[ecco-support] ECCO V4R3 SSH

Yao Yu yaoyu.9404 at gmail.com
Mon Jul 9 09:44:33 EDT 2018


Hi Rui and Ou,

  Thank you so much for your responses. My questions got solved! Also
thanks for your cool ECCO work!

Yao

2018-07-09 21:06 GMT+08:00 Ponte, Rui <RPonte at aer.com>:

> Yao,
>
>
>
> The ~25-d period variability in the Argentine Basin is described in many
> papers as being caused by nonlinear eddy interactions with mean flow and
> topography. Models need sufficient resolution to simulate those processes.
> Given the relatively coarse grid of ECCO v4r3, the eddy-driven dynamics
> relevant for that variability is most likely not well represented in the
> solution. In this regard, some higher resolution ECCO products (e.g. SOSE,
> ECCO2) might be more helpful.
>
>
>
> --
>
> Rui M. Ponte
>
> Atmospheric and Environmental Research, Inc.
>
> 131 Hartwell Avenue
>
> Lexington, MA 02421-3126 USA
>
> 781-761-2288 | www.aer.com
>
>
>
>
>
> *From: *<ecco-support-bounces at mit.edu> on behalf of ""Wang, Ou" (3244)" <
> Ou.Wang at jpl.nasa.gov>
> *Reply-To: *"ECCO support list, wider membership" <ecco-support at mit.edu>
> *Date: *Saturday, July 7, 2018 at 4:39 AM
> *To: *"ECCO support list, wider membership" <ecco-support at mit.edu>
> *Subject: *Re: [ecco-support] ECCO V4R3 SSH
>
>
>
> Hello Yao,
>
>
>
> The satellite altimetry constrain for the most recent 30 iterations or so
> is only applied to the large-scale features where the model-data misfit is
> smoothed both spatially and temporarily. This may explain why v4r3 does not
> have the small feature you are interested. It would be helpful if you could
> post a figure showing the comparison you made for the four observational
> and model products.
>
> Ou Wang
>
>
> On Jul 7, 2018, at 12:01 AM, Yao Yu <yaoyu.9404 at gmail.com> wrote:
>
>
>
> Dear EECO suport team,
>
>
>
>   I am Yao Yu, a graduate student in China. I am writing to inquire about
> the assimilation of altimetry SSH in the ECCO V4R3 OGCM.
>
>
>
>  I am using satellite altimetry measurements, GRACE measurements and two
> OGCMs (GLORYS2V4 and ECCO V4R3) to analyze an oceanic gyre in the Argentine
> Basin. However, ECCO failed to reproduce the sought-after feature (~25-day,
> ~500 km) while the three others could. I am trying to figure out the
> reason. I have read about the datasets used in ECCO (
> ftp://ecco.jpl.nasa.gov/Version4/Release3/doc/v4r3_data.pdf
> <https://urldefense.proofpoint.com/v2/url?u=ftp-3A__ecco.jpl.nasa.gov_Version4_Release3_doc_v4r3-5Fdata.pdf&d=DwMGaQ&c=birp9sjcGzT9DCP3EIAtLA&r=1L8uucM1VfjzQOg3MBsQnQ&m=lCbsvOEQyNPpqCsz6l8SqQmJCM7qor0uZ975iAThJLs&s=NZwC9m2wpmi-Fs_2qRh9r8M62_QbwNkVd-7n0BFteDM&e=>)
> and then Forgot and Ponte (2015) for details about altimeter data.
>
>
>
> I'd be grateful if you can help to answer my questions:
>
>
>
> 1. Are there any spatial (except for the bin-averaging) and temporal
> smoothing schema applied to altimeter data?  I don't think the nominal
> 1-degree spatial resolution of ECCO is coarse, however, ECCO's SSH look
> quite coarse (comparable with GRACE, ~300km) in the Argentine Basin.
>
>
>
> 2. If the answer is no for question 1, then are there any possible reasons
> that can explain inability of ECCO over the Argentine Basin?
>
>
>
> Many thanks!
>
> [image: mage removed by sender.]
>
> Yao
>
>
>
>
>
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