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Purpose:
Test the sensitivity of the coupled simulation to the thickness of the uppermost layer in MOM6.
Description:
Motivated by experiment with POP 542 that showed less warming south of the equator in the eastern tropical Pacific and correspondingly improved double ITCZ. One of the major differences between MOM and POP is the vertical resolution in the upper ocean. This run is the same as 091 533 but with dz[0]=10.0 rather than dz[0]=2.5. A zstar case was chosen for more straightforward changes in dz.
Case directory:
Locally (if still available): /glade/u/home/bryan/bryan-work/cesm3.runs/b.e23_alpha17f.BLT1850.ne30_t232.091-10m
On github:
Sandbox:
Locally (if still available): //glade/work/gmarques/cesm.sandboxes/cesm2_3_alpha17f
Purpose:
Test the sensitivity of the coupled simulation to the thickness of the uppermost layer in MOM6.
Description:
Motivated by experiment with POP 542 that showed less warming south of the equator in the eastern tropical Pacific and correspondingly improved double ITCZ. One of the major differences between MOM and POP is the vertical resolution in the upper ocean. This run is the same as 091 533 but with dz[0]=10.0 rather than dz[0]=2.5. A zstar case was chosen for more straightforward changes in dz.
Case directory:
Locally (if still available):
/glade/u/home/bryan/bryan-work/cesm3.runs/b.e23_alpha17f.BLT1850.ne30_t232.091-10m
On github:
Sandbox:
Locally (if still available):
//glade/work/gmarques/cesm.sandboxes/cesm2_3_alpha17f
On github: https://github.com/ESCOMP/cesm/tree/cesm2_3_alpha17f
Diagnostics:
Output:
/glade/u/home/bryan/scratch/archive/b.e23_alpha17f.BLT1850.ne30_t232.091-10m
Contacts:
@fobryan3
Extra details:
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