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The algorithm shows encouraging performance for the delineation of raining area in middle latitudes.
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Open image in new window Fig. 6 Delineated rain area for the scene from Mars 09, 2011 (12 30 UTC). a BT10.8 image, b rain area delineated by Radar and MLP c rain area detected by Radar and ECST.
Heavy rain accompanies the atmospheric disturbance, and the rain area may correspond to MR amplitude enhancements.
Correlation scales were analyzed for a rain-free area, weak rain area, and heavy rain area, by dividing the rain rates (R [mm/h]) into the three intensity levels, i.e., R < 0.1, 0.1 ≤ R < 10, and R ≥ 10.
Open image in new window Fig. 3 MLP for rain area delineation.
Figure 6c shows the rain area classified by both the ECST and radar.
To achieve this aim, we use a new Convective/Stratiform Rain Area Delineation Technique (CS-RADT).
Models are validated against independent rainy days during November 2009 to March 2010, not used for training the rain area delineation algorithms.
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