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Validating satellite-derived land surface
temperature over mountainous area with in
situ measurements
Imlil Valley (High Atlas) - Morocco
Yoann Malbéteau
CESBIO / Toulouse
yoann.malbeteau@cesbio.cnes.fr
http://rec.isardsat.com
Merlin O., Gascoin S., Gastellu J.P., Mattar, C. Olivera L., Khabba S., Jarlan L.
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques 1 of 15
Temperature of Earth's lands during the daytime
April 2016 marks 12th consecutive month of record warmth for globe (NOAA)
Climatic scale
Land & Ocean temperature Percentiles Jan-April 2016
NOAA’s National centers for Environmental Information
Data Source: GHCN-M version 3.3.0 & ERSST version 4.0.0
Record
Warmest
Much
Warmer than
average
Warmer than
average
Near
average
Much
Cooler than
average
Cooler than
average
Record
Coldest
Over land: +2.33°C
Over land and ocean: +1.11°C
above the 20th century average
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques 2 of 15
Land surface temperature for agriculture….
Evapotranspiration estimation / Soil moisture downscaling
amongst of others…
Regional and parcel scale
ASTER temperature (90 m)
ET (mm/day)
0 108642
Olivera-Guerra L. et al. (2014)
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques 2 of 15
Land surface temperature for agriculture….
Evapotranspiration estimation / Soil moisture downscaling
amongst of others…
Regional and parcel scale
SMOS Product
Soil moisture
Disaggregated
82 000 km2
ASTER temperature (90 m)
MODIS land surface temperature (1 km)
ET (mm/day)
0 108642
Olivera-Guerra L. et al. (2014)
Malbeteau Y. et al. (2016)
6050 km2
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
What’s land surface temperature ?
LST
(Land Surface
Temperature)
NDVI
Soil
Moisture
Albedo
texture
ET
Meteo
Topo
3 of 15
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
What’s land surface temperature ?
LST
(Land Surface
Temperature)
NDVI
Soil
Moisture
Albedo
texture
ET
Meteo
Topo
3 of 15
LST landsat at 100m resolution
05 Septembre 2014
Lake
Mountains
Clouds
55
40
30
25
50
45
35
T °C
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
What’s land surface temperature over mountains?
4 of 15
Illumination
Elevation
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Land surface temperature over mountains
5 of 15
Aremd station
Northing
Easting
Elevation
1400
0
W.m-2
Net Radiation at 8m (from DART model)
at 11h21, the 05th of September
6 km
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Land surface temperature over mountains
6 of 15
45
30
20
15
40
35
25
T °CSun-exposed
slope
Shadowed
slope
Vegetation
River
Land surface temperature observed by ASTER satellite
6 km
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Scheme placement …
7 of 15
Temperature sensors/loggers
Different illumination and elevation
Spacing: ~100m
(ASTER/landsat resolution)
6 months
45
30
20
15
40
35
25
T °C
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
How can we validate surface temperature ?
8 of 15
Temperature sensors/loggers
ibutton sensor
135 ibuttons
Set up over
45 points
Locations of the 45 ibutton plates, each of them containing 3
ibutton sensors.
Red cross indicate plates not used for the study.
