Rg. Fovell et Ps. Dailey, THE TEMPORAL BEHAVIOR OF NUMERICALLY SIMULATED MULTICELL-TYPE STORMS .1. MODES OF BEHAVIOR, Journal of the atmospheric sciences, 52(11), 1995, pp. 2073-2095
The temporal behavior of mature multicellular model storms, created in
an experiment that varied the vertical wind shear layer depth, is exa
mined herein. These storms form new cells at low levels on the storm's
forward side, in or near the forced lifting zone at the edge of the e
vaporationally chilled subcloud cold-air pool. Each moves upward and r
earward within the storm as it intensifies, matures, and decays and be
comes replaced by a new cell development. As a result, the storms osci
llate in time with respect to updraft intensity and the generation of
condensation and surface rainfall. A few model storms oscillate in a s
imply periodic fashion during maturity, generating a series of nearly
identical cells separated by a nearly constant period. Other storms ar
e still periodic but in a more complex fashion, manifesting repeat cyc
les consisting of two or more cells. Several simulations appear quite
aperiodic. Spectral analyses of temporal statistics reveal the existen
ce of a fundamental period of oscillation in every (simple or complex)
periodic case. Further, this period varies little among the simulatio
ns in the present experiment and averages about 15 minutes, a realisti
c cell production period according to observations. In this paper, the
authors examine the various modes of mature storm behavior, laying th
e foundation for a discussion of the forcings and factors responsible
for determining the period and temporal behavior of multicell-type sto
rms to come in future work.