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The revised Diagnostics of 2m Values
- Motivation, Method and Impact -
M. Raschendorfer, FE14
Matthias RaschendorferDWD COSMO Cracow 2008
Matthias RaschendorferDWD COSMO Cracow 2008
There was some significant overestimation of 2m temperature round noon
at grid points with a rough surface (city points)
accompanied by nearly saturated soil and too high 2m dew points
Obviously SMA couldn’t correct this errors
What was the reason?
Could we expect related errors in other variables?
deviation of T2m
compared to SYNOP-measure
parameters controlling evapotranspiration:
-soil moisture
modified relation between sensible and latent heat flux
daily cycle of
boundary layer profiles
for
temperature and humidity
Diagnosis onto 2m level
daily cycle of T2m, TP2m
turbulence model
SMA
-min. stomata resistance, PLCOV, LAI, root depth, sealing, soil type, …
The feed back with soil moisture analysis SMA:
Matthias RaschendorferDWD COSMO Cracow 2008
We assumed a systematic shortcoming in the calculation of 2m temperatures
at grid points with a rough surface (city points)
causing to high values at daytime
SMA reacted by moistening the soil until it was saturated
Artificial soil moistening may have caused artificial evaporation accompanied by
a too moist and too cold boundary layer
At that point SMA couldn’t correct the discrepancy any longer
As a reason of that shortcoming we found a discrepancy between
2m values referring to the whole grid box andthose taken at a standard SYNOP lawn
laminar layer
0z
u0
0A zh
logarithmic Prandtl-layer profile
unstable stable
linear interpolated
Prandtl layer
roughness layer
z
expon. roughness-layer profile
0
Bhm20
m2 S
lowest model main level
upper boundary of the lowest model layer
lower boundary of the lowest model layer
h
0B zh
Ahm10
0
m2
dHz
SYNOP station lawn profile
Mean GRID box profile
Turbulent velocity scale profile
u
Hu
SAH0
SAHz ruz
turbulence-scheme
00 dz
0SH zzu
dzr
:
Az
Bz
A s m2
• Exponential roughness layer profile is valid for the whole grid box,
• but it is not present at a SYNOP station
Sz0
H00 zzd
m2
dz
no storage capacity
Diagnosis of 2m-values with respect to a SYNOP lawn:
m2dzzddd 00H
Accumulated soil moisture increments of SMA for routine and Exp 6343:
The accumulated effect of SMA on soil moisture averaged along a domain that more or less covers Germany is plotted for the fist 6 weeks of Exp. 6343.For about the first 14 days SMA of Exp. 6343 (green and blue lines) takes water out of the soil, whereas SMA of our routine always brings additional water into the soil. During this period soil moisture has adapted to the new formulation of T2m diagnostics. Integrated along the whole 6 week period SMA of the routine has significantly moistened the soil, indicating a systematic error. In contrast SMA of Exp. 6343 shows almost no systematic trend.
Period of soil moisture adoption
m30z0 . ( & ‘plant cover’ 70% & ‘surface height’ 800m) ‘city’ :=
Soi
l de
pth
in [
cm]
Soil moisture profiles:
T2m
of
Exp
. 63
43 –
T2m
of
r th
e ro
utin
e
Roughness length
Joined frequency distribution of roughness length and difference of T2m:
For “summer”
For winter
Mean surface flux densities:
LME ROUT
LME ROUT
Matthias RaschendorferDWD COSMO Cracow 2008
Conclusion:
Discrepancy between the transfer layer of a mean model grid box and a SYNOP lawn caused
The introduction of a SYNOP lawn for deduction of 2m values cured the problem
There are still problems with the daily cycle of near surface values (too warm at midnight)
- daytime overestimation of T_2m compared to SYNOP measurement for rough grid points
- a too wet soil and a too moist and too cold boundary layer due to the action of SMA
- That may be cured by a reformulation of profile functions through the transfer layer
- This step had to be delayed due to other priorities
- We should introduce these steps now with first priority!
Thank You for attention!
Time-Height Cross-section for “errors” in the boundary layer:
Temperature “error” Dew point “error”
Too cold Too moist
800 m a.g.
0 m a.g.
For “summer”
For winter
LME ROUT
LME ROUT
Advection of a warm bias
Too cold from noon to night Still to cold during morning
Downward mixing of positive bias above