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Evaluating the H-Q model using a numerical approach based on the Finite Element Method

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SMOS SCIENCE WORKSHOP 27-29 September 2011

Arles – France

Evaluating the H-Q model using a numerical approach based on the Finite Element Method

H. Lawrence, F. Demontoux, J.-P. Wigneron, A. Mialon, Y.Kerr

The L-MEB model currently used in the SMOS inversion algorithm relates the emissivity of a bare soil to roughness parameters through the semi-empirical H-Q model. The developed model has four retrieval parameters: H

R

, Q

R

, N

RV

and N

RH

. The parameter H

R

governs the increase in emissivity, Q

R

governs the polarization mixing and N

RV

and N

RH

govern the change in the emissivity’s angular dependence at V and H polarization respectively, all of which effects are caused by surface roughness. These parameters are empirical and must be calibrated for use in the SMOS algorithm. So far they have not been conclusively linked to surface roughness values such as the standard deviation of surface heights, σ, or the autocorrelation length, L

c

. It has been suggested recently that H

R

can be linked directly to σ (Wigneron et al 2011) but this has yet to be confirmed, neither with datasets from other experimental sites nor with modelling studies.

In this paper we present a modelling study to evaluate the accuracy of the Q-H model in

general and in particular whether its parameters may be linked to geometrical roughness terms

σ and L

c

. We use a numerical modelling approach based on the Finite Element Method which

has been recently presented and validated by comparison with Method of Moments

calculations (Lawrence et al 2011). However this is a new approach that has not yet been

compared to experimental data so we begin by comparing results of the calculated emissivity

to the SMOSREX 2006 dataset (Mialon et al 2011). Once this has been done we then use the

model to calculate the emissivity for a range of different roughness values, soil moisture

values, measurement angles and for both H and V polarizations. We invert the parameters H

R

,

Q

R

, N

RV

and N

RH

from all calculated emissivity values and evaluate their relationship to all

variables, including σ, L

c

, measurement angle, soil moisture and polarization.

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SMOS SCIENCE WORKSHOP 27-29 September 2011

Arles – France

References:

J.-P. Wigneron, A. Chanzy, Y. H. Kerr, H. Lawrence, J. Shi, M. J. Escorihuela, V. Mironov, A. Mialon, F. Demontoux, P. de Rosnay, and K. Saleh-Contell, “Evaluating an Improved Parameterization of the Soil Emission in L-MEB”, IEEE Trans. Geosci. Remote Sens, vol. 49 (4), pp. 1177 – 1189, Apr 2011.

H. Lawrence, F. Demontoux, J.-P. Wigneron, P. Paillou, T.-D. Wu and Y. H. Kerr,

"Evaluation of a Numerical Modeling Approach based on the Finite Element Method for calculating the Rough Surface Scattering and Emission of a soil layer" IEEE Trans. Geosci.

Remote Sens Lett, in press

A. Mialon, J.-P. Wigneron, P. de Rosnay, M. J. Escorihuela, and Y. H. Kerr, “Evaluating the

L-MEB model from long term microwave measurements over a rough field, SMOSREX

2006,” submitted Apr 2011

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