Well, I have about similar case. There is a x=60m, y=20m (periodic boundaries), z=30m case with a 30 MW/m "line" fire that is consisting close to 50 separate tree trunks (HRRPUA boundary condition). Three different cases for the wind (dx=dy=dz=0.25m):
v1: "Open sky"
&VENT PBX= 0.0, SURF_ID='WallOfWind', COLOR='BLUE', OUTLINE=.TRUE. /
&SURF ID='WallOfWind', PROFILE='ATMOSPHERIC',
VEL=-5.0, Z0=5.0, PLE=0.3 /
&VENT PBX=60.0, SURF_ID='OPEN' /
&VENT PBY= 0.0, SURF_ID='PERIODIC FLOW ONLY', COLOR='CYAN', OUTLINE=.TRUE. /
&VENT PBY=20.0, SURF_ID='PERIODIC FLOW ONLY', COLOR='CYAN', OUTLINE=.TRUE. /
&VENT PBZ= 0.0, SURF_ID='GROUND' /
&VENT PBZ=30.0, SURF_ID='OPEN' /
v2: "free slip and vel_grad=0 sky"
&VENT PBX= 0.0, SURF_ID='WallOfWind', COLOR='BLUE', OUTLINE=.TRUE. /
&SURF ID='WallOfWind', PROFILE='ATMOSPHERIC',
VEL=-5.0, Z0=5.0, PLE=0.3 /
&VENT PBX=60.0, SURF_ID='OPEN' /
&VENT PBY= 0.0, SURF_ID='PERIODIC FLOW ONLY', COLOR='CYAN', OUTLINE=.TRUE. /
&VENT PBY=20.0, SURF_ID='PERIODIC FLOW ONLY', COLOR='CYAN', OUTLINE=.TRUE. /
&VENT PBZ= 0.0, SURF_ID='GROUND' /
&VENT PBZ=30.0, SURF_ID='Sky' /
&SURF ID='Sky', COLOR='MAGENTA', VEL_GRAD=0.0, FREE_SLIP=T /
v3: M-O similarity
L=1000000.0 neutral => no T(z) => corresponds to wall of wind inputs
Z_0=0.0002 => sea => corresponds to wall of wind inputs
&WIND SPEED=5.0, Z_REF=5.0, DIRECTION=270.0, L=1000000.0 , Z_0=0.0002 /
&VENT PBX= 0.0, SURF_ID='OPEN' /
&VENT PBX=60.0, SURF_ID='OPEN' /
&VENT PBY= 0.0, SURF_ID='PERIODIC FLOW ONLY', COLOR='CYAN', OUTLINE=.TRUE. /
&VENT PBY=20.0, SURF_ID='PERIODIC FLOW ONLY', COLOR='CYAN', OUTLINE=.TRUE. /
&VENT PBZ= 0.0, SURF_ID='GROUND' /
&VENT PBZ=30.0, SURF_ID='OPEN' /
All cases are run just with the wind and wind+fire (file names correspondinly v1, v1fire, v2, v2fire, v3, v3fire).
&RADI RADIATION=.FALSE. / no fire test case
&PRES VELOCITY_TOLERANCE=0.001, MAX_PRESSURE_ITERATIONS=100 /
I have done also v3 with radiation, but same results. And the PRES I have, because some of cases had numerical instability without it, but the cases look same with and without PRES (as long as the without PRES did run).
The figure below are in the order:
v1
v2
v3
v1fire
v2fire
v3fire
Show are: HRRPUV (Smokeview orange color, does not show up very well in the figures) and velocity (magnitude) SLCF and black is 5.0 m/s there, which is the wind speed in the inputs at the elevation of 5m.
I did also the cases with 15 m/s first, but with similar results ==> something seemed to be wrong ==> reduced the wind speed to 5 m/s. And I have run the 5 m/s cases v1fire and v2fire using both 90m and 150m z_max. I have not checked them yet, they are downloading slowly from the Linux cluster to my laptop (I'm remote working still due to covid situation). But I would say that the v1 and v2 cases do not change much due to the z_max. But I'm just checking there how much sky I should add to the "wall of wind" model that I will be using in actual cases. This is just a test case that was done some 15 years ago by someone else than me. I.e, I was trying to check if I'm able to get the old results. Not to check how FDS has changed during the years, the aim was more or less to validaty myself (Am I able to do this kind of simulations?).
Something that I can see form the figures below: The v1 case (wall of wind with open sky) is not too good with z_max=30m. The fire plume (whole y range line source) is pushing the incoming air upwards to escape from the OPEN boundary. The v2 case performs better with the free slip and vel_grad at the sky. I would expect, that the v1 and v2 cases would be closer to each other, when I see the z_max = 90 and 150 m cases.
The v3 (M-O) case does something that is wrong. It pushes the flames along the ground (horizontally) towards the building. This is clearly seen in the temperature slice (not attached) and also the HRRPUA (orange color in Smokeview). The HRRPUA is "in the three trunk" region and next to it on the right side, it does not rise upwards at all. In the v1 and v2 cases HRRPUA is along the fire plume, the velocity slice shows it similarly as the temperature slice (not atttached here).
Wbr,
Timo