N1850OCBDRDDMS_f09_tn14_ice4_gam288_20181220
Contents
N1850OCBDRDDMS_f09_tn14_ice4_gam288_20181220#
Data storage#
The data is stored on NIRD @ sigma2
/projects/NS2345K/noresm/cases/N1850OCBDRDDMS_f09_tn14_ice4_gam288_20181220
Path to case directory#
on Fram @ sigma2
/cluster/projects/nn2345k/matsbn/NorESM/cases/N1850OCBDRDDMS_f19_tn14_201218
Path to diagnostics#
http://ns2345k.web.sigma2.no/diagnostics/noresm/common/N1850OCBDRDDMS_f09_tn14_ice4_gam288_20181220/
Summary of simulation#
The fist simulation (of many) in the NorESM2-MM spin up tree. No SourceMods included.
Namelist changes compared to repository for CAM6-Nor:
cldfrc_iceopt = 5 -> 4
clubb_gamma_coef = 0.308 -> 0.288
tau_0_ubc = .false. -> .true.
micro_mg_dcs = 500.D-6 -> 5.5e-4
zmconv_c0_lnd = 0.0300D0 -> 0.0200D0
zmconv_c0_ocn = 0.0300D0 -> 0.0200D0
Namelist changes compared to repository for CLM5:
reset_snow = .true.
Simulation specifics#
CESM parent |
CESM2.0.0 |
Parent |
- |
Run type |
startup |
Branch time from parent |
- |
Simulated years |
01-01-0001 - 31-12-0120 |
Compset |
1850_CAM60%PTAERO_CLM50%BGC-CROP_CICE_MICOM%ECO_MOSART_SGLC_SWAV_BGC%BDRDDMS |
Git branch |
featureCESM2-OsloDevelopment |
Git commit |
46a9911 |
Resolution |
f09_tn14 |
Machine |
Fram |
Node allocation#
<entry id="NTASKS">
<type>integer</type>
<values>
<value compclass="ATM">1536</value>
<value compclass="CPL">1536</value>
<value compclass="OCN">91</value>
<value compclass="WAV">300</value>
<value compclass="GLC">1536</value>
<value compclass="ICE">736</value>
<value compclass="ROF">20</value>
<value compclass="LND">780</value>
<value compclass="ESP">1</value>
</values>
<desc>number of tasks for each component</desc>
</entry>
Code modifications (SourceMods)#
Includes the long wave aod error#
Information about the bug: The aerosol long wave calculations used information from the aerosol shortwave interpolation on aerosol size. The result was that aerosol longwave forcing was not included during night. A first estimate based on estimates from AMIP simulation is + 0.03 W/m2. The forcing is not evenly distributed, but mostly focused on Sahara including downstream and the Arabian peninsula. The numbers here are around 1-2 W/m2.
Note this bug was fixed in N1850OCBDRDDMS_f09_tn14_alwfix_sg30_qmnmx_20190314
User name lists#
gamma#
Gamma controls the skewness of Gaussian PDF for the subgrid vertical velocities (used in the Cloud Layers Unified By Binormals (CLUBB) scheme). A low gamma generally increases the amount of low clouds and hence gives a higher short-wave cloud forcing.
iceopt#
Iceopt is used for setting the parameterisation of ice-cloud fraction. The CESM2 default scheme for the parameterisation of the ice-cloud fraction is iceopt = 5, which includes a functional dependence of ice cloud fraction on the environmental relative humidity. In this simulation the iceopt = 4, for which there is no such dependence. This was changed later in N1850OCBDRDDMS_f09_tn14_qmnmxrhmin_20190314
user_nl_cam#
! Users should add all user specific namelist changes below in the form of
! namelist_var = new_namelist_value
&dyn_fv_inparm
fv_am_correction= .true.
fv_am_diag = .true.
fv_am_fix_lbl = .true.
fv_am_fixer = .true.
&phys_ctl_nl
dme_energy_adjust = .true.
&circ_diag_nl
do_circulation_diags = .true.
clubb_history = .false.
history_budget = .false.
history_vdiag = .true.
&zmconv_nl
zmconv_c0_lnd = 0.0200D0
zmconv_c0_ocn = 0.0200D0
zmconv_ke = 8.0E-6
µ_mg_nl
micro_mg_dcs = 5.5e-4
&clubb_params_nl
clubb_gamma_coef = 0.288
&gw_drag_nl
tau_0_ubc = .true.
&cldfrc_nl
cldfrc_iceopt = 4
user_nl_clm#
finidat = '/cluster/shared/noresm/inputdata/cesm2_init/b.e20.B1850.f09_g17.pi_control.all.297/0308-01-01/b.e20.B1850.f09_g17.pi_control.all.297.clm2.r.0308-01-01-00000.nc'
use_init_interp = .true.
reset_snow = .true.
Time series of spinup#
NorESM2-MM spinup simulation
Left column (from top to bottom): Globally and annually averaged Surface (2m) air temperature, global and volume averaged ocean temperature, Sea surface temperature (SST).
Right column (from top to bottom): Globally and annually Globally and annually averaged Net radiation @ top of model, Atlantic meridional oveturning circulation (AMOC) @ 26.5N.
NorESM2-MM spinup simulation
Left column (from top to bottom): Globally and annually sum of Sea salt surface emissions, DMS (dimethylsulfide) surface emissions, POM (primary organic matter) surface emissions.
Right column (from top to bottom): Globally and annually averaged shortwave cloud forcing and longwave cloud forcing.