Intercomparison of Vertical Structure of Storms Revealed by Ground-Based (NMQ) and Spaceborne Radars (CloudSat-CPR and TRMM-PR)

<table>The vertical profile of reflectivity from Columbia, SC. The blue line indicates the reflectivity values for stratiform precipitation, where the peak shows the brightband level.</table>

The Scientific World Journal

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Figure 5

Figure 5: Intercomparison of Vertical Structure of Storms Revealed by Ground-Based (NMQ) and Spaceborne Radars (CloudSat-CPR and TRMM-PR) 