-
Raphaela Vogel19/05/2022, 09:15Talk
Shallow-convective organization and rain are two sides of the same coin. The mesoscale organization of shallow convection tends to increase rain rates, and rain is an important ingredient for organising shallow convection. Rain induces mesoscale organization preferentially through evaporatively-driven downdrafts, which trigger cold pools that spread out at the surface as density currents. Cold...
Go to contribution page -
Pier Siebesma (Delft University of Technology), Louise Nuijens (TU Delft)19/05/2022, 09:45Talk
It has become clear over the last couple of years that shallow cumulus convection over the subtropical oceans has a strong tendency to develop itself into a rich variety of spatial cloud structures. It is particular challenging to simulate these mesoscale cloud patterns. On the one hand, it requires turbulence resolving resolutions of 100 m to represent the vertical convective mixing processes...
Go to contribution page -
Benjamin Fildier (Laboratoire de Météorologie Dynamique, ENS, Paris)19/05/2022, 10:00Talk
In models, a local maximum of clear-sky radiative cooling in the lower troposphere often appears as a necessary condition for the development and persistence of convective organization. However, no robust understanding has been provided for the emergence and disappearance of lower-tropospheric cooling in the atmosphere. Here we propose a theoretical characterization of clear-sky radiative...
Go to contribution page -
Reyk Börner (University of Reading)19/05/2022, 10:15Talk
The diurnal variability of sea skin temperature (SST) is suspected to play an important role for convective organization above the tropical ocean, from driving cumulus congestus convection to triggering the active phase of the Madden-Julian Oscillation. Recent cloud-resolving simulations demonstrate how imposed diurnal SST oscillations strongly impact mesoscale convective aggregation,...
Go to contribution page
Choose timezone
Your profile timezone: