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Quantifying uncertainty in radar rainfall estimates using an X-band dual polarisation weather radar

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Figure

Figure 2.1: Variation in retrieved rainfall intensity resulting from the use of different DSD parametrisations
Figure 2.3: Two orthogonal polarised planes in the horizontal (solid) and vertical (dashed)
Figure 2.5: Theoretical variation of differential reflectivity with increasing equivolume diameter at S, C and X-band
Figure 3.1: The modified Meteor 50DX operated by NCAS deployed at the Burn testing site, 30-01-2013
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