THE TEMPORAL BEHAVIOR OF NUMERICALLY SIMULATED MULTICELL-TYPE STORMS - PART-II - THE CONVECTIVE CELL LIFE-CYCLE AND CELL REGENERATION

Authors
Citation
Rg. Fovell et Ph. Tan, THE TEMPORAL BEHAVIOR OF NUMERICALLY SIMULATED MULTICELL-TYPE STORMS - PART-II - THE CONVECTIVE CELL LIFE-CYCLE AND CELL REGENERATION, Monthly weather review, 126(3), 1998, pp. 551-577
Citations number
41
Categorie Soggetti
Metereology & Atmospheric Sciences
Journal title
ISSN journal
00270644
Volume
126
Issue
3
Year of publication
1998
Pages
551 - 577
Database
ISI
SICI code
0027-0644(1998)126:3<551:TTBONS>2.0.ZU;2-0
Abstract
The authors study herein the convective cell life cycle and the cell g eneration process in mature, multicellular squall-line storms possessi ng well-developed subcloud cold pools using two-and three-dimensional models. The multicellular storm establishes new cells on its forward s ide, in the vicinity of the forced updraft formed at the pool boundary , that first intensify and then decay as they travel rearward within t he storm's upward sloping front-to-rear airflow. The principal effort is expended on the two-dimensional case owing to the strong similarity in basic behavior seen in the two geometries. The cell life cycle is examined in several complementary fashions. The cells are shown to be convectively active entities that induce local circulations that alter nately enhance and suppress the forced updraft, modulating the influx of the potentially warm inflow. This transient circulation also drives the episodic mixing of stable air into the inflow that results in the cell's ultimate dissipation. The timing of cell regeneration is also examined; an explanation involving two separate and successive phases, each with their own timescales, is proposed. The second of these phas es can be shortened if a ''convective trigger,'' another by-product of the cell's circulation, is present in the storm's inflow environment. Sensitivity of the results to strictly numerical model details is als o discussed.