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Estimating ice phenology on large northern lakes from AMSR-E: algorithm development and application to Great Bear Lake and Great Slave Lake, Canada

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Academic year: 2017

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Fig. 1. Map showing location of Great Bear Lake (GBL) and Great Slave Lake (GSL), and their meteorological stations (Deline,  Yel-lowknife, and Hay River) within the Mackenzie River Basin
Fig. 2. Temporal evolution of horizontal (top) and vertical (middle) polarized brightness temperature at 18.7 (light violet), 23.8 (middle violet), 36.5 (dark violet), 89.0 (dark grey) GHz (2003–2004) for sampling site on GBL (see Fig
Fig. 3. Flowchart of ice phenology algorithm based on AMSR- AMSR-E 18.7 GHz horizontal polarization (H-pol) brightness temperature (T B )
Fig. 4. Freeze-onset (FO), ice-on, and freeze-duration on average (2002–2009) for GBL (left panel) and GSL (right panel)
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