Damage Surveys


This is the unofficial, WWW version of the VORTEX-95 Operations Plan. It may differ from the published operations plan which is available by 15 March from the National Severe Storms Laboratory.


Near-Field Tornado Damage and Microbursts

In VORTEX, we are concerned with the effects of damage caused by tornadoes and by any microbursts that may accompany tornadoes with the target storms. Later in this chapter, a special survey effort is described. In that work, debris that is lofted high into the storm and deposited several to many tens of kilometers from the tornado will be documented. This phenomenon is called " far field" debris deposition.

Damage assessment

Since extensive damage surveys are planned for VORTEX, and there will be a number of different measurements of tornadic windflow, VORTEX presents an opportunity to provide an information base by which damage assessment can be " calibrated" (this work is not presently planned by VORTEX investigators, however). That is, the traditional F-scale approach to rating tornadic intensity is the present tool we use for assessing tornado intensity. It has been a topic of considerable debate, because damage assessment after the fact is the convolution of the tornadic winds with the objects in the damage swath. Much of the debate is associated with the rating system, which is keyed to typical frame homes as the baseline for assessment of tornado intensity. The construction details of structures affected by the tornado are typically not known, and the meteorologists who do much of the F-scale rating usually are not familiar with engineering. Moreover, not all tornadoes hit frame homes, and may not hit a frame home when at their peak intensity. There is relatively little information relating other forms of damage (trees being stripped of branches, objects driven into other objects, etc.) to tornadic intensity. Further, the F-scale system attempts to relate estimated windspeeds to the damage. These windspeeds have never been subjected to a systematic validation; they simply are estimates of the windspeeds required to do a given amount of damage and originally were intended to be an extension to the subjective Beaufort windspeed scale.

We propose to meld the various windspeed measurements taken during the tornado\qs life cycle with the information from a detailed damage survey. This will provide information about as much of the windfield as we have sampled and analyzed, not just the peak windspeed in the storm. We do not expect to provide answers to all the questions regarding F-scale ratings, but we hope to begin a process of using direct observations of tornadic windspeed to relate to damage observations of all sorts, not just to the standard frame home. It is hoped that this data base will provide useful guidance to interpreting damage in situations where the resources of a field experiment are not available.

It is our intent that we provide a range of estimates based on information that may or may not be available in operational damage assessment. This will provide the rating official with some sense of how to use the available input to make an assessment. We also are urging the national F-scale rating data base to include as part of the rating an indication of the method(s) used in arriving at the F-scale rating. Techniques include, but may not be limited to, the following.

If possible, the day after the field teams intercept a storm that produces wind damage, a survey will be organized. The turtles team, mobile labs, and mobile mesonets will meet in the morning at the regular 0930 LT briefing/debriefing and establish a plan of routes that will be surveyed by each team. Only those teams that are actually required, based on the extent of area affected by tornadoes that were observed by VORTEX, will be used. The NOC will make contact with local law enforcement and disaster preparedness officials to obtain approval for the teams to be in the disaster area. The routes will then be driven and/or walked, with all damage documented in detail in order to produce maps of the damage swaths.

All participants are urged to study the publication " A Guide to Conducting Convective Windstorm Studies" by Bunting and Smith. Several copies of this guide will be available from the FC and taken to the field.

Engineering studies

If damage occurs to a structure that was probably designed to certain engineering specifications, such as a business, church, school, etc., we will immediately notify Jim McDonald and/or Richard Peterson at Texas Tech University. If such damage is suspected based on field team observations during intercept work, the FC should be notified, who will notify the Texas Tech researchers.

Lofting and Debris Deposition

Acquiring much of the data regarding debris deposition will depend on " leads" generated through the media and local governmental agencies.

Prior to the beginning of this experiment, letters will be sent to the following groups informing them of the purpose of the experiment, and soliciting their cooperation in the event of a damaging tornado:

/BODY>These individuals would be encouraged to mention our experiment and needs at spotter training sessions and other meetings.

If a damaging tornado occurs, the individuals above would be sent a questionnaire, and postage-paid envelope. The questionnaire will seek information regarding debris deposition and the names and phone numbers of others who might have helpful information. Additional questionnaires will be mailed to individuals mentioned in newspaper clippings and other media reports. Other contacts and personal visits will be made as appropriate based on the information gathered through the contacts and mailings.

In addition, a toll-free telephone number will be established and widely publicized so that persons finding debris from a damaging tornado can call and report the nature and location of the debris. Field survey teams, directed by John Snow of OU, will travel into the areas of debris deposition and document all identifiable pieces. Information regarding debris deposition will be synthesized into detailed maps and archived for later research.

Aerial Surveys

Aerial surveys will be arranged and conducted in an ad hoc manner in VORTEX-95. Decisions regarding the logistics and need for these surveys will be discussed at the daily debriefing at 0930 LT, NSSL Main Conference Room. For a significant event, NOAA has agreed to operate one of its photogrammetry aircraft to obtain large-format, high-resolution images of the damage path. This survey will be arranged by contacting Dr. Joe Golden directly; he will manage the rest of the logsitical details. Interested individuals should contact Erik Rasmussen for updated information.

Return to Table of Contents