Correction to the Parallel SREF
Physics Diversity Eta BMJ-SAT and KF-DET memberS
Brad Ferrier, Jun Du, Geoff
Manikin, Binbin Zhou and Jeff McQueen
Implemented in Parallel runs on : June
10, 2004, 21 Z
Summary of change:
A bug was found and corrected in the two BMJ-SAT members of the SREF
system which caused strong overprediction of precipitation and
occasional execution failures. In addition, an improvement is
proposed
for the two KF-DET members to reduce a precip bias noted during
the
parallel evaluation.
Description of Problem .
- A logical flag used to define the experimental
Betts-Miller-Janjic (BMJ)
convective scheme using moistened reference profiles (referred to as
BMJ_SAT)
was not passed into the Eta driver, resulting in convection not being
called. This resulted in strong overprediction of precipitation
and
occasional execution failures of the 2 BMJ-SAT members.
The impact of the change will be positive as a result of stabilization
by convection occurring in the revised runs. The change will be
manifested
in improved QPF with fewer grid-point bombs and spurious precipitation
maxima, better pre-convective forecast soundings, and overall model
performance.
The reference profiles are not saturated but rather are half way
between
saturation and the moisture profiles currently used in the operational
Eta.
- Slight modifications to the Kain-Fritsch (KF) convective scheme
will implement
the change intended to be made in April, in that half of the rain and
snow
in the convective updrafts are detrained back onto the grid with the
remaining
convective precipitation reaching the surface. The impact of this
"half detrainment" change is to produce some convective precipitation,
replacing the "full detrainment" version where no convective
precipitation
is produced. This change is also expected to reduce both the low
bias in precipitation, and the cool, moist bias that has formed in
association
with these two Eta members.
Analysis
of Change
Below are a series of SREF member ETA-BMJ-SAT and KF-DET runs using
the same (perturbed) ICs and LBCs obtained
from the bred n4 (SAT) run that failed on 20040602 at 21 Z.. For
reference,
here is the 24-h CPC/RFC verification.
Below is a table of images showing 24-h total (2nd column),
convective
(3rd), and grid scale (last) precipitation for each run (described in
1st
column). You can see from this table the following:
- The total absence of convective precip in the original SAT run
(1st row),
which then shows up in the corrected versions (rows 2-4).
- The sensitivity of the (corrected, modified) SAT runs to the
different
moisture profiles (rows 2-4). The largest area of precip is
predicted
using the operational moisture profiles (2nd row), progressively
shrinking
with more grid-scale and less convective precip as the reference
profiles
moisten (3rd, 4th rows; saturated profiles assumed in 4th row).
- A drawback in assuming moister profiles, which I only realize
now, is that
it exacerbates the low bias in precip out west.
- The 5th row shows the impact of the current KF detrainment run,
showing
no convective precip and only grid-scale precip, even though we
intended
to have only half of the convective rainfall detrained onto the grid
scale
and the rest fall to the surface as rain. The last row shows that
this was fixed, in which most of the precip is still convective despite
having half of the condensate in the updrafts detrained back onto the
grid.
Regards,
Brad
RUN
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Total Precip (15-39 h)
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Conv Precip (15-39 h)
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Grid Precip (15-39 h)
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Original SAT
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Corrected SAT,
operational moisture profiles
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Corrected SAT,
moistened moisture profiles (half way to
saturation)
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Original DET,
full detrainment in KF
(what we intended to be "half detrainment")
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Modified DET,
half detrainment in KF
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Technical contact on These Changes:
Brad Ferrier
<Brad.Ferrier@noaa.gov
>
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NOAA/NWS/NCEP/EMC &
SAIC/GSO
EMC/Mesoscale
Modeling Branch
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