Hi group,
I just recently start using WRF-LES to study buoyant plumes, so I think it is an ideal case.
To study buoyant plumes, we set up a heat-flux from z=0 entering the domains. But the inflow gas has gas constant R=488.92 which is not air, and I think the ambient in the domain is air with R_air=288. So I am wondering what are the physical mechanisms between the inflow and the ambient air?
What is the inflow gas being treated, a new second species, a passive scalar or still just air? Or what happen when the inflow mixes with the air? What R should I use for post-processing?
The input file is attached, our team made some changes to the code so the input file may have additional inputs. I just start learning WRF and I used to develop inhouse DNS.
I just recently start using WRF-LES to study buoyant plumes, so I think it is an ideal case.
To study buoyant plumes, we set up a heat-flux from z=0 entering the domains. But the inflow gas has gas constant R=488.92 which is not air, and I think the ambient in the domain is air with R_air=288. So I am wondering what are the physical mechanisms between the inflow and the ambient air?
What is the inflow gas being treated, a new second species, a passive scalar or still just air? Or what happen when the inflow mixes with the air? What R should I use for post-processing?
The input file is attached, our team made some changes to the code so the input file may have additional inputs. I just start learning WRF and I used to develop inhouse DNS.