contributor author | Lin, Yuh-Lang | |
contributor author | Deal, Roy L. | |
contributor author | Kulie, Mark S. | |
date accessioned | 2017-06-09T14:35:04Z | |
date available | 2017-06-09T14:35:04Z | |
date copyright | 1998/05/01 | |
date issued | 1998 | |
identifier issn | 0022-4928 | |
identifier other | ams-22190.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4158613 | |
description abstract | In this study, mechanisms of cell regeneration, development, and propagation within a two-dimensional multicell storm are investigated using a numerical cloud model. The cell regeneration is explained by the advection mechanism. The following processes occur periodically during cell regeneration: (i) Near the edge of the gust front, the gust front updraft is formed by low-level convergence ahead of the gust front near the surface. (ii) The upper portion of the gust front updraft grows by midlevel inflow since the gust front propagates faster than the basic wind. (iii) The growing cell tends to produce and is flanked by strong compensating downdrafts. The upstream downdraft tends to cut off the growing cell from the gust front updraft. It is found that the period of cell regeneration is inversely proportional to the midlevel, strong relative wind speed. This advection mechanism is different from that proposed by Yang and Houze, which views the rearward propagating cell as gravity waves generated by the quasi-steady updraft moving through the ambient flow. Cell development and propagation within a two-dimensional multicell storm may be described in terms of two distinctive modes: (i) a growing mode and (ii) a propagating mode. When a growing cell reaches its maximum intensity, it splits and then propagates downstream without amplification. The dynamics of cell development and propagation is explained here by critical level argument. For the growing mode there is growth because of a conditionally unstable environment leading to steering level propagation, while for the propagating mode there is no growth because of a more stable environment leading to propagation relative to the flow (i.e., absence of critical level). It is found that the phase relationship between w? and ?? (w? and u?) in the growing mode is different from that in the propagating mode and can be explained by the dominance of latent heating in the thermodynamic equation. The propagating mode is dominated by horizontal advection. The propagating mode exhibits gravity wave properties and propagates faster than the growing mode. | |
publisher | American Meteorological Society | |
title | Mechanisms of Cell Regeneration, Development, and Propagation within a Two-Dimensional Multicell Storm | |
type | Journal Paper | |
journal volume | 55 | |
journal issue | 10 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1998)055<1867:MOCRDA>2.0.CO;2 | |
journal fristpage | 1867 | |
journal lastpage | 1886 | |
tree | Journal of the Atmospheric Sciences:;1998:;Volume( 055 ):;issue: 010 | |
contenttype | Fulltext | |