An Evaluation of Terrain-Based Downscaling of MODIS-Based Fractional Snow- Covered Area Datasets Over the Tuolumne River, CA, Based on LiDAR-Derived Snow Data (Extended Abstract)

TitleAn Evaluation of Terrain-Based Downscaling of MODIS-Based Fractional Snow- Covered Area Datasets Over the Tuolumne River, CA, Based on LiDAR-Derived Snow Data (Extended Abstract)
Publication TypeConference Proceedings
Year of Conference2016
AuthorsCristea, Nicoleta C., and Lundquist Jessica D.
Conference Name84th Annual Western Snow Conference
Date Published2016
Conference LocationSeattle, Washington
Abstract

Remotely-sensed snow covered area (SCA) datasets with both high spatial and temporal resolutions are needed for research, planning, and management of hydrologic and ecologic resources. MODIS-based products provide good temporal resolution (daily), but on coarse scale grids (~463 m). This coarse spatial scale can be refined through applying downscaling procedures, which consist of using the fractional snow cover area product (fSCA, the percentage snow cover within a MODIS pixel area) to assign binary (presence/absence) SCA data on higher resolution grids. Current methods rely on representing ablation effects on snow spatial variability by using topographic radiation-derived slope factors and relative elevation as primary indicators of snow presence/absence (Walters et al., 2015), or a degree-day approach (Li et al., 2015). In both studies satellite-derived data were utilized for model input and validation. Uncertainty associated with the input and validation data in assessing downscaling performance could be better understood if reliable, platform-independent fine scale SCA data were available. Here, we propose such a framework for testing and developing a new downscaling procedure based on LiDAR-derived snow depth data collected over the Tuolumne River watershed, CA. Our new downscaling procedure is based on terrain-derived indices that are representative of both ablation and accumulation, drivers of snow spatial variability in complex terrain. The use of the LiDAR-derived dataset has several advantages over using the satellite data. First, the validation data is more accurate, as LiDAR-derived data are high resolution (1-3m). Second, accurate fSCA datasets can be derived from the high resolution LiDAR-derived snow data at the MODIS scale to be used as input data. Third, the downscaling performance can also be tested over vegetated areas, where LiDAR-derived data is presumably more accurate than the satellite data.

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