WesternWRF
New member
Good day,
I am a seasoned WRF user but never at high resolutions with cu physics turned off. I have performed a case study simulation over Nepal for a convective event. I'm using V3.9 and have 3 domains (12km/4km/1km) and I am using ndown to complete (also a new approach for me).
The issues I am having is relating the convective structures present in the model with the resulting precipitation. With cu_phys turned off, I am only looking at RAINNC for precip (although I confirmed RAINC contained zero fields).
Precipitation values are quite small (on the order of a few mm) for the intensity of convection as shown by max dbz fields and omega fields interpolated to various pressure levels. The spatial patterns just don't seem to match up and there are areas that see no precip despite an active and intense storm overhead.
I'm attaching both my namelist.input files (altered a bit to best represent the complete ndown process) and a pdf showing a snippet of output for a few hours of model time plotting max dbz (top), model accumulated precip (middle; mm), and 500-mb omega (bottom). In the dbz panel, there is a black dot representing Kathmandu's location for spatial context.
I'm hoping someone might be able to serve as a sanity check that there isn't some glaring issue with my namelist that would lead to the model's microphysics not translating into precipitation. I'm under the assumption that when cu_physics is off, the model's microphysics is responsible for all of the precip but maybe I'm missing another field in addition to RAINNC? The model produced the convective event just about perfectly so after my initial pleasure on that I need to make sure I didn't miss some small detail that is translating to poor precip performance (and all the subsequent model interactions).
I am a seasoned WRF user but never at high resolutions with cu physics turned off. I have performed a case study simulation over Nepal for a convective event. I'm using V3.9 and have 3 domains (12km/4km/1km) and I am using ndown to complete (also a new approach for me).
The issues I am having is relating the convective structures present in the model with the resulting precipitation. With cu_phys turned off, I am only looking at RAINNC for precip (although I confirmed RAINC contained zero fields).
Precipitation values are quite small (on the order of a few mm) for the intensity of convection as shown by max dbz fields and omega fields interpolated to various pressure levels. The spatial patterns just don't seem to match up and there are areas that see no precip despite an active and intense storm overhead.
I'm attaching both my namelist.input files (altered a bit to best represent the complete ndown process) and a pdf showing a snippet of output for a few hours of model time plotting max dbz (top), model accumulated precip (middle; mm), and 500-mb omega (bottom). In the dbz panel, there is a black dot representing Kathmandu's location for spatial context.
I'm hoping someone might be able to serve as a sanity check that there isn't some glaring issue with my namelist that would lead to the model's microphysics not translating into precipitation. I'm under the assumption that when cu_physics is off, the model's microphysics is responsible for all of the precip but maybe I'm missing another field in addition to RAINNC? The model produced the convective event just about perfectly so after my initial pleasure on that I need to make sure I didn't miss some small detail that is translating to poor precip performance (and all the subsequent model interactions).