Changes between Version 7 and Version 8 of DevelopmentActivities/CMIP6/DevelopmentsCMIP6/zo_evaporation


Ignore:
Timestamp:
01/14/16 09:51:09 (5 years ago)
Author:
fwang
Comment:

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  • DevelopmentActivities/CMIP6/DevelopmentsCMIP6/zo_evaporation

    v7 v8  
    145145 SU01Z0MH2: same as SU01Z0MH1, but u* by (2) method [[BR]] 
    146146 
    147  Results are shown in fig. z0mh_s01_mh_jan.pdf  [[BR]] 
     147 Results are shown in fig. z0mh_s01_mh_january.pdf  [[BR]] 
    148148 https://forge.ipsl.jussieu.fr/orchidee/attachment/wiki/DevelopmentActivities/CMIP6/DevelopmentsCMIP6/zo_evaporation/z0mh_s01_mh_january.pdf [[BR]] 
    149149 The impacts of using different u* on temp_sol can be as large as 1-2K for vegetated area. [[BR]] 
    150150 
    151 2. The results by using SU formula with cdrag (neutual) corrected: [[BR]] 
     1512. The results by using SU formula with cdrag (neutral) corrected: [[BR]] 
    152152 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]] 
     153 The model is LMDZ(NPv3.2)+ORCHIDEE(CWRR). It is 1-year nudged simulation after spinup.  [[BR]] 
     154 In the figure, CTL means simulation using trunk. SU means simulation by changing z0m and z0h to SU's formula (same as Nicolas V. did). [[BR]] 
    154155 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 The latent heat flux decreases by ~ 3-6 W/m2 for most regions. [[BR]] 
    156157