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Add RRFS-SD reader #154
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Add RRFS-SD reader #154
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this addresses #152 |
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Just few initial comments. I'll work on the pressure calculation once I have extracted some sample data.
if "ug/kg" in dset[i].attrs["units"]: | ||
# ug/kg -> ug/m3 using dry air density | ||
dset[i] = dset[i] * dset["pres_pa_mid"] / dset["temperature_k"] / 287.05535 | ||
dset[i].attrs["units"] = r"$\mu g m^{-3}$" |
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If we really want a pretty version here could use unicode, e.g. μg/m³
or μg m⁻³
. But maybe better to use just ASCII ug/m3
or ug m-3
.
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Let’s stick with ascii. It may cause issues down the pipeline if we save the raw files out. It might not be recognized as CF convention otherwise
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Then I think ug m-3
best for CF (though they would want kg m-3
for canonical).
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# convert "ug/kg to ug/m3" |
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Do we want this to be optional like Jordan's?
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I dont see why
Co-authored-by: Zachary Moon <[email protected]>
Co-authored-by: Zachary Moon <[email protected]>
Co-authored-by: Zachary Moon <[email protected]>
Co-authored-by: Zachary Moon <[email protected]>
Co-authored-by: Zachary Moon <[email protected]>
phalf(k) = a(k) + surfpres * b(k) | ||
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Mid layer pressures are calculated by: | ||
pfull(k) = (phalf(k+1)-phalf(k))/log(phalf(k+1)/phalf(k)) |
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not sure where this formula came from
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This is the formula used in the post_fv3 https://github.com/NOAA-EMC/fv3atm/blob/a82381c0b751a15e5343de5078ef836b2c444c89/io/post_fv3.F90#L4266-L4276
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@zmoon still not sure where this formula came from
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@rschwant do you know? I think that you originally did this
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Raffaele sent it to me to describe the vertical structure in the model when I was helping with the boundary conditions. I'll forward you all the email. This is how he described it to me.
Interface pressure levels are computed using the hybrid interface formula:
p(k) = a(k) + ps * b(k)
where ps is the (actual/reference) surface pressure. These pressure levels correspond to phalf in your output dyn*.nc files, while pfull are computed as:
pfull(k) = (phalf(k+1)-phalf(k))/log(phalf(k+1)/phalf(k))
If there is an official typical way of calculating this we can use that instead too. We haven't really tested this much since we have not used the aircraft evaluation in MELDODIES MONET much in the RRFS-CMAQ model.
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I'll compare the two methods' results.
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this is how Raffaele calculated it for UFS-Aerosols in the exglobal_aero_init function https://github.com/NOAA-EMC/global-workflow/blob/develop/ush/merge_fv3_aerosol_tile.py#L99-L101
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I think that we should use that
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p = dset.dp_pa.copy().load() # Have to load into memory here so can assign levels. | ||
srfpres = dset.surfpres_pa.copy().load() | ||
for k in range(len(dset.z)): | ||
if surf_only: | ||
pres_2 = 0.0 + srfpres * 0.9978736 | ||
pres_1 = 0.0 + srfpres * 1.0 | ||
else: | ||
pres_2 = dset.ak[k + 1] + srfpres * dset.bk[k + 1] | ||
pres_1 = dset.ak[k] + srfpres * dset.bk[k] | ||
p[:, k, :, :] = (pres_2 - pres_1) / np.log(pres_2 / pres_1) |
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Maybe something like this
p = dset.dp_pa.copy().load() # Have to load into memory here so can assign levels. | |
srfpres = dset.surfpres_pa.copy().load() | |
for k in range(len(dset.z)): | |
if surf_only: | |
pres_2 = 0.0 + srfpres * 0.9978736 | |
pres_1 = 0.0 + srfpres * 1.0 | |
else: | |
pres_2 = dset.ak[k + 1] + srfpres * dset.bk[k + 1] | |
pres_1 = dset.ak[k] + srfpres * dset.bk[k] | |
p[:, k, :, :] = (pres_2 - pres_1) / np.log(pres_2 / pres_1) | |
surfpres = dset.surfpres_pa | |
a = dset.ak | |
b = dset.bk | |
if surf_only: | |
phalf_kp1 = 0.0 + surfpres * 0.9978736 | |
phalf_k = 0.0 + surfpres * 1.0 | |
else: | |
phalf_kp1 = a.shift(z=-1) + surfpres * b.shift(z=-1) | |
phalf_k = a + surfpres * b | |
p = (phalf_kp1 - phalf_k) / np.log(phalf_kp1 / phalf_k) |
going for consistency with the docstring variable names
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Since ak
and bk
are dataset attrs, not variables
phalf_kp1 = a[1:] + surfpres * b[1:]
but may need to make them DataArray
s for the dims to match up properly and such, maybe create
a_k = xr.DataArray(ds.ak[:-1], dims="z")
a_kp1 = xr.DataArray(ds.ak[1:], dims="z")
b_k = xr.DataArray(ds.bk[:-1], dims="z")
b_kp1 = xr.DataArray(ds.bk[1:], dims="z")
@bbakernoaa I made an extraction (forecast hour 6 of the run you shared, 5 levels closest to surface, selected variables, etc.), now available at https://csl.noaa.gov/groups/csl4/modeldata/melodies-monet/data/example_model_data/rrfssd_example/rrfs-sd_dynf006.nc (104M) for testing. We can set it up like I did here, which also uses data stored in that location. |
maybe we can add some netcdf tricks to compress that even further using integers instead of floats and the add_offset and scale_factor netcdf attributes |
Perhaps, but I think it is better to keep format closer to the original. And I used NCO lossy compression, which already decreases the size a lot due to quantization, I don't know if additionally doing the int packing transform would make it any more compressible. |
Geoptential height with attributes. | ||
""" | ||
sfc = f.surfalt_m.load() | ||
dz = f.dz_m.load() * -1.0 |
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This (loading all dz) is what Maggie's run is failing on, specifically:
Unable to allocate 129. GiB for an array with shape (37, 65, 2961, 4881) and data type float32
Like the pressure calc we should be able to write this in a Dask-friendly way.
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Also like pressure calc, for the surf-only case there is a short version.
# These are negative in RRFS-CMAQ, but you resorted and are adding from the surface, | ||
# so make them positive. | ||
dz[:, 0, :, :] = dz[:, 0, :, :] + sfc # Add the surface altitude to the first model level only | ||
z = dz.rolling(z=len(f.z), min_periods=1).sum() |
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I would think .cumsum()
could be used.
create a separate reader for RRFS-SD. This is based on
_rrfs_cmaq_mm
but removes many of the functions as rrfs-sd is obviously much simpler.