5
views
0
recommends
+1 Recommend
0 collections
    0
    shares
      • Record: found
      • Abstract: found
      • Article: found
      Is Open Access

      Evaluation of VIIRS and MODIS Snow Cover Fraction in High-Mountain Asia Using Landsat 8 OLI

      , , , ,
      Frontiers in Remote Sensing
      Frontiers Media SA

      Read this article at

      Bookmark
          There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

          Abstract

          We present the first application of the Snow Covered Area and Grain size model (SCAG) to the Visible Infrared imaging Radiometer Suite (VIIRS) and assess these retrievals with finer‐resolution fractional snow cover maps from Landsat 8 Operational Land Imager (OLI). Because Landsat 8 OLI avoids saturation issues common to Landsat 1–7 in the visible wavelengths, we re-assess the accuracy of the SCAG fractional snow cover maps from Moderate Resolution Imaging Spectroradiometer (MODIS) that were previously evaluated using data from earlier Landsat sensors. Use of the fractional snow cover maps from Landsat 8 OLI shows a negative bias of −0.5% for MODSCAG and −1.3% for VIIRSCAG, whereas previous MODSCAG evaluations found a bias of −7.6% in the Himalaya. We find similar root mean squared error (RMSE) values of 0.133 and 0.125 for MODIS and VIIRS, respectively. The Recall statistic (probability of detection) for cells with more than 15% snow cover in this challenging steep topography was found to be 0.90 for both MODSCAG and VIIRSCAG, significantly higher than previous evaluations based on Landsat 5 Thematic Mapper (TM) and 7 Enhanced Thematic Mapper Plus (ETM+). In addition, daily retrievals from MODIS and VIIRS are consistent across gradients of elevation, slope, and aspect. Different native resolutions of the gridded products at 1 km and 500 m for VIIRS and MODIS, respectively, result in snow cover maps showing a slightly different distribution of values with VIIRS having more mixed pixels and MODIS having 7% more pure snow pixels. Despite the resolution differences, the snow maps from both sensors produce similar total snow-covered areas and snow-line elevations in this region, with R 2 values of 0.98 and 0.88, respectively. We find that the SCAG algorithm performs consistently across various spatial resolutions and that fractional snow cover maps from the VIIRS instruments aboard Suomi NPP, JPPS–1, and JPPS–2 can be a suitable replacement as MODIS sensors reach their ends of life.

          Related collections

          Most cited references62

          • Record: found
          • Abstract: not found
          • Article: not found

          A Model for the Spectral Albedo of Snow. I: Pure Snow

            Bookmark
            • Record: found
            • Abstract: not found
            • Article: not found

            Mapping Chaparral in the Santa Monica Mountains Using Multiple Endmember Spectral Mixture Models

              Bookmark
              • Record: found
              • Abstract: not found
              • Article: not found

              Optical constants of ice from the ultraviolet to the microwave: A revised compilation

                Bookmark

                Author and article information

                Journal
                Frontiers in Remote Sensing
                Front. Remote Sens.
                Frontiers Media SA
                2673-6187
                May 10 2021
                May 10 2021
                : 2
                Article
                10.3389/frsen.2021.647154
                ef85afee-9de0-4cf1-b239-2b1ff59dfeb2
                © 2021

                Free to read

                https://creativecommons.org/licenses/by/4.0/

                History

                Comments

                Comment on this article