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Melt ponds on Arctic sea ice determined from MODIS satellite data using an artificial neural network

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Figure

Fig. 1. Tracks, locations and dates of validation data sets. Detailed descriptions are given in the text.
Table 1. Spectral reflectances (ri) of surface types used in the un-mixing algorithm (after Tschudi et al., 2008).
Fig. 3. Architecture of the MLP networks used for this study. Theinput layer are the MODIS surface reflectances for the three bands1, 3, and 4
Fig. 4. Seasonal cycle of the relative melt pond fraction from MODIS satellite data for the Arctic for the example of the 2008 melt season.White pixels represent missing data.
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