Thermal plume model Generic PCM
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Contents
Description of the Thermal plume model
Implementation in the Generic PCM
Code
Edition history
Authors: F. Hourdin, C. Rio, A. Mathieu, A. Boissinot, A. Le Saux
Version du 09.02.07
Calculation of vertical transport in the boundary layer in the presence of explicitly represented “thermals” with cloud processes
Rewriting from a paper listing in Habas, 14/02/00
Thermal energy is assumed to be homogeneous and dissipated by mixing with its surroundings.
The length l_mix controls the mixing efficiency.
The transport of the different species is calculated by taking into account:
1. upward mass flux
2. downward mass flux
3. entrainment
4. a detrainment
Modif 2013/01/04 (FH hourdin@lmd.jussieu.fr)
Introduction of an implicit computation of vertical advection in the environment of thermal plumes in thermcell_dq
impl = 0 : explicit ; impl = 1 : implicit ; impl =-1 : old version
controled by iflag_thermals =
15, 16 run with impl=-1 : numerical convergence with NPv3
17, 18 run with impl=1 : more stable
15 and 17 correspond to the activation of the stratocumulus "bidouille"
Major changes 2018-19 (AB alexandre.boissinot@lmd.jussieu.fr)
New detr and entre formulae (no longer alimentation) lmin can be greater than 1 Mix every tracer Can stack verticaly multiple plumes (it makes thermcell_dv2 unusable for the moment)
Modif 2024 (ALS, arthur.le-saux@lmd.ipsl.fr)
Implementation to take into account generic tracers
How to use it?
In a 1D rcm1d run
The TPM is activated in callphys.def with
calltherm = .True.
Remember to also turn off the convective adjustment scheme to use only one parametrisation of convection
calladj = .True.
Then, several options may be used to tune the model
dvimpl = .False. dqimpl = .True. r_aspect_thermals = 2.0 tau_thermals = 0.0 betalpha = 0.9 afact = 0.9 fact_epsilon = 1.e-4 alpha_max = 0.7 fomass_max = 0.5 pres_limit = 1.e3 nu = 0.0
