Editorial Type:
Article
Article Type:
Research Article

Finescale Structure of the LaGrange, Wyoming, Tornado during VORTEX2: GBVTD and Photogrammetric Analyses

Roger M. Wakimoto National Center for Atmospheric Research,* Boulder, Colorado

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Phillip Stauffer National Center for Atmospheric Research,* Boulder, Colorado

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Wen-Chau Lee National Center for Atmospheric Research,* Boulder, Colorado

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Nolan T. Atkins Department of Atmospheric Sciences, Lyndon State College, Lyndonville, Vermont

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Joshua Wurman Center for Severe Weather Research, Boulder, Colorado

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Print Publication:
01 Nov 2012
DOI:
https://doi.org/10.1175/MWR-D-12-00036.1
Page(s):
3397–3418
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Abstract

A ground-based velocity track display (GBVTD) analysis of the LaGrange, Wyoming, tornado on 5 June 2009 during the Second Verification of the Origins of Rotation in Tornadoes Experiment (VORTEX2) is photogrammetrically combined with a series of pictures of the funnel cloud. This analysis reveals the relationship between the vertical velocity, radial and tangential velocities, perturbation pressure, vertical vorticity, and angular momentum with the visual features of the tornado. An intense axial downdraft was evident and was supported by a downward-directed perturbation pressure gradient. The radial inflow at low levels was weak and difficult to retrieve owing to a combination of centrifuging of hydrometeors/debris in the intense circulation and the inability of the radar beam to fully resolve the flow. The tornado was weakening during the analysis period, which was supported by angular momentum being advected out of the tornado.

The availability of a dual-Doppler wind synthesis for this tornadic event provided a unique opportunity to assess the assumptions in the GBVTD methodology. The analysis suggests that the simplified GBVTD equations that have been applied in past studies of tornadoes are not appropriate in the present case. The most accurate retrieval of the radial velocities requires that a higher-order term that is typically neglected be retained. A quantitative assessment of the impact of centrifuging of hydrometeors on the synthesized wind field was attempted. The results suggest that the radial and vertical velocity profile near and within the tornado core can be significantly altered for tornadoes (EF2) that are accompanied by a small radius of maximum wind and relatively weaker low-level inflow.

The National Center for Atmospheric Research is sponsored by the National Science Foundation.

Corresponding author address: Roger M. Wakimoto, NCAR, P.O. Box 3000, Boulder, CO 80307. E-mail: wakimoto@ucar.edu

Abstract

A ground-based velocity track display (GBVTD) analysis of the LaGrange, Wyoming, tornado on 5 June 2009 during the Second Verification of the Origins of Rotation in Tornadoes Experiment (VORTEX2) is photogrammetrically combined with a series of pictures of the funnel cloud. This analysis reveals the relationship between the vertical velocity, radial and tangential velocities, perturbation pressure, vertical vorticity, and angular momentum with the visual features of the tornado. An intense axial downdraft was evident and was supported by a downward-directed perturbation pressure gradient. The radial inflow at low levels was weak and difficult to retrieve owing to a combination of centrifuging of hydrometeors/debris in the intense circulation and the inability of the radar beam to fully resolve the flow. The tornado was weakening during the analysis period, which was supported by angular momentum being advected out of the tornado.

The availability of a dual-Doppler wind synthesis for this tornadic event provided a unique opportunity to assess the assumptions in the GBVTD methodology. The analysis suggests that the simplified GBVTD equations that have been applied in past studies of tornadoes are not appropriate in the present case. The most accurate retrieval of the radial velocities requires that a higher-order term that is typically neglected be retained. A quantitative assessment of the impact of centrifuging of hydrometeors on the synthesized wind field was attempted. The results suggest that the radial and vertical velocity profile near and within the tornado core can be significantly altered for tornadoes (EF2) that are accompanied by a small radius of maximum wind and relatively weaker low-level inflow.

The National Center for Atmospheric Research is sponsored by the National Science Foundation.

Corresponding author address: Roger M. Wakimoto, NCAR, P.O. Box 3000, Boulder, CO 80307. E-mail: wakimoto@ucar.edu
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