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Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
CMSAF water vapour in comparison to radiosondes and
CHAMP
Ralf Lindau
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
Water vapour from ATOVS
Global daily fields of Layered Precipitable Water LPW are calculated by kriging method on 90 km resolution.
Advantage of kriging : An error map is available for each field.
Example: 1.10.2004
850 – 700 hPa
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
Radiosondes
173 GUAN (GCOS Upper-Air Network)stations well distributed over the globe.
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
It‘s the resolution, stupid
For any comparison of two data sets resolution is crucial.
If resolutions are not equal, the often actually seriously presented conclusion would be:
The low resolved observations underestimate high values and overestimate low values.
ATOVS fields: Daily , 90 kmRadiosondes: 4 times a day, point measurements
Thus, average the radiosondes over 1 day.But still Radiosonde data include additionally the spatial variance of daily
means within 90 x 90 km2
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
Variability of Water Vapour
Famous paper:
Lindau, R. and E. Ruprecht, 2000: SSM/I-derived total vapour content over the Baltic Sea compared to independent data, Met.Zeitschrift, 9, No.2, 117-123.
1 day include 8 mm2 of variance
90 by 90 km2
include 3 mm2 of variance
The spatial variance of temporal means must be smaller than that of individuals (3 mm2).
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
October 2004
+ 3.82 mm + 17 %
High correlation: r = 0.95
But wet bias of 3.82 mm2
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
Happy with correlation ?
Correlation reduction due errors is:
1 - r = e2 / (2 + e2 )= 7.5 mm2 / 225 mm2
= 0.03
More than half of the scatter is explainedby random errors in ATOVS and RS.
But there is still the bias....
The error of ATOVS is explicitelycalculated within kriging.
The mean error variance for October 2004 and for those 173 gridboxes, where RS data is available is:
eAT = 6.19 mm2
The error variance of daily means from RS is calculated by: Internal variance / observ number:
eRS = 7.65 mm2
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
Different layers
+ 2.35 mm + 21 % + 0.18 mm
+ 5 %
1000 – 850 hPa 700 – 500 hPa
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
Time series of the bias
The bias is not confined to October 2004.
It persists through 10 month
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
Discriminating GUAM data
Ocean / Land Height above sea
or is it the ice surface in the Antarctica?
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
Ocean, Height, Ice ?
+ 2.85 mm + 16 %
+ 1.68 mm + 9 %
- 0.18 mm - 7 %
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
Different First-guesses
No
GME
NCEP
Different first-guess (taken asbasis for the retrieval) result in strong differences.
Example: 1.9.2006, 700-500 hPa
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
ATOVS vs Radiosondes
No
GME
NCEP
- 0.82 mm - 3 %
+ 3.67 mm + 14 %
+ 7.08 mm + 27 %
The corresponding bias vanishes for „No first guess“
and is doubled, if NCEP is used.
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
... and what about Champ ?
Example for 1 monthof Champ data.
4239 obs/month1 obs/10 min
Irregularly spreadedover the globe
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
ATOVS vs Champ850 – 700 hP
a700 – 500 hP
a
- 3.20 mm- 15 %
- 0.15 mm- 5 %
+ 0.02 mm+ 2 %
Diplomanden-Doktoranden-Seminar Bonn, now Cologne – 8 Januar 2007
Conclusion
ATOVS vs radiosondes- ATOVS has a wet bias compared to radiosondes.- Bias is decreasing with height.- It persists through all discrimination experiments.- First guesses play an important role for the retrieval.
Champ vs ATOVS- Champ has dry bias compared to ATOVS- (thus, seems to agree with RS, but no direct comparison possible)- Bias is decresing with height.