Summary – 28 May 2008

Today’s operations were quite successful. After the 1 pm briefing, our teams of two forecasters worked archive cases with PAR and CASA such that everyone has seen both data platforms in the two day period. Emphasis then shifted to the Probabilistic Warning program, beginning with an introductory presentation, then moving to the Hazardous Weather Testbed to practice the knobology of issuing warnings with WDSSII. The forecasters used data from a hail-producing thunderstorm in far southwest Texas to practice.

When operations began at 2200 UTC, operations moved up into New Mexico, within a tornado watch box where moist low level upslope, veering wind profiles, and an impinging broad jet stream supported supercell structures. Team 1 (Brad and Mark) were assigned a hail-producing storm near Los Alamos, where the SHAVE project was able to make verification calls in real time. Team 2 (Kevin/Eric) jumped onto a rightward-moving supercell in a rural area ENE from Albuquerque. The event was particularly well defined for Team 2, who followed this and a second supercell that developed in close proximity…for the entire 3.5 hour IOP. They maintained high tornado and hail probabilities with the lead supercell until it became HP, at which time the tornado probabilities decreased somewhat. The second supercell followed the path of the first, and the team had lower tornado probabilities until a well defined RFD caused probabilities to spike just at the end of operations.

Team 1 issued hail swaths on a series of storms that initiated in the foothills near Los Alamos. SHAVE verified this with marginally severe hail, and one golf ball report. After this area was overturned by a train of cells, the team shifted operations to southeast New Mexico. Much like Team 2, Team 1 was able to handle probabilistic threats for hail on two different storms, with a short-lived tornado probability on the eastern-most storm. The activity was just becoming elevated with a weakening trend when operations ended at 0130 UTC. The groups then gathered around with our two Prob-Warn cognizant scientists, Kristine and Travis, for a post-event discussion. We will take a fresh look at this event during the first part of our briefing on Thursday.

Patrick Burke (EWP Weekly Coordinator, 27-30 May)

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Live Blog – 28 May 2008 (7:57pm)

Both teams continue to follow the same storms mentioned in the previous post. A glitch has prevented auto-updates in AWIPS D2D, but WDSSII is operating well. Team 2 notes their lead storm is taking on HP character as it approaches the north side of Tucumcari. They are toning the tornado probability down while maintaining a high probability of severe hail. They will also initiate a damaging wind threat area.

Kevin of Team 2 examining side-by-side supercells:

Tucumcari Storm

Team 1 has threats for hail on both the Chaves and Alamagordo storms. They have a low probability tornado threat area for the Chaves storm, which has just begun to interact with the aforementioned boundary.

Brad with Team 1 monitors the Alamagordo storm from his workstation and using the SADS:

NM and SADS

Patrick Burke (EWP Weekly Coordinator, 27-30 May)

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Live Blog – 28 May 2008 (7:15pm)

Both teams appear comfortable with handling multiple threats, even on multiple storms. Team 1 is warning for hail with the storm east of Chaves. They are curious to see how this storm evolves upon interacting with a NNW-SSE oriented boundary located in the path of the storm. They also issued a high confidence hail warning for a storm southeast of Alamagordo…which has a 3-body scatter spike, and for which MESH indicates 3 inch hail.

Team 2 has been following a long-lived supercell which has occasionally produced a TVS, and at one time a fairly strong TVS…tracking just north of I-40 toward Tucumcari. They are maintaining high probabilities for hail and tornado with this cell…and have just added a low probability for tornado with a second supercell following in the path of the first. These cells are moving along an east-west oriented boundary of unknown origin…which may have bee produced by differential heating.

Patrick Burke (EWP Weekly Coordinator, 27-30 May)

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Live Blog – 28 May 2008 (4:30pm)

PROB-WARN Ramping Up

Forecasters will head back to the Hazardous Weather Testbed to practice drawing probabilistic warnings…then an intensive operations period is planned beginning sometime after 2200 UTC…most likely in the area just east and southeast of Albuquerque, NM. Northeast parts of the state may be too stable to support a long-lived storm.

Patrick Burke (EWP Weekly Coordinator, 27-30 May)

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Live Blog – 28 May 2008 (3:37pm)

Eastern New Mexico Heating Up

The SPC has outlined a mesoscale discussion for eastern New Mexico, where a weather watch may be needed soon. Satellite and surface observations suggest the original target of northeast NM has been slow to warm up beneath widespread stratocumulus clouds north of the frontal boundary. Greater destabilization has taken place along the I-25 corridor and into east-central/southeast NM. This zone of greater instability should develop northward this afternoon. Thunderstorms are initiating in a widely scattered fashion between Albuquerque, Pecos, and Clovis. One cell near ABQ briefly exhibited supercell character with a small appendage and sharp reflectivity gradient.

Patrick Burke (EWP Weekly Coordinator, 27-30 May)

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Live Blog – 28 May 2008 (3:26pm)

Archive Cases Ending…Prob Warn Training to Begin

Our teams are filling out PAR and CASA evaluations following their archived events.

Kevin/Eric discussed how to best display CASA data. They would like to be able to easily choose one radar and tilt up to higher elevation. They like the utility of CASA at low levels for wind/tornado threat without much thought to hail threat.

