In this study, snow slab data collected from the Arctic Snow Microstructure Experiment was used in conjunction with a six-directional flux coefficient model to calculate individual slab absorption and scattering coefficients. These coefficients formed the basis for a new semi-empirical extinction coefficient model, using both frequency and optical diameter as input parameters, along with the complex dielectric constant of snow. Radiometric observations, at 18.7, 21.0, and 36.5 GHz at both horizontal and vertical polarizations, and snowpit data collected as part of the Sodankylä Radiometer Experiment were used to compare and contrast the simulated brightness temperatures produced by the n-HUT snow emission model, utilizing both the original ...
Applications of microwave brightness temperature measurements in meteorology, hydrology,climatology ...
The feasibility of a radiance assimilation using a multi-layered snow physical model to estimate sno...
The feasibility of a radiance assimilation using a multi-layered snow physical model to estimate sno...
In this study, snow slab data collected from the Arctic Snow Microstructure Experiment were used in ...
Global observations of snow cover and snow water equivalent are vitally important for climatological...
The Arctic Snow Microstructure Experiment (ASMEx) took place in Sodankylä, Finland in the winters of...
Spatial variations of snowpack properties are an essential component in flood predictions and water ...
Spatial variations of snowpack properties are an essential component in flood predictions and water ...
Plot-scale brightness temperature (TB) measurements at 6.9, 19, 37, and 89 GHz were acquired in fore...
Microwave emission models are a critical component of snow water equivalent retrieval algorithms app...
Abstract A thermal Microwave Emission Model of Layered Snowpacks (MEMLS) was developed for the frequ...
International audienceTo interpret the snowpack evolution, and in particular to estimate snow water ...
International audienceTo interpret the snowpack evolution, and in particular to estimate snow water ...
International audienceTo interpret the snowpack evolution, and in particular to estimate snow water ...
International audienceTo interpret the snowpack evolution, and in particular to estimate snow water ...
Applications of microwave brightness temperature measurements in meteorology, hydrology,climatology ...
The feasibility of a radiance assimilation using a multi-layered snow physical model to estimate sno...
The feasibility of a radiance assimilation using a multi-layered snow physical model to estimate sno...
In this study, snow slab data collected from the Arctic Snow Microstructure Experiment were used in ...
Global observations of snow cover and snow water equivalent are vitally important for climatological...
The Arctic Snow Microstructure Experiment (ASMEx) took place in Sodankylä, Finland in the winters of...
Spatial variations of snowpack properties are an essential component in flood predictions and water ...
Spatial variations of snowpack properties are an essential component in flood predictions and water ...
Plot-scale brightness temperature (TB) measurements at 6.9, 19, 37, and 89 GHz were acquired in fore...
Microwave emission models are a critical component of snow water equivalent retrieval algorithms app...
Abstract A thermal Microwave Emission Model of Layered Snowpacks (MEMLS) was developed for the frequ...
International audienceTo interpret the snowpack evolution, and in particular to estimate snow water ...
International audienceTo interpret the snowpack evolution, and in particular to estimate snow water ...
International audienceTo interpret the snowpack evolution, and in particular to estimate snow water ...
International audienceTo interpret the snowpack evolution, and in particular to estimate snow water ...
Applications of microwave brightness temperature measurements in meteorology, hydrology,climatology ...
The feasibility of a radiance assimilation using a multi-layered snow physical model to estimate sno...
The feasibility of a radiance assimilation using a multi-layered snow physical model to estimate sno...