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Results: sample of in situ surface temperature
9 of 15
Date (mm/dd/2014)
Surfacetemperature(°C)
Sun exposed shadow exposed
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Results: sample of in situ surface temperature
Date (mm/dd/2014)
Surfacetemperature(°C)
Sun exposed shadow exposed
14°C
5°C
9 of 15
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Results: sample of in situ surface temperature
Date (mm/dd/2014)
Surfacetemperature(°C)
lag time
9 of 15
Sun exposed shadow exposed
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Results: sample of in situ surface temperature
Date (mm/dd/2014)
Surfacetemperature(°C)
Cloudy day
9 of 15
Energy balance
Transpiration
Evaporation
land surface
temperature
𝑻 𝑬𝑩 = 𝒇𝒗 𝑻𝒗 𝑬𝑩 + 𝟏 − 𝒇𝒗 𝑻𝒔 𝑬𝑩
Based on double source
(vegetation/soil) energy
balance model
𝑻𝒔 𝑬𝑩 = 𝒇𝒔𝒔 𝑻𝒔, 𝒅𝒓𝒚 𝑬𝑩 + 𝟏 − 𝒇𝒔𝒔 𝑻𝒔, 𝒘𝒆𝒕 𝑬𝑩
𝑻𝒗 𝑬𝑩 = 𝒇𝒔𝒗 𝑻𝒗, 𝒅𝒓𝒚 𝑬𝑩 + 𝟏 − 𝒇𝒔𝒗 𝑻𝒗, 𝒘𝒆𝒕 𝑬𝑩
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Modeling topographic effect over mountains
10 of 15
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Modeling topographic effect over mountains
ASTER LST simulated LST
45
30
20
15
40
35
25
T °C
90 m resolution 8 m resolution
Representativeness
11 of 15
6 km6 km
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Useful for model and observed data validation
14th April 2014 30th April 2014 05th September 2014
Simulated LST
ASTER LST
R (correlation) 14th April 30th April 05th September
Simulated LST 0.75 0.68 0.64
Observed LST 0.64 0.68 0.67
Scatterplots of ASTER and simulated LST at 90m
resolution versus ibutton measurements
12 of 15
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Useful for model and observed data validation
14th April 2014 30th April 2014 05th September 2014
Simulated LST
ASTER LST
R (correlation) 14th April 30th April 05th September
Simulated LST 0.75 0.68 0.64
Observed LST 0.64 0.68 0.67
B (bias) 14th April 30th April 05th September
Simulated LST 1.48 2.74 -0.43
Observed LST 3.04 3.38 0.78
Scatterplots of ASTER and simulated LST at 90m
resolution versus ibutton measurements
12 of 15
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Additional slide….
for future application over mountains
45
30
20
15
40
35
25
T °C
Before correction After correction
13 of 15
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Conclusion
Challenges:
Representativeness of in situ measurement for remote sensing data validation
solution ? very dense in situ measurement  aggregation
few in situ measurement  disaggregation (downscaling)
in situ measurement representative at the scale resolution
14 of 15
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Conclusion
Challenges:
Representativeness of in situ measurement for remote sensing data validation
solution ? very dense in situ measurement  aggregation
few in situ measurement  disaggregation (downscaling)
in situ measurement representative at the scale resolution
intercomparison between remotely sensed data
14 of 15
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Conclusion
Challenges:
Representativeness of in situ measurement for remote sensing data validation
solution ? very dense in situ measurement  aggregation
few in situ measurement  disaggregation (downscaling)
in situ measurement representative at the scale resolution
intercomparison between remotely sensed data
Terrain accessibility … “When science goes messy”
14 of 15
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Conclusion
Challenges:
Representativeness of in situ measurement for remote sensing data validation
solution ? very dense in situ measurement  aggregation
few in situ measurement  disaggregation (downscaling)
in situ measurement representative at the scale resolution
intercomparison between remotely sensed data
Terrain accessibility … “When science goes messy”
14 of 15
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Conclusion
Challenges:
Representativeness of in situ measurement for remote sensing data validation
solution ? very dense in situ measurement  aggregation
few in situ measurement  disaggregation (downscaling)
in situ measurement representative at the scale resolution
intercomparison between remotely sensed data
Terrain accessibility … “When science goes messy”
14 of 15
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Conclusion
Challenges:
Representativeness of in situ measurement for remote sensing data validation
solution ? very dense in situ measurement  aggregation
few in situ measurement  disaggregation (downscaling)
in situ measurement representative at the scale resolution
intercomparison between remotely sensed data
Terrain accessibility … “When science goes messy”
14 of 15
Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques
Conclusion
Challenges:
Representativeness of in situ measurement for remote sensing data validation
solution ? very dense in situ measurement  aggregation
few in situ measurement  disaggregation (downscaling)
in situ measurement representative at the scale resolution
intercomparison between remotely sensed data
Terrain accessibility
But it is great …
14 of 15
Validating satellite-derived land surface
temperature over mountainous area with in situ
measurements

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Validating satellite-derived land surface temperature over mountainous area with in situ measurements

  • 1. Validating satellite-derived land surface temperature over mountainous area with in situ measurements Imlil Valley (High Atlas) - Morocco Yoann Malbéteau CESBIO / Toulouse yoann.malbeteau@cesbio.cnes.fr http://rec.isardsat.com Merlin O., Gascoin S., Gastellu J.P., Mattar, C. Olivera L., Khabba S., Jarlan L.
