Landsat, MODIS, and VIIRS snow cover mapping algorithm performance asvalidated by airborne lidar datasets

被引:31
|
作者
Stillinger, Timbo [1 ]
Rittger, Karl [1 ,2 ]
Raleigh, Mark S. [3 ]
Michell, Alex [1 ]
Davis, Robert E. [4 ]
Bair, Edward H. [1 ]
机构
[1] Univ Calif Santa Barbara, Earth Res Inst, Santa Barbara, CA 93106 USA
[2] Univ Colorado Boulder, Inst Arctic & Alpine Res, Boulder, CO 80309 USA
[3] Oregon State Univ, Coll Earth Ocean & Atmospher Sci, Corvallis, OR 97331 USA
[4] Cold Reg Res & Engn Lab, Hanover, NH 03755 USA
来源
CRYOSPHERE | 2023年 / 17卷 / 02期
关键词
GRAIN-SIZE; WATER EQUIVALENT; IMAGING SPECTROMETER; SIERRA-NEVADA; GAP FRACTIONS; RIVER-BASIN; ALBEDO; AREA; VALIDATION; RESOLUTION;
D O I
10.5194/tc-17-567-2023
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Snow cover mapping algorithms utilizing multispectral satellite data at various spatial resolutions are available, each treating subpixel variation differently. Past evaluations of snow mapping accuracy typically relied on satellite data collected at a higher spatial resolution than the data in question. However, these optical data cannot characterize snow cover mapping performance under forest canopies or at the meter scale. Here, we use 3 m spatial resolution snow depth maps collected on 116 d by an aerial laser scanner to validate band ratio and spectral-mixture snow cover mapping algorithms. Such a comprehensive evaluation of sub-canopy snow mapping performance has not been undertaken previously. The following standard (produced operationally by an agency) products are evaluated: NASA gap-filled Moderate Resolution Imaging Spectroradiometer (MODIS) MOD10A1F, NASA gap-filled Visible Infrared Imaging Radiometer Suite (VIIRS) VNP10A1F, and United States Geological Survey (USGS) Landsat 8 Level-3 Fractional Snow Covered Area. Two spectral-unmixing approaches are also evaluated: Snow-Covered Area and Grain Size (SCAG) and Snow Property Inversion from Remote Sensing (SPIReS), both of which are gap-filled MODIS products and are also run on Landsat 8. We assess subpixel snow mapping performance while considering the fractional snow-covered area (fSCA), canopy cover, sensor zenith angle, and other variables within six global seasonal snow classes. Metrics are calculated at the pixel and basin scales, including the root-mean-square error (RMSE), bias, and F statistic (a detection measure). The newer MOD10A1F Version 61 and VNP10A1F Version 1 product biases (- 7.1 %, -9.5 %) improve significantly when linear equations developed for older products are applied (2.8 %, -2.7 %) to convert band ratios to fSCA. The F statistics are unchanged (94.4 %, 93.1 %) and the VNP10A1F RMSE improves (18.6 % to 15.7 %), while the MOD10A1F RMSE worsens (12.7 % to 13.7 %). Consistent with previous studies, spectral-unmixing approaches (SCAG, SPIReS) show lower biases (-0.1 %, -0.1 %) and RMSE (12.1 %, 12.0 %), with higher F statistics (95.6 %, 96.1 %) relative to the band ratio approaches for MODIS. Landsat 8 products are all spectral-mixture methods with low biases (-0.4 % to 0.3 %), low RMSE (11.4 % to 15.8 %), and high F statistics (97.3 % to 99.1 %). Spectral-unmixing methods can improve snow cover mapping at the global scale.
引用
收藏
页码:567 / 590
页数:24
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