Abstract
The first simulation uses liquid water-only microphysics and is denoted as the liquid water model (LWM). The second includes both liquid water and ice microphysics and is designated as the hail category model (HCM). Results from the two simulations show that the inclusion of ice significantly alters the dynamics, kinematics, thermodynamics, and distributions of water in the storm, especially at the lower levels. Supercell features such as a rotating intense updraft, bounded weak-echo region, large forward overhanging anvil, and hooklike structure in the low-level rainwater field are present in both simulations. these features are generally more pronounced, however, and have a longer lifetime in the HCM. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 745-759 |
| Number of pages | 15 |
| Journal | Journal of Applied Meteorology |
| Volume | 32 |
| Issue number | 4 |
| DOIs | |
| Publication status | Published - 1993 |
All Science Journal Classification (ASJC) codes
- Atmospheric Science
Fingerprint
Dive into the research topics of 'Numerical simulations of the 2 August 1991 CCOPE supercell storm with and without ice microphysics'. Together they form a unique fingerprint.Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver