Deriving Snow Depth From ICESat-2 Lidar Multiple Scattering Measurements: Uncertainty Analyses
نویسندگان
چکیده
The application of diffusion theory and Monte Carlo lidar radiative transfer simulations presented in Part I this series study suggests that snow depth can be derived from the first-, second- third-order moments backscattering pathlength distribution. These methods are now applied to satellite ICESat-2 measurements over Arctic sea ice land surfaces Northern Hemisphere. Over ice, retrieved depths agree well with co-located IceBridge radar measured values a root-mean-square (RMS) difference 7.8 cm or 29.2% mean depth. terrestrial show drastic spatial variation snowpack along ground tracks Hemisphere, which consistent University Arizona (UA) Canadian Meteorological Centre (CMC) gridded daily products. RMS between UA products is 14 cm, 28% To better understand these results, we also discuss possible sources errors depths, including surface roughness within laser footprint, atmospheric forward scattering, solar background noise, detector dark current. Simulation results indicate would less than 5 if standard deviation pulse spreading due 50 cm. Our demonstrate used reliably derive depth, critical geophysical parameter for cryosphere studies thickness estimation provides important constraints modeling hydrological processes.
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ژورنال
عنوان ژورنال: Frontiers in remote sensing
سال: 2022
ISSN: ['2673-6187']
DOI: https://doi.org/10.3389/frsen.2022.891481