A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2017; you can also visit the original URL.
The file type is application/pdf
.
Global Snow Mass Measurements and the Effect of Stratigraphic Detail on Inversion of Microwave Brightness Temperatures
[chapter]
2013
Space Sciences Series of ISSI
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:10.1007/978-94-017-8789-5_14
fatcat:k3pf4l7cxjbfdgqd64nnok5mum