Thursday, June 26, 2008

Weekend Storms?

It's been an active week and a half for much of the Northern Plains, and the same song and dance continues this evening with several severe weather watches in effect. Fortunately, the tornado outbreaks have been limited by a fairly weak zonal flow aloft. Unfortunately, large hail storms have been the rule, and I'm sure the insurance companies are staying quite busy.

Turning my attention closer to home, models are in good agreement on digging an abnormally strong trough into the Southeast U.S. this weekend. After reading area forecast discussions around the area, I'm a bit surprised that the severe weather threat is not being hit harder. There should be plenty of instability in advance of the cold front. Combine that with unseasonably strong wind fields, and this set-up should support a much higher than normal chance of severe weather in states like Alabama, Mississippi, Tennessee, and Arkansas. It will be interesting to see if this gets more hype tomorrow. Regardless, the cold front should push well into the Deep South by Monday and will cool temperatures off significantly for most areas -- at least for a couple of days.

Very quiet weather continues to dominate the tropics, but I get the feeling that won't last much longer. Any storms that do form later in the year will probably intense with the undisturbed ocean waters. However, it will be interesting to see if a weak El Nino develops this season, which may help to limit the number of named storms. The 90 day SOI is fairly neutral and doesn't point to any strong signals of a La Nina or El Nino event.

Friday, June 13, 2008

Wednesday Storm Surveys

Just a few links to select storm surveys from this past Wednesday's tornado outbreak across the Central Plains.
Manhattan, KS tornado -- EF4
Chapman, KS tornado -- EF3
Little Sioux, IA tornado -- EF3

A northwest flow aloft should develop across the Plains states this week and will likely prevent large tornado outbreaks for the foreseeable future. The chances for MCSs will increase and with that the likelihood of more flooding rains across the Missouri and Mississippi Valleys. I like this pattern in the summer because it means chances for surprise nocturnal thunderstorm complexes and lightning photography opportunities in Mississippi!

Thursday, June 12, 2008

Little Sioux, IA Tornado

The big news from yesterday's tornado outbreak was the killer tornado just north of Little Sioux, IA. Four scout troops died at the Little Sioux Scout Ranch when the tornado tore through the campground. The storm that spawned the tornado was clustered in a line of storms -- certainly not an ideal setup for tornadoes. The yellow triangle (Tornado Detection Algorithm) indicates the approximate location of the tornado in the messy base reflectivity scan.


However, the storm relative velocity clears up the picture and certainly shows strong rotation within the storm. The Omaha, NE radar sampled the storm at about 2,500 feet above the surface, and the SRV product shows a 41 knot inbound velocity and a 56 knot outbound velocity. The gate-to-gate rotation was 97 knots or 112 mph.


The same storm system produced a rash of tornadoes in north-central Kansas last evening as well (see the post below). In fact, heavy damage was reported around Kansas State University, including a building that houses a nuclear research reactor! The same supercell earlier wiped out the town of Chapman and later killed a person near Soldier, KS.

Wednesday, June 11, 2008

Manhattan, KS Tornado

A long-lived supercell plowed across north-central Kansas and produced several tornadoes along its track. One of the supercell's tornadoes struck Manhattan, home of Kansas State University, around 11:00 p.m. this evening. The base reflectivity and storm relative velocity images I saved show a classic tornado signature. In fact, the base reflectivity (scanned at 0.5 degrees) shows a possible debris signature associated with the tornado. The high reflectivity (66 dBZ) that I circled is a significant energy return, but the VIL product at the same time only returned 16 kg m^-2. Furthermore, the echo was only 1,400 feet above the ground, and there was no hail core suspended above this signature. Therefore, it's quite possible this could be some type of debris that was sampled by the radar.


The storm relative velocity sampled at the same time also shows a very tight, cyclonic circulation at the approximate location of the high reflectivity return. The green colors indicate motion toward the radar, and the red/pink colors indicate motion away from the radar; the Topeka radar is southeast of this image. The inner green color is a 33 knot inbound velocity, and the inner pink is a 58 knot outbound velocity; added together, that is a 91 knot (105 mph) total circulation -- quite impressive for about 1,400 feet above the ground.

Wednesday, June 4, 2008

Iowa Supercell


A pristine environment for supercells developed across Iowa this evening with large instability (MLCAPE >3,000 J kg-1) balanced by strong deep layer wind shear (55 kts). One large, discrete and cyclical supercell has persisted for the last several hours over southwest Iowa, and has occasionally produced large tornadoes. This is a classic example of a supercell riding along a boundary and ingesting large amounts of storm relative helicity, which helps aid in tornadogenesis. For more information about this, I highly recommend the Markowski et al. (1998) paper.

Tomorrow's severe weather environment setup looks great for a large portion of the Central and Southern Plains. The western U.S. trough swings out into the Plains tomorrow and should provide the lift necessary to generate a severe weather outbreak. It appears that storms should initially develop across Nebraska as discrete supercells, but they should congeal into a linear complex somewhat quickly given the parallel orientation of the deep layer shear vectors to the front. Further south across Kansas and Oklahoma, it appears as though the winds may be slightly more perpendicular to the front to allow for a longer period of discrete storms. Therefore, this should increase the risk for a tornado outbreak across these two states, especially given that 0-1 km SRH values are forecast to range between 150-300 m^2 s^-2. Sadly, I'll be arm chairing this event.

Monday, June 2, 2008

Monday Thoughts

A derecho swept across northern Kansas to southwest Missouri today. Derechoes are notoriously known for the wind damage they produce, but this particular derecho produced significant hail in addition to damaging winds. In fact, 4.25" hail was reported near Manhattan and Waverly, KS this morning. 4.25" hail is just slightly smaller than a softball!

I was fortunate enough to capture the image below at sunset last evening. After we got back to Starkville, a long-lived MCS moved through and produced gusty winds and minor tree damage in town. After its exit, it made for a picturesque sunset.


The deepening western trough kicks out into the Plains on Thursday, and pattern recognition certainly suggests the potential for a significant severe weather outbreak. Copious moisture will surge northward Wednesday evening and Thursday. Meanwhile, an energetic upper-air system will spread across the warm sector, and will create an environment highly supportive of supercells. More specific details tomorrow.