EGU22-9649
https://doi.org/10.5194/egusphere-egu22-9649
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Investigating extreme precipitation in tropical squall lines

Sophie Abramian1, Caroline Muller2, and Camille Risi1
Sophie Abramian et al.
  • 1Laboratoire de Météorologie Dynamique, ENS Géosciences, France (sophie.abramian@gmail.com)
  • 2Institute of Science and Technology Austria (IST Austria), Klosterneuburg, Austria

Squall lines are the consequence of the interaction of low-level shear with cold pools associated with convective downdrafts, and beyond a critical shear, squall lines tend to orient themselves. It has been shown that this orientation has the effect of reducing the incoming wind shear to the squall line and maintains equilibrium between wind shear and cold pool spreading (Abramian et al 2021).

While the mechanisms behind squall line orientation seem to be increasingly well understood, few studies have focused on the implications of this organization. Yet, Roca and Fiolleau 2020 shows that mesoscale convective systems, including squall lines, are disproportionately involved in rainfall extremes in the tropics. One may then question whether the orientation of squall lines has an impact on the rainfall extremes, and if so, how and why.

Using a CRM, we perform simulations of tropical squall lines by imposing a vertical wind shear in radiative convective equilibrium. Our results show that the extreme precipitation in the squall lines is more intense in the critical organized case. It seems that when the condensation rate increases with the shear, the precipitation efficiency decreases strongly. The critical case appears to be the most favorable compromise between these two contributions, a hypothesis that we further investigate here.

How to cite: Abramian, S., Muller, C., and Risi, C.: Investigating extreme precipitation in tropical squall lines, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-9649, https://doi.org/10.5194/egusphere-egu22-9649, 2022.

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