EGU2020-7076
https://doi.org/10.5194/egusphere-egu2020-7076
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

The influence of convective momentum transport and vertical wind shear on the evolution of a cold air outbreak

Beatrice Saggiorato1, Louise Nuijens1, A. Pier Siebesma1,2, Stephan de Roode1, Irina Sandu3, and Lukas Papritz4
Beatrice Saggiorato et al.
  • 1TU Delft, GRS, Delft, Netherlands (b.saggiorato@tudelft.nl)
  • 2Royal Netherlands Meteorological Institute (KNMI), The Netherlands
  • 3European Centre for Medium-Range Weather Forecasts (ECMWF), Reading, UK
  • 4Institute for Atmospheric and Climate Science, ETH, Zurich, Switzerland

To study the influence of convective momentum transport (CMT) on wind, boundary layer and cloud evolution in a marine cold air outbreak (CAO) we use Large-Eddy Simulations subjected to different baroclinicity (wind shear) but similar surface forcing. The simulated domain is large enough ( ≈100 × 100 km2) to develop typical mesoscale cellular convective structures.  We find that a maximum friction induced by momentum transport (MT) locates in the cloud layer for an increase of geostrophic wind with height (forward shear, FW) and near the surface for a decrease of wind with height (backward shear, BW). Although the total MT always acts as a friction, the interaction of friction-induced cross-isobaric flow with the Coriolis force can develop super-geostrophic winds near the surface (FW) or in the cloud layer (BW). The contribution of convection to MT is evaluated by decomposing the momentum flux by column water vapor and eddy size, revealing that CMT acts to accelerate sub-cloud layer winds under FW shear and that mesoscale circulations contribute significantly to MT for this horizontal resolution (250 m), even if small scale eddies are non-negligible and likely more important as resolution increases. Under FW shear, a deeper boundary layer and faster cloud transition are simulated, because MT acts to increase surface fluxes and wind shear enhances turbulent mixing across cloud tops. Our results show that the coupling between winds and convection is crucial for a range of problems, from CAO lifetime and cloud transitions to ocean heat loss and near-surface wind variability.

How to cite: Saggiorato, B., Nuijens, L., Siebesma, A. P., de Roode, S., Sandu, I., and Papritz, L.: The influence of convective momentum transport and vertical wind shear on the evolution of a cold air outbreak, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7076, https://doi.org/10.5194/egusphere-egu2020-7076, 2020

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