Dear Jon, dear all,
Many thanks for raising this issue, and for moving the discussion towards the
summary below. Indeed, it is timely to raise this issue. As it happens, within
the European IS-ENES2 project we had a small technical workshop last week
dealing with closely related issues. Among
On 3/21/17 9:20 AM, Jonathan Gregory wrote:
Dear Karl
sea_surface_height_above_geoid
I'm not sure it's true that "In an ocean GCM the geoid is the
surface of zero depth". Many ocean models have an ocean surface
that rises above the geoid in some areas and falls below in other
areas.
Dear Karl
> sea_surface_height_above_geoid
>
> The geoid is a surface of constant geopotential with which mean sea
> level would coincide if the ocean were at rest. (The volume enclosed
> between the geoid and the sea floor equals the mean volume of water
> in the ocean.) In an ocean GCM the
Dear all,
Thank you Alison for all your work on our wave proposal, and thanks for
postponing the table update.
I agree with all of your suggestions, for updated definitions and new
names.
Regards,
Elodie
On 16/03/2017 16:57, alison.pamm...@stfc.ac.uk wrote:
>
> Dear Stephane,
>
>
>
> Thanks