Abstract
The ACSL are discontinuous lines of organized mesoscale cloud clusters that propagate across the central Amazon Basin at speeds of 50-60 km h-1. The ACSL undergo six possible life cycle stages: coastal genesis, intensification, maturity, weakening, reintensification, and dissipation. Analysis also indicates that mesoscale clusters within the ACSL are composed of three distinct cloud components: a prestorm region that often contains towering cumulus, leading edge convection (LEC), and multiple, precipitating cloud layers in the trailing stratiform region (TSR). Divergence and vertical velocity calculations indicate deep vertical ascent in the LEC and a region of midlevel convergence (~500 mb) in the TSR. The latter midlevel convergence is associated with a weak updraft above 500 mb and an unsaturated downdraft below. Vertical motions in the TSR are an order of magnitude smaller than in the LEC. -from Authors
Cite
CITATION STYLE
Garstang, M., Massie, H. L., Halverson, J., Greco, S., & Scala, J. (1994). Amazon coastal squall lines. Part I: structure and kinematics. Monthly Weather Review, 122(4), 608–622. https://doi.org/10.1175/1520-0493(1994)122<0608:ACSLPI>2.0.CO;2
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.