Soil emissivity of Arctic regions is a key parameter for assessing surface properties from microwave brightness temperature(Tb)measurements.Particularly in winter,frozen soil permittivity and roughness are two poorly ...Soil emissivity of Arctic regions is a key parameter for assessing surface properties from microwave brightness temperature(Tb)measurements.Particularly in winter,frozen soil permittivity and roughness are two poorly characterized unknowns that must be considered.Here,we show that after removing snow,the 3D soil roughness can be accurately inferred from in-situ photogrammetry using Structure from Motion(SfM).We focus on using SfM techniques to provide accurate roughness measurements and improve emissivity models parametrization of frozen arctic soil for microwave applications.Validation was performed from ground-based radiometric measurements at 19 and 37 GHz using three different soil emission models:the Wegmüller and Mätzler[1999,TGRS]model(Weg99),the Wang and Choudhury[1981,JGR]model(QNH),and a geometrical optics model(Geo Optics).Measured and simulated brightness temperatures over different tundra and rock sites in the Canadian High Arctic show that Weg99,parametrized with SfM-based roughness and optimized permittivity(1),yielded an RMSE of 3.1 K(R2=0.71)for all frequencies and polarizations.Our SfM based approach allowed us to measure roughness with 0.1 mm accuracy at 55 locations of different land cover type using a digital camera and metal plates of know dimensions.展开更多
基金This research was made possible thanks to the financial support of the Natural Sciences and Engineering Research Council of Canada(NSERC)Polar Knowledge Canada,Canada Foundation for Innovation(CFI)+2 种基金Fonds québécois de la recherche sur la nature et les technologies(FRQNT-Québec)Northern Scientific Training Program(NSTP)Environment and Climate Change Canada Grant and Contribution program and research funding from Northumbria University,UK.
文摘Soil emissivity of Arctic regions is a key parameter for assessing surface properties from microwave brightness temperature(Tb)measurements.Particularly in winter,frozen soil permittivity and roughness are two poorly characterized unknowns that must be considered.Here,we show that after removing snow,the 3D soil roughness can be accurately inferred from in-situ photogrammetry using Structure from Motion(SfM).We focus on using SfM techniques to provide accurate roughness measurements and improve emissivity models parametrization of frozen arctic soil for microwave applications.Validation was performed from ground-based radiometric measurements at 19 and 37 GHz using three different soil emission models:the Wegmüller and Mätzler[1999,TGRS]model(Weg99),the Wang and Choudhury[1981,JGR]model(QNH),and a geometrical optics model(Geo Optics).Measured and simulated brightness temperatures over different tundra and rock sites in the Canadian High Arctic show that Weg99,parametrized with SfM-based roughness and optimized permittivity(1),yielded an RMSE of 3.1 K(R2=0.71)for all frequencies and polarizations.Our SfM based approach allowed us to measure roughness with 0.1 mm accuracy at 55 locations of different land cover type using a digital camera and metal plates of know dimensions.
