Articles | Volume 11, issue 7
Geosci. Model Dev., 11, 2763–2788, 2018
Geosci. Model Dev., 11, 2763–2788, 2018

Model description paper 11 Jul 2018

Model description paper | 11 Jul 2018

SMRT: an active–passive microwave radiative transfer model for snow with multiple microstructure and scattering formulations (v1.0)

Ghislain Picard et al.

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Cited articles

Abdalati, W. and Steffen, K.: Snowmelt on the Greenland Ice Sheet as Derived from Passive Microwave Satellite Data, J. Climate, 10, 165–175, 1997.
Abdalati, W. and Steffen, K.: Accumulation and hoar effects on microwave emission on the Greenland ice sheet dry snow zones, J. Glaciol., 44, 523–531, 1998.
Andreadis, K. M. and Lettenmaier, D. P.: Implications of Representing Snowpack Stratigraphy for the Assimilation of Passive Microwave Satellite Observations, J. Hydrometeorol., 13, 1493–1506,, 2012.
Arthern, R. J., Winebrenner, D. P., and Vaughan, D. G.: Antarctic snow accumulation mapped using polarization of 4.3-cm wavelength microwave emission, J. Geophys. Res., 111, D06107,, 2006.
Barre, H. M. J. P., Duesmann, B., and Kerr, Y. H.: SMOS: The Mission and the System, IEEE T. Geosci. Remote, 46, 587–593,, 2008.
Short summary
The Snow Microwave Radiative Transfer (SMRT) is a novel model developed to calculate how microwaves are scattered and emitted by snow. The model is built from separate, interconnecting modules to make it easy to compare different aspects of the theory. SMRT is the first model to allow a choice of how to represent the microstructure of the snow, which is extremely important, and has been used to unite multiple previous studies. This model will ultimately be used to observe snow from space.