[MITgcm-support] ETA with making Boussinesq approximations
连展
lianzhan at fio.org.cn
Wed Aug 26 02:05:00 EDT 2009
OH!Im sorry.I have maked a mistake.I mean ETA in a model without Boussinesq approximations
----- Original Message -----
From: 连展
To: MIT讨论组
Sent: Wednesday, August 26, 2009 11:44 AM
Subject: [MITgcm-support] ETA with making Boussinesq approximations
Hi,everyone,
I am trying to study the change of ETA in a model with making Boussinesq approximations.I start from the example experiment "tutorial_global_oce_in_p". However,I find that the model output ETA in pressure coordinates in this experiment.Can I output the ETA in Z-coordinates diretly?
I translated the ETA from pressure coordinates to Z-coordinates by dividing rho(suferface layer)*g,and I found the result is very different from the result of experiment "tutorial_global_oce_latlon".Does "ETA" have the same meaning in this two experiment?How could I get the free-surface_r-anomaly(m) in a model with making Boussinesq approximations?
Thanks!!
lian
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