  • 2. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques 1 of 15 Temperature of Earth's lands during the daytime April 2016 marks 12th consecutive month of record warmth for globe (NOAA) Climatic scale Land & Ocean temperature Percentiles Jan-April 2016 NOAA’s National centers for Environmental Information Data Source: GHCN-M version 3.3.0 & ERSST version 4.0.0 Record Warmest Much Warmer than average Warmer than average Near average Much Cooler than average Cooler than average Record Coldest Over land: +2.33°C Over land and ocean: +1.11°C above the 20th century average
  • 3. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques 2 of 15 Land surface temperature for agriculture…. Evapotranspiration estimation / Soil moisture downscaling amongst of others… Regional and parcel scale ASTER temperature (90 m) ET (mm/day) 0 108642 Olivera-Guerra L. et al. (2014)
  • 4. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques 2 of 15 Land surface temperature for agriculture…. Evapotranspiration estimation / Soil moisture downscaling amongst of others… Regional and parcel scale SMOS Product Soil moisture Disaggregated 82 000 km2 ASTER temperature (90 m) MODIS land surface temperature (1 km) ET (mm/day) 0 108642 Olivera-Guerra L. et al. (2014) Malbeteau Y. et al. (2016) 6050 km2
  • 5. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques What’s land surface temperature ? LST (Land Surface Temperature) NDVI Soil Moisture Albedo texture ET Meteo Topo 3 of 15
  • 6. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques What’s land surface temperature ? LST (Land Surface Temperature) NDVI Soil Moisture Albedo texture ET Meteo Topo 3 of 15 LST landsat at 100m resolution 05 Septembre 2014 Lake Mountains Clouds 55 40 30 25 50 45 35 T °C
  • 7. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques What’s land surface temperature over mountains? 4 of 15 Illumination Elevation
  • 8. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Land surface temperature over mountains 5 of 15 Aremd station Northing Easting Elevation 1400 0 W.m-2 Net Radiation at 8m (from DART model) at 11h21, the 05th of September 6 km
  • 9. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Land surface temperature over mountains 6 of 15 45 30 20 15 40 35 25 T °CSun-exposed slope Shadowed slope Vegetation River Land surface temperature observed by ASTER satellite 6 km
  • 10. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Scheme placement … 7 of 15 Temperature sensors/loggers Different illumination and elevation Spacing: ~100m (ASTER/landsat resolution) 6 months 45 30 20 15 40 35 25 T °C
  • 11. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques How can we validate surface temperature ? 8 of 15 Temperature sensors/loggers ibutton sensor 135 ibuttons Set up over 45 points Locations of the 45 ibutton plates, each of them containing 3 ibutton sensors. Red cross indicate plates not used for the study.
