVR/TOR.
Correct, but what is the likelihood of a non-severe storm having rotation? Are these true mesos?
I've seen meso icons on GRL3 & Baron appear on storms that weren't even severe-warned. How accurate are these icons?
AMA Glossary of Meteorology said:supercell—An often dangerous convective storm that consists primarily of a single, quasi-steady rotating updraft, which persists for a period of time much longer than it takes an air parcel to rise from the base of the updraft to its summit (often much longer than 10–20 min).
Most rotating updrafts are characterized by cyclonic vorticity (see mesocyclone). The supercell typically has a very organized internal structure that enables it to propagate continuously. It may exist for several hours and usually forms in an environment with strong vertical wind shear. Supercells often propagate in a direction and with a speed other than indicated by the mean wind in the environment. Such storms sometimes evolve through a splitting process, which produces a cyclonic, right-moving (with respect to the mean wind), and anticyclonic, left-moving, pair of supercells. Severe weather often accompanies supercells, which are capable of producing high winds, large hail, and strong, long-lived tornadoes. See also convective storm, thunderstorm, splitting convective storm, cell, bulk Richardson number.
Not true. The MDA requires two vertically-associated features from adjacent elevation angles, and that the depth is at least a) 3 km or b) 25% of the average depth of the 10 strongest SCIT detections. It also requires detections on two adjacent volume scans for persistence.Supercell mesocyclones must be vertically deep and persistent, but the MDA will trip for shallow (one elevation scan) rotation during only one volume scan.
Not true. The MDA requires two vertically-associated features from adjacent elevation angles, and that the depth is at least a) 3 km or b) 25% of the average depth of the 10 strongest SCIT detections. It also requires detections on two adjacent volume scans for persistence.
That being said, there are other issues with the MDA that are currently being investigated, 1) decreased data quality in the clear air since 2006 causing false shear detection, and 2) a small bug in the code for low-core detections.
</snip></snip>NWS WDTB: RDA/RPG Build 9.0 Training said:A minimum of two elevation angles is needed for the 3D correlation of 2D features to identify a circulation or a mesocyclone.
<snip><snip>
I've seen chief meteorologists in tornado-prone markets relying solely on the 'shear markers' while doing live break-ins and not really expounding on their own observations...makes me wonder if they're even capable.<!-- / message --><!-- sig -->