TY - JOUR
T1 - Predicting supercell motion using a new hodograph technique
AU - Bunkers, Matthew J.
AU - Klimowski, Brian A.
AU - Zeitler, Jon W.
AU - Thompson, Richard L.
AU - Weisman, Morris L.
PY - 2000/2
Y1 - 2000/2
N2 - A physically based, shear-relative, and Galilean invariant method for predicting supercell motion using a hodograph is presented. It is founded on numerous observational and modeling studies since the 1940s, which suggest a consistent pattern to supercell motion exists. Two components are assumed to be largely responsible for supercell motion: (i) advection of the storm by a representative mean wind, and (ii) propagation away from the mean wind either toward the right or toward the left of the vertical wind shear-due to internal supercell dynamics. Using 290 supercell hodographs, this new method is shown to be statistically superior to existing methods in predicting supercell motion for both right- and left-moving storms. Other external factors such as interaction with atmospheric boundaries and orography can have a pronounced effect on supercell motion, but these are difficult to quantify prior to storm development using only a hodograph.
AB - A physically based, shear-relative, and Galilean invariant method for predicting supercell motion using a hodograph is presented. It is founded on numerous observational and modeling studies since the 1940s, which suggest a consistent pattern to supercell motion exists. Two components are assumed to be largely responsible for supercell motion: (i) advection of the storm by a representative mean wind, and (ii) propagation away from the mean wind either toward the right or toward the left of the vertical wind shear-due to internal supercell dynamics. Using 290 supercell hodographs, this new method is shown to be statistically superior to existing methods in predicting supercell motion for both right- and left-moving storms. Other external factors such as interaction with atmospheric boundaries and orography can have a pronounced effect on supercell motion, but these are difficult to quantify prior to storm development using only a hodograph.
UR - https://www.scopus.com/pages/publications/0034110159
U2 - 10.1175/1520-0434(2000)015<0061:PSMUAN>2.0.CO;2
DO - 10.1175/1520-0434(2000)015<0061:PSMUAN>2.0.CO;2
M3 - Article
AN - SCOPUS:0034110159
SN - 0882-8156
VL - 15
SP - 61
EP - 79
JO - Weather and Forecasting
JF - Weather and Forecasting
IS - 1
ER -