| 143 | The simulations are:[[BR]] |
| 144 | SU01Z0MH1: replace z0m and z0h by SU formula, u* by (1) method [[BR]] |
| 145 | SU01Z0MH2: same as SU01Z0MH1, but u* by (2) method [[BR]] |
| 146 | |
| 147 | Results are shown in fig. z0mh_s01_mh_jan.pdf [[BR]] |
| 148 | https://forge.ipsl.jussieu.fr/orchidee/attachment/wiki/DevelopmentActivities/CMIP6/DevelopmentsCMIP6/zo_evaporation/z0mh_s01_mh_january.pdf [[BR]] |
| 149 | The impacts of using different u* on temp_sol can be as large as 1-2K for vegetated area. [[BR]] |
| 150 | |
| 151 | 2. The results by using SU formula with cdrag (neutual) corrected: [[BR]] |
| 152 | https://forge.ipsl.jussieu.fr/orchidee/attachment/wiki/DevelopmentActivities/CMIP6/DevelopmentsCMIP6/zo_evaporation/z0mh_SU.pdf [[BR]] |
| 153 | In the figure, CTL means simulation using trunk. SU means simulation using SU formular (same as Nicolas V.). [[BR]] |
| 154 | The Ts increases by ~0.5K for most regions with the maximum increases being 1-1.5 K (JJA over desert). [[BR]] |
| 155 | The latent heat flux decreases by ~3W/m2 for most regions. [[BR]] |
| 156 | |