[MITgcm-support] difference between PH and PHL
Jody Klymak
jklymak at uvic.ca
Mon Aug 5 16:42:42 EDT 2013
Hi All,
On Aug 5, 2013, at 13:24 PM, Nicolas Grisouard <nicolas.grisouard at stanford.edu> wrote:
> I'm going to quote Jean-Michel, who answered this question when I asked it a couple of years ago (Jan. 7 2012 to be specific):
>
> "From those output files, the pressure P can be obtained as:
> P(i,j,k)/rhoConst = -g*rC(k) + PH(i,j,k) + PNH(i,j,k)
Except this isn't quite correct.
> P(i,j,k)/rhoConst = -g*rC(k) + PH(i,j,k) + PNH(i,j,k) + PHref(k)
where PHref(k) is the hydrostatic pressure due to Tref and Sref.
see calc_phi_hyd.F and find_rho.F. Unless I am grossly misunderstanding the code.
Thanks, Jody
>
> And PHL would be the equivalent of PH (hydrostatic pressure potential anomaly)
> but at the bottom, so that the hydrostatic pressure at the bottom Pb
> would be: Pb(i,j)/rhoConst = g*Depth(i,j) + PHL(i,j)
>
> Cheers,
> Jean-Michel"
>
> It's pretty useful, because you don't have to interpolate the hydrostatic pressure on the topography.
> Cheers,
> Nico.
>
> On 05/08/13 06:12, Robert Nazarian wrote:
>> Hi,
>>
>> I'm using the MITgcm internal wave code and analyzing the pressure perturbations. I noticed in the output directory that there are PH and PHL files, which are both hydrostatic pressure files. Can someone elaborate on the difference between the two?
>>
>> Thanks so much,
>> Rob
>>
>> Robert Nazarian
>> Department of Atmospheric and Oceanic Sciences
>> Princeton University
>> rn2 at princeton.edu
>>
>>
>> _______________________________________________
>> MITgcm-support mailing list
>> MITgcm-support at mitgcm.org
>> http://mitgcm.org/mailman/listinfo/mitgcm-support
>
>
> --
> Nicolas Grisouard - Postdoctoral Scholar
> Stanford School of Earth Sciences
> 473 via Ortega - room M11
> Stanford, CA 94305-4216
> Dept. fax: (+1) 650-498-5099
> Office Skype ID: nicolas.grisouard
> http://nicolas.grisouard.free.fr
> http://www.mendeley.com/profiles/nicolas-grisouard/
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--
Jody Klymak
http://web.uvic.ca/~jklymak/
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