  • 12. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Results: sample of in situ surface temperature 9 of 15 Date (mm/dd/2014) Surfacetemperature(°C) Sun exposed shadow exposed
  • 13. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Results: sample of in situ surface temperature Date (mm/dd/2014) Surfacetemperature(°C) Sun exposed shadow exposed 14°C 5°C 9 of 15
  • 14. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Results: sample of in situ surface temperature Date (mm/dd/2014) Surfacetemperature(°C) lag time 9 of 15 Sun exposed shadow exposed
  • 15. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Results: sample of in situ surface temperature Date (mm/dd/2014) Surfacetemperature(°C) Cloudy day 9 of 15
  • 16. Energy balance Transpiration Evaporation land surface temperature 𝑻 𝑬𝑩 = 𝒇𝒗 𝑻𝒗 𝑬𝑩 + 𝟏 − 𝒇𝒗 𝑻𝒔 𝑬𝑩 Based on double source (vegetation/soil) energy balance model 𝑻𝒔 𝑬𝑩 = 𝒇𝒔𝒔 𝑻𝒔, 𝒅𝒓𝒚 𝑬𝑩 + 𝟏 − 𝒇𝒔𝒔 𝑻𝒔, 𝒘𝒆𝒕 𝑬𝑩 𝑻𝒗 𝑬𝑩 = 𝒇𝒔𝒗 𝑻𝒗, 𝒅𝒓𝒚 𝑬𝑩 + 𝟏 − 𝒇𝒔𝒗 𝑻𝒗, 𝒘𝒆𝒕 𝑬𝑩 Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Modeling topographic effect over mountains 10 of 15
  • 17. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Modeling topographic effect over mountains ASTER LST simulated LST 45 30 20 15 40 35 25 T °C 90 m resolution 8 m resolution Representativeness 11 of 15 6 km6 km
  • 18. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Useful for model and observed data validation 14th April 2014 30th April 2014 05th September 2014 Simulated LST ASTER LST R (correlation) 14th April 30th April 05th September Simulated LST 0.75 0.68 0.64 Observed LST 0.64 0.68 0.67 Scatterplots of ASTER and simulated LST at 90m resolution versus ibutton measurements 12 of 15
  • 19. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Useful for model and observed data validation 14th April 2014 30th April 2014 05th September 2014 Simulated LST ASTER LST R (correlation) 14th April 30th April 05th September Simulated LST 0.75 0.68 0.64 Observed LST 0.64 0.68 0.67 B (bias) 14th April 30th April 05th September Simulated LST 1.48 2.74 -0.43 Observed LST 3.04 3.38 0.78 Scatterplots of ASTER and simulated LST at 90m resolution versus ibutton measurements 12 of 15
  • 20. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Additional slide…. for future application over mountains 45 30 20 15 40 35 25 T °C Before correction After correction 13 of 15
  • 21. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Conclusion Challenges: Representativeness of in situ measurement for remote sensing data validation solution ? very dense in situ measurement  aggregation few in situ measurement  disaggregation (downscaling) in situ measurement representative at the scale resolution 14 of 15
  • 22. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Conclusion Challenges: Representativeness of in situ measurement for remote sensing data validation solution ? very dense in situ measurement  aggregation few in situ measurement  disaggregation (downscaling) in situ measurement representative at the scale resolution intercomparison between remotely sensed data 14 of 15
  • 23. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Conclusion Challenges: Representativeness of in situ measurement for remote sensing data validation solution ? very dense in situ measurement  aggregation few in situ measurement  disaggregation (downscaling) in situ measurement representative at the scale resolution intercomparison between remotely sensed data Terrain accessibility … “When science goes messy” 14 of 15
  • 24. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Conclusion Challenges: Representativeness of in situ measurement for remote sensing data validation solution ? very dense in situ measurement  aggregation few in situ measurement  disaggregation (downscaling) in situ measurement representative at the scale resolution intercomparison between remotely sensed data Terrain accessibility … “When science goes messy” 14 of 15
  • 25. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Conclusion Challenges: Representativeness of in situ measurement for remote sensing data validation solution ? very dense in situ measurement  aggregation few in situ measurement  disaggregation (downscaling) in situ measurement representative at the scale resolution intercomparison between remotely sensed data Terrain accessibility … “When science goes messy” 14 of 15
  • 26. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Conclusion Challenges: Representativeness of in situ measurement for remote sensing data validation solution ? very dense in situ measurement  aggregation few in situ measurement  disaggregation (downscaling) in situ measurement representative at the scale resolution intercomparison between remotely sensed data Terrain accessibility … “When science goes messy” 14 of 15
  • 27. Validació de dades teletransportades en camp; Aplicacions agrícoles i hidrogeològiques Conclusion Challenges: Representativeness of in situ measurement for remote sensing data validation solution ? very dense in situ measurement  aggregation few in situ measurement  disaggregation (downscaling) in situ measurement representative at the scale resolution intercomparison between remotely sensed data Terrain accessibility But it is great … 14 of 15
  • 28. Validating satellite-derived land surface temperature over mountainous area with in situ measurements