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Global Snow Mass Measurements and the Effect of Stratigraphic Detail on Inversion of Microwave Brightness Temperatures
2013
Surveys in geophysics
Snow provides large seasonal storage of freshwater, and information about the distribution 6 of snow mass as Snow Water Equivalent (SWE) is important for hydrological planning and detecting 7 climate change impacts. Large regional disagreements remain between estimates from reanalyses, 8 remote sensing and modelling. Assimilating passive microwave information improves SWE estimates 9 in many regions but the assimilation must account for how microwave scattering depends on snow 10 stratigraphy.
doi:10.1007/s10712-013-9263-x
fatcat:3szz4iminnaz7gh54jnjuapa7i