No subject
Tue May 11 10:12:20 EDT 2010
Does that make sense?
Martin
On Sep 15, 2011, at 10:49 PM, Katherine Quinn wrote:
> Hi all,
>
> I'm trying to get a bottom pressure anomaly within the MITgcm code instead doing the usual remove the time mean from phihydlow after running an experiment. The bottom pressure anomaly I need shouldn't have any topography signal in it. The phihydlow values have a range of approximately -1000 to 1000 and have a clear topography signal.
>
> As I understand it from past email list messages and the code, phihydlow should be the hydrostatic potential anomaly at the depths in R_low. Given this, I would have expected the time mean of phihydlow to be a linear function of R_low. When you do the linear fit it's approximately -0.4*(R_low - spatialmean(R_low)). But the fit to R_low is actually more like a quadratic. Does anyone know what I need to remove from phihydlow to get a true bottom pressure anomaly with no topography signal?
>
> thanks, Katy
>
> --
> Katherine J. Quinn
> Atmospheric and Environmental Research, Inc. voice: 781-761-2234
> 131 Hartwell Avenue fax: 781-761-2299
> Lexington, MA 02421-3126 e-mail: kquinn at aer.com
>
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