Shear-convection interactions, and orientation of tropical squall lines
| Autor: | Camille Risi, Caroline Muller, Sophie Abramian |
|---|---|
| Rok vydání: | 2021 |
| Předmět: |
Convection
010504 meteorology & atmospheric sciences Magnitude (mathematics) Mechanics 01 natural sciences 010305 fluids & plasmas Shear (sheet metal) Geophysics Orientation (geometry) 0103 physical sciences General Earth and Planetary Sciences Squall line Geology 0105 earth and related environmental sciences |
| Zdroj: | Geophysical Research Letters |
| DOI: | 10.1002/essoar.10507697.1 |
| Popis: | Squall lines are known to be the consequence of the interaction of low-level shear with cold pools associated with convective downdrafts. Also, as the magnitude of the shear increases beyond a critical shear, squall lines tend to orient themselves. The existing literature suggests that this orientation reduces incoming wind shear to the squall line, and maintains equilibrium between wind shear and cold pool spreading. Although this theory is widely accepted, very few quantitative studies have been conducted on supercritical regime especially. Here, we test this hypothesis with tropical squall lines obtained by imposing a vertical wind shear in cloud resolving simulations in radiative convective equilibrium. In the sub-critical regime, squall lines are perpendicular to the shear. In the super-critical regime, their orientation maintain the equilibrium, supporting existing theories. We also find that as shear increases, cold pools become more intense. However, this intensification has little impact on squall line orientation. |
| Databáze: | OpenAIRE |
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