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As the model levels get further apart near the top, this will tend to produce pressures that are too large since pressure varies approximately exponentially with height. It would be more accurate to interpolate log(P), then convert back to P afterward (similar to what is done for the model top extrapolation on L415). Although I do not know how pres2_p is used after this calculation, this could be a source of inaccuracy.
Note that the interpolation of P is inconsistent with core_init_atmosphere, which interpolates log(P).
The
MPAS_to_physics
subroutine interpolates pressure linearly with the height coordinate (see below).MPAS-Model/src/core_atmosphere/physics/mpas_atmphys_interface.F
Line 397 in 7601162
As the model levels get further apart near the top, this will tend to produce pressures that are too large since pressure varies approximately exponentially with height. It would be more accurate to interpolate log(P), then convert back to P afterward (similar to what is done for the model top extrapolation on L415). Although I do not know how
pres2_p
is used after this calculation, this could be a source of inaccuracy.Note that the interpolation of P is inconsistent with
core_init_atmosphere
, which interpolates log(P).See https://github.com/JCSDA-internal/mpas-jedi/issues/795 for more discussion.
EDIT: also see the related WRF publication, https://journals.ametsoc.org/view/journals/mwre/140/12/mwr-d-12-00045.1.xml
@liujake @mgduda @ldfowler58 @byoung-joo @metdyn
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