VORTEX2: Damage Survey and Photogrammetric Analyses of Tornadoes, Mesocyclones, and Hook Echoes Observed during VORTEX II

Lyndon State College, Lyndonville VT

Investigators

Abstract

This award is one component of a mutli-investigator effort known as the Verification of the Origins of Rotation in Tornadoes Experiment 2 (VORTEX 2). VORTEX 2 is a follow on to VORTEX 1 whose field phase was conducted during the Spring of 1994 and 1995. The VORTEX 1 advanced knowledge of the kinematic structures of tornadic and non tornadic storms and provided some hints as to the sensitivity of the evolution of supercell storms and tornadogenesis to very fine spatial scale heterogeneity. The VORTEX 2 research objectives will focus on the genesis and maintenance of tornadoes and on the structure of the near wind field of the tornado. The VORTEX 2 is being conducted in conjunction with the National Oceanic and Atmospheric Administration and it will involve an unprecedented observational network of stationary and mobile facilities that include Doppler radars, surface and upper air observations. . The Principal Investigators will perform detailed ground and aerial damage surveys and collect high-resolution photographic data of tornadic storms during the VORTEX II. This data will be combined with high-resolution, ground-based radar data to address the following three objectives. The first objective is to better understand the relationship between the tornado and its parent circulation. Specifically, the time evolution of tornado, mesocyclone, and damage intensities will be examined. Previous studies suggest both strong and weak correlations between tornado and mesocyclone strength. The causes of nonlinear surface damage patterns such as trochoidal and scalloping marks, left and right turns, and sinusoidal patterns documented in past damage survey data will also be explored. These patterns have been attributed to single or multiple vortices orbiting around the parent circulation. Surprisingly, no previous study has verified the visual characteristics of suction vortex and trochoidal marks in surface damage. Recent high-resolution mobile Doppler radar data sets have revealed intriguing single-Doppler velocity features, multi-parameter signatures, and reflectivity features such as weak echo eyes and debris rings within the hook echo of tornadic supercells. The second objective will be to superimpose damage survey and cloud photography data onto these radar features. Such an analysis will further understanding of the relationship between the visual characteristics of the tornado and attendant debris cloud, damage, and the radar-detected features within the hook echo. Finally, it has been shown that ground based Doppler radars at close range to large tornadoes are able to sample the flow within and around the tornado. The third objective is to examine the relationship between radar-detected wind speeds with wind speed estimates based on the Enhanced Fujita (EF) scale assessments. Such an analysis will verify the wind speeds associated with the various degrees of damage for a given damage indicator and potentially identify new damage indicators. The analysis will also examine the correlation of different wind intensity metrics such as highest wind gusts, duration of intense winds, time integrated wind speeds, and local accelerations with observed damage intensity. Intellectual Merit Realizing the above objectives will further understanding of the relationship between the mesocyclone, tornado, and attendant surface damage intensity and damage patterns. Superposition of photography and damage survey data onto high-resolution radar data will allow proper interpretation of intriguing features observed within the hook echo region. It is also anticipated that a better understanding of how tornadic flow creates observed damage will result from this research along with refinements to the newly adopted EF scale. Broader Impacts The research results will have important operational implications for the tornado detection and warning process. A better understanding of the relationship between the mesocyclone and tornado will be very useful in the tornado warning process. An improved understanding of the single-Doppler data within the hook echo may lead to tornadic precursors or identifiable features when the tornado is producing damage at the surface. Any modifications to the EF scale will improve the accuracy of the United States tornado climatology. The research will also expose undergraduate students to the data collection process during a major field experiment and the subsequent analysis. The work will enhance the research infrastructure at Lyndon State College (LSC) and the knowledge gained will be incorporated into many of the undergraduate classes taught at LSC.