| 570 | == Testing roughness length for heat in LMDZOR == |
| 571 | |
| 572 | 01-Sep-2015 by Fuxing WANG, Frederique CHERUY. [[BR]] |
| 573 | |
| 574 | Background: |
| 575 | The roughness length for heat (z0h) is generally not identical to roughness length for momentum (z0m). [[BR]] |
| 576 | In LMDZOR, z0h = z0m. A short description of related code is (only in coupled mode): https://forge.ipsl.jussieu.fr/orchidee/attachment/wiki/Meetings/CMIP6/Physic/condveg_z0cdrag.pdf [[BR]] |
| 577 | Objective: |
| 578 | To test the sensitively of LMDZOR to z0h.[[BR]] |
| 579 | Simulations: |
| 580 | Two simulations (1-year) were done with LMDZOR after 20 years spin-up.[[BR]] |
| 581 | (1) CTL: z0h = z0m; ORCHIDEE-rev 2664, LMDZ-rev 2287; new soil vertical discretization and soil thermodynamics [[BR]] |
| 582 | (2) EXP: The same as CTL, but z0h = 0.1 * z0m. [[BR]] |
| 583 | Results: |
| 584 | Results are compared over different seasons (annual mean, JJA and DJF): https://forge.ipsl.jussieu.fr/orchidee/attachment/wiki/Meetings/CMIP6/Physic/z0mh_annual_jja_djf.pdf. [[BR]] |
| 585 | The left side in the figures is "CTL: z0h = z0m", the right side is the 'EXP-CTL' (except the last row which is the " EXP/CTL"). [[BR]] |
| 586 | The Ts (temp_sol) increases over most regions. The maximum increase is over 0N-90N in JJA (1-2K), while it is over 30N-60S in DJF (0.5-1.5K).(Fig b) [[BR]] |
| 587 | The pattern of fluxsens is similar for different seasons. It increases over most regions (3 W/m2 for most regions).[[BR]] |
| 588 | The variation of fluxlat (+/- 6 W/m2 over most regions) and precipitation (+/-0.5mm/d over most regions) is less systematic than Ts and fluxsens. [[BR]] |