Supercell Motion, Supercell Longevity, and Hodograph Resources

Bounded Weak Echo Region (BWER) 

Background Material

Supercell motion has remained an interesting topic since the 1940s when the documentation of these storms was in its infancy.  The feature that sets supercells apart from ordinary thunderstorms is the presence of deep and persistent rotation (counterclockwise for right-moving storms and clockwise for left-moving storms, irrespective of hemisphere).  This rotation induces a propagation component which is at right angles to the vertical wind shear (and not the mean wind).  This sometimes can lead to a supercell motion that is at significant angles to the mean wind, and in a few instances, supercells have been observed to move "upstream" against the mean flow.  As a result of these observations, and along with inspiration from the COMET module, "Anticipating Convective Storm Structure and Evolution," we began research in 1996 to further study the behavior of supercell motion, with a goal of being able to better predict supercell motion prior to storm formation.  Our results support many of the previous theoretical and modeling studies, which indicate that supercell motion is primarily determined by advection plus rotationally induced propagation across the vertical wind shear.  Studies by Ramsay and Doswell (2005) and Thomson et al. (2007) have supported our work.  We also note that thermodynamics may play a noteworthy role in modulating supercell motion on occasion, and recent modeling work sheds some light on this topic (Kirkpatrick et al. 2007).  After completing the above storm motion project, we looked at the vertical wind shear in environments of both right- and left-moving supercells (Bunkers 2002).  We found that the bulk and total wind shear are similar for the two classes, but the absolute value of storm-relative helicity is larger for right-moving supercells, relative to the left-movers, across the United States.

Contact:  If you have questions or comments about supercell motion, supercell longevity, or any of the other references listed on this page, please e-mail Matthew Bunkers, the Science and Operations Officer at the National Weather Service (NWS) in Rapid City, SD.

 

Latest Papers

Bunkers, M. J., D. A. Barber, R. L. Thompson, R. Edwards, and J. Garner, 2014: Choosing a universal mean wind for supercell motion prediction. J. Operational Meteor., 2 (11), 115–129, doi: http://dx.doi.org/10.15191/nwajom.2014.0211Click here for a PDF.

Bunkers, M. J., and M. A. Baxter, 2011:  Radar tornadic debris signatures on 27 April 2011. Electronic J. Operational Meteor., 12 (7), 1–6.

* This is the inaugural issue of the "Images of Note" category for the National Weather Association (NWA) Electronic Journal of Operational Meteorology (EJOM).

 

Hodographs & 2005 Virtual Institute for Satellite Integration Training (VISIT) Teletraining

a)  Hodograph (with SRH contours)
b)  Hodograph (with storm-relative winds)
c)  Hodograph (with 250-m spacing)
d)  Supercell Motion Teletraining (includes audio playback version)
e)  Predicting Supercell Motion in Operations (standalone PPT)

 

Formal Publications 

 

Informal Publications

  • Bunkers, M. J., 1996a:  Examination of the preconvective environment associated with a severe nontornadic supercell:  Variations in CAPE and SREH. Preprints, 18th Conf. on Severe Local Storms, San Francisco, CA, Amer. Meteor. Soc., 703–707.
  • Bunkers, M. J., 1996b:  On the use of the WSR-88D during situations of rapidly developing severe thunderstorms. NOAA/NWS WFO Rapid City, SD , Internal Report, 6 p.
  • Bunkers, M. J., 2002:  A new convective sounding analysis program for AWIPS. Preprints, 18th International Conference on Interactive Information and Processing Systems (IIPS), Orlando, FL, Amer. Meteor. Soc., 209–210.
  • Bunkers, M. J., 2010:  How midlevel horizontal humidity gradients affect simulated storm morphology. Preprints, 25th Conf. on Severe Local Storms, Denver, CO, Amer. Meteor. Soc., P7.1.
  • Bunkers, M. J., and J. W. Zeitler, 2000:  On the nature of highly deviant supercell motion. Preprints, 20th Conf. on Severe Local Storms, Orlando, FL, Amer. Meteor. Soc., 236–239.
  • Bunkers, M. J., B. A. Klimowski, J. W. Zeitler, R. L. Thompson, and M. L. Weisman, 1998:  Predicting supercell motion using hodograph techniques. Preprints, 19th Conf. on Severe Local Storms, Minneapolis, MN, Amer. Meteor. Soc., 611–614.
  • Bunkers, M. J., B. A. Klimowski, and J. W. Zeitler, 2002:  The importance of parcel choice and the measure of vertical wind shear in evaluating the convective environment. Preprints, 21st Conf. on Severe Local Storms, San Antonio, TX, Amer. Meteor. Soc., 379–382.
  • Bunkers, M. J., J. S. Johnson, J. M. Grzywacz, L. J. Czepyha, and B. A. Klimowski, 2002:  A preliminary investigation of supercell longevity. Preprints, 21st Conf. on Severe Local Storms, San Antonio, TX, Amer. Meteor. Soc., 655–658.
  • Hintz, D. L., and M. J. Bunkers, 1995:  Examination of an apparent landspout in the eastern Black Hills of western South Dakota. NOAA/NWS CR Tech. Attach. 95-08, 11 pp. [Available from NWS Central Region, 601 E. 12th St., Rm 1836, Kansas City, MO  64106-2897.]
  • Lindsey, D. T., and M. J. Bunkers, 2004:  On the motion and interaction between left-moving and right-moving supercells on 4 May 2003. 22nd Conf. on Severe Local Storms, Hyannis, MA, Amer. Meteor. Soc., CD-ROM, 12.2.
  • Yu, X., M. A. Magsig, and M. J. Bunkers, 2002:  Enhancements to a new convective sounding analysis program for AWIPS. Preprints, 21st Conf. on Severe Local Storms, San Antonio, TX, Amer. Meteor. Soc., J77–J80.
  • Zeitler, J. W., and M. J. Bunkers, 2002:  Anticipating and monitoring supercell motion for severe weather operations. Preprints, 21st Conf. on Severe Local Storms, San Antonio, TX, Amer. Meteor. Soc., J61–J64.

 

Presentations 

 

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