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research_blog/2023/03/14/lwsrc-idealized-run #25
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Aurora, small note: I think in the code (where it adds the tracer) turning off LTracerSrc only has an effect if you are not using MPDATA. PM |
Got it. Nice checking.
…On Wed, Mar 15, 2023 at 10:11 AM ajleeson ***@***.***> wrote:
Hi Parker,
Thanks for checking in! I ran a quick test, and it seems that LTracerSrc =
F works even when using MPDATA. Below is a salinity section across a
freshwater point source with LTracerSrc = F:
[image: ltracersrcF]
<https://user-images.githubusercontent.com/15829099/225387168-b0e665d2-aabf-4b22-a021-793e6f71cedd.png>
And here is one for LTracerSrc = T:
[image: ltracersrcT]
<https://user-images.githubusercontent.com/15829099/225387176-a3169bd6-5465-48c3-bf51-24eeb3cf217f.png>
MPDATA was used in both cases.
Given these results, I think the idealized estuary results in the blog
post shouldn't be impacted by buoyancy effects.
Aurora
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First, we had quiche in celebration of Pi day (and an apple pie), so I definitely think tart counts. |
Hi Alex, Thanks for the input! It is very strange that the horizontal velocity at the source is different than elsewhere. I'll subtract the tidal velocity and see what it looks like. Like you mentioned, maybe this will give us more clues about how the sources are implemented in ROMS. Aurora |
Note that the velocity from a mooring extraction is just pulled in by
nearest-neighbor, so it is not interpolated to the rho-grid.
In contrast, the section making code (if you are using my new version) does
interpolate everything.
PM
…On Thu, Mar 16, 2023 at 9:24 AM ajleeson ***@***.***> wrote:
Hi Alex,
Thanks for the input! It is very strange that the horizontal velocity at
the source is different than elsewhere. I'll subtract the tidal velocity
and see what it looks like. Like you mentioned, maybe this will give us
more clues about how the sources are implemented in ROMS.
Aurora
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Looking at LwSrc in Idealized Runs | Weekly Research Update
First order of business: Happy Pi Day! Does a tart count as a pie? This week I tested out a couple of different combinations of mixing coefficients and advectoin schemes, but still nothing seems to improve conditions at Birch Bay WWTP. I then focused my attention on the idealized estuary. I re-ran the model for one day with point sources discharging at a rate of 1 m3/s (rather than 1000 m3/s). I also disabled LtracerSrc so that the inflowing water enters at the same temperature and salinity as the water already in the grid cell. The results are not as extreme as what we observe at point sources in LiveOcean, however there are still interesting vertical velocity patterns in the water column. More details below. Mixing Coeff
https://ajleeson.github.io/research_blog/2023/03/14/lwsrc-idealized-run.html
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