Yesterday…they were hanging on every 1-minute update with PAR, looking intently for changes in storm character. They did not experience the same type of anticipation with CASA today. This could be related to the case selection. Some positives they point out are the fine spatial resolution and near ground sampling.

With both PAR and CASA, Kevin sees need for substantial training to avoid dramatic increase in false alarm rate. These small scale signatures and short-lived shear couplets or RFDs have always been out there. Now that we can see them, it doesn’t necessarily mean we should be warning for each of them.

Brad/Eric are discussing when additional information becomes too much. “Rarely would a meteorologist decline more information, but in some cases it just becomes more on the floor (or tossed aside).”

All forecasters are moving to a seminar room for training on Probabilistic Warnings from 2045-2130 UTC.

Patrick Burke (EWP Weekly Coordinator, 27-30 May)

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Outlook – 28 May 2008

We have potential for a Prob-Warn exercise this afternoon across the high plains adjacent to the mountains of eastern Wyoming through eastern New Mexico. Thunderstorms are not imminent, however, so to make the most of this shortened week, we will run archive PAR and CASA events between 1830 and 2030 UTC. The forecaster teams will be the same as yesterday, with Kevin and Eric moving over to the CASA desk and Mark and Brad working PAR.

Training on probabilistic warnings will ensue between 2030 and 2200 UTC. We then intend to run Prob-Warn operations in eastern New Mexico from 2200-0200 UTC. Moderate southwesterly upper flow is in place on the far western high plains, while moist southeasterly low-level upslope is increasing. A stalled frontal boundary will begin to lift northward through New Mexico this afternoon, and veering wind profiles north of the front will favor rotation with updrafts initiating in the deep mixing zone along the high terrain. Deep layer shear may actually be stronger up north toward Wyoming…but greater moisture/instablity, and a potentially wider CAPE axis favors operations in northeast New Mexico…where several models, including the short range ensemble, suggest a high probability of thunderstorms. The SPC has outlooked that area with a Slight Risk, including a small 5% tornado contour.

Day1 Outlook

Patrick Burke (EWP Weekly Coordinator, 27-30 May)

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Summary – 27 May 2008

Our four visiting forecasters arrived ready to work, and the day promised a fair chance of Oklahoma-based operations. After a quick tour of the National Weather Center, the group convened in the NSSL Develoment Lab for orientation, followed by a map discussion. Participants were trained on the PAR and CASA data platforms before moving to the Hazardous Weather Testbed around 21 UTC. Software training for the WDSSII used real-time data of a supercell occurring near Altus, OK.

Kevin (WFO OUN) and Eric (WFO AFG) then jumped on at the PAR workstation to dissect the Altus supercell at long range. Brad (WFO SEA) and Mark (Environment Canada – Winnipeg) practiced WDSSII using KFDR data on the same supercell, and were on standby for possible CASA operations. By 23 UTC, though, it became clear that thunderstorms would propagate southward into northwest Texas…as stable air emanating from a second storm complex had overspread the CASA domain.

By 2330 UTC…real-time operations ended, and both groups of forecasters turned to archive events. The pace slowed down, allowing more time for discussion of data strengths and weaknesses. The PAR data, in particular, spurred some interesting ideas as to what forecasters would ideally like to receive from a radar system. The CASA participants expressed some difficulty operating in a small domain using multiple radars. They also noted that the KTLX 88D better sampled one occurrence of strong straight-line winds, simply owing to viewing angle. They were impressed, however, at the temporal and spatial resolution of the CASA data which captures many interesting storm and sub-storm scale features.

Patrick Burke (EWP Weekly Coordinator, 27-30 May)

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Live Blog – 27 May 2008 (6:29pm)

Storms in western Oklahoma have either weakened or moved southward to very long range from central Oklahoma radars. Today’s severe potential is largely driven by the diurnal cycle, and there is little hope of additional activity; the MCS outflow from this morning simply proved too deep and widespread across central Oklahoma. The event did provide Eric and Kevin a chance to become familiar with PAR data, and they will continue that theme by working an archived event this evening.

Eric and Kevin Examine archived PAR data.

Meanwhile, Brad and Mark are viewing archived CASA data to increase their comfort level with the look and feel of that data. Between 2330 UTC and 0130 UTC they plan to run through another event in real-time playback to evaluate the utility of CASA data in making warning decisions.

Brad and Mark work with Jerry Brotzge viewing archive CASA data.

Patrick Burke (EWP Weekly Coordinator, 27-30 May)

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Live Blog – 27 May 2008 (5:40pm)

PAR Temporal Resolution Discussion…

Eric & Kevin are working the Altus storm… and their first look at PAR and 88D side by side has sparked discussion of the differences in resolution and sampling techniques. Kevin would like to see enhanced azimuthal resolution (lower beam width) for PAR in the future. Kevin remarks that the 1-minute update has made it easier to pick up on new cell development along the storm’s rear outflow flank. The forecasters earlier observed a supercell split on the Elk City storm…and felt the rapid updates were beneficial to seeing this.

Eric has another interesting perspective. He thinks the 1-minute resolution might be “annoying” early in an event when you don’t yet have a particular severe weather threat or focus. It may be overwhelming to process so much data. Maybe we should apply the forecast funnel to this… and be able to choose when to switch from 5 or 10 minute resolution down to the 1-minute resolution as needed.

Patrick Burke (EWP Weekly Coordinator, 27-30 May)

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