A detailed look at the MOD16 ET algorithm Natalie Schultz Heat budget group meeting 7/11/13.

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Presentation transcript:

A detailed look at the MOD16 ET algorithm Natalie Schultz Heat budget group meeting 7/11/13

MOD16 Global 1km 2 dataset of ET, LE, PET, PLE for million km 2 of global vegetated land Computed daily Produced at 8-day, monthly, annual intervals Available from Currently available through group’s website: U Montana. According to Mu 2011, this algorithm has been submitted to NASA for full review to be available through the MODIS Land product DAAC.

Remote sensing ET methods 1)Empirical or statistical methods – link measured or estimated ET with remotely sensed vegetation indices 2)Physical models that calculate ET as the residual of the surface energy balance (SEB) – relies heavily on LST measurements 3)Other physical models such as Penman-Monteith that include the main drivers of ET – includes surface energy partitioning processes & environmental constraints on ET – not overly sensitive to any one input

Penman-Monteith equation λE = latent heat flux λ = latent heat of evaporation s = d(e sat )/dT A = available energy ρ = air density C p = specific heat capacity of air r a = aerodynamic resistance r s = surface resistance γ = psychrometric constant

ET algorithm logic Mu, et al. 2011

Data sources MODIS data Land cover type (MOD12Q1) FPAR & LAI (MOD15A2) albedo (MOD43C1) Linear interpolation used to fill missing/unreliable data Meteorological data 1.0 ° × 1.25 ° GMAO – solar radiation – air temperature – air pressure – humidity non-linearly interpolated to 1km 2 pixel level based on four surrounding pixels

Gap filling & Interpolation Zhao, et al. 2005

MODIS Land Cover Type Biome Properties Look-Up Table (BPLUT) Mu, et al. 2011

MODIS FPAR & LAI

MODIS Albedo

ET components wet canopy fraction (Fwet) estimated from relative humidity partitioned using vegetation fraction estimated from FPAR

Results Mu, et al. 2011

Old version vs. improved version Mu, et al. 2011

Comparison with flux towers Mu, et al. 2011

Uncertainties 1)Input data uncertainties 2)Inaccuracies in measured data 3)Flux tower vs. MODIS footprint size 4)Algorithm limitations/assumptions 5)Land cover misclassifications

Conclusions MOD16 useful tool for examining global terrestrial water and energy cycles, and environmental change. At smaller spatial scales, there may be biases between MOD16 and surface measurements. Validation using surface measurements.