Japan Geoscience Union Meeting 2025

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-CG Complex & General

[A-CG41] Satellite Earth Environment Observation

Thu. May 29, 2025 9:00 AM - 10:30 AM Exhibition Hall Special Setting (5) (Exhibition Hall 7&8, Makuhari Messe)

convener:Riko Oki(Japan Aerospace Exploration Agency), Yoshiaki HONDA(Center for Environmental Remote Sensing, Chiba University), Tsuneo Matsunaga(Center for Global Environmental Research and Satellite Observation Center, National Institute for Environmental Studies), Nobuhiro Takahashi(Institute for Space-Earth Environmental Research, Nagoya University), Chairperson:Hiroshi Murakami(Earth Observation Research Center, Japan Aerospace Exploration Agency), Yoshiaki HONDA(Center for Environmental Remote Sensing, Chiba University)

10:00 AM - 10:15 AM

[ACG41-11] A Roadmap to Global High Spatial/Temporal Resolution Snow Depth Survey Through Synergistic Active/Passive Optical Spectral Measurements

*Yongxiang Hu1 (1.NASA Langley Research Center, Hampton, Virginia 23681, USA)

Keywords:snow depth , snow density, lidar , spectrometer, machine learning

In our previous articles (Hu et al., 2022; Lu et al., 2022, Hu et al., 2023), we introduced a theoretical snow depth and snow density measurements concept using lidar measurements. The key findings of these studies are: (1) snow depth and snow density are linked to the probability distribution of diffused photon scattering inside snow; (2) when absorption can be ignored, the averaged photon pathlength of laser light or sunlight traveling inside snow is twice of the snow depth; (3) snow density also affect spectral absorptions and the higher order statistics of the diffused photon pathlength distribution.

Spectral reflectance, R(k), of sunlight is a Laplace transform of the diffuse photon pathlength probability, p(L), from pathlength domain to the absorption coefficient, k. The averaged pathlength, <L>, can be derived from the derivatives of R(k). Thus, snow depth can be derived from spectral reflectance of sunlight. Snow depths can be derived with machine learning that uses lidar measurements of snow depth to train the collocated spectral solar reflectance measurements, and the algorithm can be applied to broad swath, high spatial resolution spectral imaging measurements from space.

This presentation describes the theory behind the measurements and demonstrates the concept with collocated PACE and ICESat-2 observations.