Abstract
The key assumption underlying convection parameterizations is that rising plumes develop in a horizontally homogeneous environment. With this in mind, we investigate the impact of environmental cloud layer heterogeneities on shallow convection using large-eddy simulation that applies a master-slave methodology. In the master-slave approach, two independent sets of thermodynamic variables (master and slave) are driven by one dynamics (coupled with the master) to remove the impact of internal variability of the dynamical system considered. The two thermodynamic sets include either a realistic heterogeneous environment or an environment that is homogenized outside clouds. The key is that homogenization also excludes subsiding shells surrounding cumulus clouds. The results show a small impact of the homogenization on cloud field properties. The physical explanation highlights the role of the subsiding shell shielding a shallow cumulus cloud from its environment.
| Original language | English |
|---|---|
| Pages (from-to) | 1785-1793 |
| Number of pages | 9 |
| Journal | Geophysical Research Letters |
| Volume | 46 |
| Issue number | 3 |
| DOIs | |
| State | Published - Feb 16 2019 |
| Externally published | Yes |
Keywords
- heterogeneous environment
- homogeneous environment
- parameterization assumption
- shallow convection