12 |
done offline. A good approximation of the pressure load anomaly is |
done offline. A good approximation of the pressure load anomaly is |
13 |
necessary to avoid large initial adjustment processes underneath |
necessary to avoid large initial adjustment processes underneath |
14 |
deep-reaching shelfice. |
deep-reaching shelfice. |
15 |
- small fix in shelfice_thermodynamics |
- small fix in ISOMIP shelfice_thermodynamics |
16 |
|
- add more sophisticated thermodynamics of Hellmer (1989), this is |
17 |
|
now the default |
18 |
|
- give a few constants more intuitive names |
19 |
o add code to balance EmPmP and Qnet at the end of do_ocean_physics. Useful |
o add code to balance EmPmP and Qnet at the end of do_ocean_physics. Useful |
20 |
if bulk formulae are used in long integration (especially EmPmR). Turn |
if bulk formulae are used in long integration (especially EmPmR). Turn |
21 |
on with balanceEmPmR = .true. or balanceQnet = .true. in data, PARM01 |
on with balanceEmPmR = .true. or balanceQnet = .true. in data, PARM01 |