Hello,
I am running WRF using LDAPS data (KMA, 1.5 km) as the initial and boundary condition.
Most variables (U10/V10, pressure, winds, precipitation) look reasonable compared to observations, but near-surface temperature (T2) shows a strong cold bias.
My settings:
The issue:
Questions:
Thank you in advance for your help!
I am running WRF using LDAPS data (KMA, 1.5 km) as the initial and boundary condition.
Most variables (U10/V10, pressure, winds, precipitation) look reasonable compared to observations, but near-surface temperature (T2) shows a strong cold bias.
My settings:
- Initial condition: LDAPS (1.5 km)
- Domains: 500 m resolution, 100 × 100 grid (very small domain)
- Start time: 03 KST, with 21 h spin-up, using the following 24 h for analysis
- Physics:
- mp_physics = 8 (Thompson)
- bl_pbl_physics = 2 (MYJ)
- sf_surface_physics = 4 (Noah-MP)
- ra_lw_physics = 4, ra_sw_physics = 4 (RRTMG)
- cu_physics = 0
- sf_urban_physics = 0 (no UCM)
- num_land_cat = 21 (MODIS)
The issue:
- T2 is consistently colder than both LDAPS and observations (especially at night).
- Other variables do not show such a strong bias.
Questions:
- What are the common causes when WRF produces a strong cold bias in T2 while other fields are okay?
- Could the very small domain size (100×100, 500 m) or the start time (03 KST) be contributing to this?
- Would you recommend specific PBL or land-surface scheme changes (e.g., MYNN, UCM) to reduce this bias?
- Are there other diagnostics (HFX, LH, RNET, SWDOWN, LWDOWN, etc.) I should check to understand why T2 is too low?
Thank you in advance for your help!