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DFG Round Table – Frankfurt a.M. – 23th May 2006
Soil moisture in Tibet derived from satellite obsevations
C. Simmer and R. Lindau
University of Bonn
DFG Round Table – Frankfurt a.M. – 23th May 2006
ANOVA of Soil Moisture measurements
Variance in mm2 Number of bins
Error of the total
mean
Seeming external variance
Error of external means
Internal variance
True external variance
Relative external variance
Annual Cycle 36 2 388 51 10343 338 3.16%
Interstation 48 2 9133 10 1558 9123 85.40%
Interannual 8 2 39 12 10654 26 0.25%
Total variance External variance Internal variance
= Variance between + Mean variance
the means of the within the subsamples subsamples
DFG Round Table – Frankfurt a.M. – 23th May 2006
Local longtime means
single cumulative
Climatolog. rain 58.6 58.6
Soil texture 0.5 69.0
Vegetation 37.7 72.8
Terrain slope 2.8 73.0
73% of the soil moisture variance is explained by four parameters :
DFG Round Table – Frankfurt a.M. – 23th May 2006
Two-step Retrieval
Climatological mean
derived from:
• Longterm precipitation• Soil texture• Vegetation density• Terrain slope
Temporal anomalies from:
• Brightness temperatures at 10 GHz• Anomalies of rain and air temperature
+
DFG Round Table – Frankfurt a.M. – 23th May 2006
Application: DEKLIM
BALTIMOS within DEKLIM (Deutsches Klimaforschungsprogramm):
Validation of a 10-years climate run of the regional model REMO using SMMR. Example: Oder catchment
R. Lindau and C. Simmer: Derivation of a root zone soil moisture algorithm and its application to validate model data. Nordic Hydrology, accepted for publ.
DFG Round Table – Frankfurt a.M. – 23th May 2006
Application: AMSR
GEOLAND within GMES (Global Monitoring for Environment and Security):
Derivation of global soil moisture fields from AMSR
M. Leroy, R. Lacaze, R. Lindau, F. Oleson, L. Pessanha, I. Piccard, A. Rosema, J-L. Roujean, F. Rubel, W. Wagner, M. Weiss, 2004: Towards a European Service Center for Monitoring land surfaces at global and regional Scales: The GEOLAND/ CSP Project International Archives of Photogrammetry and Remote Sensing, XXth ISPRS Congress, Istanbul, 35 (B4), 783-790.
Long
term
mea
nT
empo
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nom
aly
DFG Round Table – Frankfurt a.M. – 23th May 2006
Mean Soil Moisture in Tibet
• The longtime mean field is characterized by strong gradients
Three points on the above section show decreasing soil moisture towards NWwith a minimum in August