Cumulonimbus vertical velocity events in GATE. Part II: synthesis and model core structure.

188Citations
Citations of this article
36Readers
Mendeley users who have this article in their library.
Get full text

Abstract

By our definition a convective updraft must have a positive vertical velocity for 0.5km, and exceed 0.5 m s-1 for 1 s; a convective updraft core must exceed 1 m s-1 for 0.5km. Downdrafts and downdraft cores are defined analogously. Here the properties of the drafts and cores are compared to results of previous work. In addition, the implications of the results in Part I are discussed.-from Authors Nat. Center for Atmos. Res., Boulder, CO 80307, U.S.A.

Cite

CITATION STYLE

APA

Zipser, E. J., & Lemone, M. A. (1980). Cumulonimbus vertical velocity events in GATE. Part II: synthesis and model core structure. Journal of the Atmospheric Sciences, 37(11), 2458–2469. https://doi.org/10.1175/1520-0469(1980)037<2458:CVVEIG>2.0.CO;2

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free