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New SciDoc doxygen configuration file #314

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climbfuji merged 3 commits into
NCAR:gmtb/developfrom
ligiabernardet:SciDoc_update
Sep 9, 2019
Merged

New SciDoc doxygen configuration file #314
climbfuji merged 3 commits into
NCAR:gmtb/developfrom
ligiabernardet:SciDoc_update

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@ligiabernardet
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Added a new SciDoc doxygen configuration file so it is not V3-specific and incorporates include HTML files. This update is referenced in a companion PR to ccpp-framework (PR # 214 about TechDoc).

…dentical to ccppv3_doxyfile, except that it is not specific to the V3 release and contains information about where to find the HTML files containing the metadata tables created from the .meta files (new metadata format).
Comment thread physics/docs/ccpp_doxyfile
Comment thread physics/docs/ccpp_doxyfile
OPTIMIZE_OUTPUT_VHDL = NO
EXTENSION_MAPPING = .f=FortranFree \
.F90=FortranFree \
.f90=FortranFree
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can you add .F here as well, please? .F and .f should be FortranFixed (or whatever the correct name for it is)?

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@ligiabernardet can you also address this comment, please, and try if .f=FortranFixed (or whatever the correct name for it is) and .F=FortranFixed work as expected?

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I made this change and pushed the commit. It did not alter the SciDoc HTML output.

… documented (added .F). Remove mention of V3 release so documentation is generic.
@climbfuji climbfuji merged commit 20dd8d2 into NCAR:gmtb/develop Sep 9, 2019
@ligiabernardet ligiabernardet deleted the SciDoc_update branch March 30, 2020 21:45
hannahcbarnes pushed a commit to hannahcbarnes/ccpp-physics that referenced this pull request Aug 3, 2022
…CAR#314)

Cumulus convection:
a) More strict convection trigger
b) Reduced entrainment rate below cloud base
c) Enhanced downdraft detrainments starting from 60mb above the ground surface
d) Reduced rain evaporation
e) Modification of cloud depth separating shallow convection from deep convection

PBL and surface layer:
a) Inclusion of wind shear effect reducing characteristic mixing length
b) Reduction of background diffusivity in the inversion layers as a function of surface roughness and green vegetation fraction
c) PBL updraft overshooting limited by bulk Richardson number-based-PBL depth
d) Inclusion of new canopy heat storage parameterization
e) Modification of thermal roughness calculation over land
f) Increase of momentum roughness length over sea
g) Inclusion of sea spray effect parameterization
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2 participants