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Can we combine satellite derived Soil Moisture with
hydrological models?
VanderSat
● Founded in 2015
● 10, 14 23 employees (scientists ( > 50 % has a phd in
EO) and entrepreneurs)
● Transition from startup to SME
● Located in Haarlem
● Commercial EO services
● Prime focus on Microwave data and Soil Moisture
● Mission:
Build the best satellite products to solve the
global water and food crisis and always
keep innovating.
Soil moisture and hydrology
1. Soil moisture
● Indicator for drought
● Indicator for floods
● Derive discharge rating from soil moisture
● Input to models
2. Surface water
● Identify water seasonality
● Post flood analysis
● Flood monitoring/risk
The state of the system (now) is the
most important factor in determining
the quality of modelling results ->
Soil moisture helps a LOT in doing
that!
Inputtomodels
Monitoring
Also VOD and Temp
Why Soil moisture?
1. Represent a store (not a flux)
2. Indicator for floods and droughts
3. Check the relation between Q and soil
moisture and Q and precipitation
Satellite Soil Moisture
Case study of a catchment in Australia, Van der Schalie et al., 2015: RSE
7
Data architecture
<12 hr for L1
(7d for L4)
Downscaling //
LPRM //
Corrections //
Flagging //
L1
L3
+ 2 hr
Viewer //
API connected //
< 14 hr
https://maps.vandersat.com/
Success parameters….
1. The soil moisture to be used should:
a. be of sufficient quality and preferably
come with defined errors
b. have sufficient spatial and temporal
resolution
c. operational product
2. The model should be able to properly
represent (top) soil moisture
a. Sometimes derived parameters
(discharge) can be used
3. The model should be able to handle the
new input data
VanderSat Soil Moisture VS Cosmic Ray
VanderSat Soil Moisture VS Cosmic Ray
VanderSat Soil Moisture VS Cosmic Ray
Calibration with Soil
Moisture
1. Demonstrate here in PCR-GLOBWB
2. Can be done globally
Assimilation with Soil
Moisture
1. Demonstrate here in PCR-GLOBWB
2. Performance close to a locally calibrated
model
Assimilation of Q derived from
satellite soil moisture in
wflow_sbm
Mozambique
1. Used layered wflow_sbm to
match different zones
2. Large uncertainties in:
a. Precipi
b. Soil
c. but also the soil
moisture
3. When it matches we have
more certainty
Conclusions
1. Satellite soil moisture is available at NRT globally
(between 2 and 7 times per week)
2. New layered wflow_sbm can be configured to match the
satellite observed soil moisture
3. For models that do not have a surface soil moisture store
we can use a Derived Root Zone Soil Moisture or
discharge derived from soil moisture/wetness
4. Improvement is large for poorly or uncalibrated models
and smaller for well calibrated models
5. If a model is well calibrated but for the wrong reasons
adding soil moisture will show this -> recalibration
required
jschellekens@vandersat.com
www.vandersat.com

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DSD-INT 2018 Can we combine satellite derived Soil Moisture with hydrological models - Schellekens

  • 1. Can we combine satellite derived Soil Moisture with hydrological models?
  • 2. VanderSat ● Founded in 2015 ● 10, 14 23 employees (scientists ( > 50 % has a phd in EO) and entrepreneurs) ● Transition from startup to SME ● Located in Haarlem ● Commercial EO services ● Prime focus on Microwave data and Soil Moisture ● Mission: Build the best satellite products to solve the global water and food crisis and always keep innovating.
  • 3. Soil moisture and hydrology 1. Soil moisture ● Indicator for drought ● Indicator for floods ● Derive discharge rating from soil moisture ● Input to models 2. Surface water ● Identify water seasonality ● Post flood analysis ● Flood monitoring/risk The state of the system (now) is the most important factor in determining the quality of modelling results -> Soil moisture helps a LOT in doing that! Inputtomodels Monitoring Also VOD and Temp
  • 4. Why Soil moisture? 1. Represent a store (not a flux) 2. Indicator for floods and droughts 3. Check the relation between Q and soil moisture and Q and precipitation
  • 5. Satellite Soil Moisture Case study of a catchment in Australia, Van der Schalie et al., 2015: RSE
  • 6. 7 Data architecture <12 hr for L1 (7d for L4) Downscaling // LPRM // Corrections // Flagging // L1 L3 + 2 hr Viewer // API connected // < 14 hr
  • 8. Success parameters…. 1. The soil moisture to be used should: a. be of sufficient quality and preferably come with defined errors b. have sufficient spatial and temporal resolution c. operational product 2. The model should be able to properly represent (top) soil moisture a. Sometimes derived parameters (discharge) can be used 3. The model should be able to handle the new input data
  • 9. VanderSat Soil Moisture VS Cosmic Ray
  • 10. VanderSat Soil Moisture VS Cosmic Ray
  • 11. VanderSat Soil Moisture VS Cosmic Ray
  • 12. Calibration with Soil Moisture 1. Demonstrate here in PCR-GLOBWB 2. Can be done globally
  • 13. Assimilation with Soil Moisture 1. Demonstrate here in PCR-GLOBWB 2. Performance close to a locally calibrated model
  • 14. Assimilation of Q derived from satellite soil moisture in wflow_sbm
  • 15. Mozambique 1. Used layered wflow_sbm to match different zones 2. Large uncertainties in: a. Precipi b. Soil c. but also the soil moisture 3. When it matches we have more certainty
  • 16.
  • 17. Conclusions 1. Satellite soil moisture is available at NRT globally (between 2 and 7 times per week) 2. New layered wflow_sbm can be configured to match the satellite observed soil moisture 3. For models that do not have a surface soil moisture store we can use a Derived Root Zone Soil Moisture or discharge derived from soil moisture/wetness 4. Improvement is large for poorly or uncalibrated models and smaller for well calibrated models 5. If a model is well calibrated but for the wrong reasons adding soil moisture will show this -> recalibration required