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Stephanie M. Wingo, Walter A. Petersen, Patrick N. Gatlin, Charanjit S. Pabla, David A. Marks, and David B. Wolff

overpass is such that a single scan from the DPR (row of pixels with the same observation time) is in near-perfect alignment with the 230°/50° RHI from the NPOL and D3R (note the NPOL 50° RHI line is perpendicular to the DPR swath lines in Fig. 4b ). For this example, we will consider variations in the vertical profile along this line, extending up the Quinault River Valley. Fig . 4. Overview of 3 Dec 2015 OLYMPEX GPM overpass case. (a) Regional view of GPM GMI (red) and DPR (green) swath lines over

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M. Petracca, L. P. D’Adderio, F. Porcù, G. Vulpiani, S. Sebastianelli, and S. Puca

Measurement precipitation processing system: File specification 2ADPR. NASA/JAXA Tech. Rep., 127 pp., https://storm.pps.eosdis.nasa.gov/storm/data/docs/filespec.GPM.V1.2ADPR.pdf . Nash , J. E. , and J. V. Sutcliff , 1970 : River flow forecasting through conceptual models 1: A discussion of principles . J. Hydrol. , 10 , 282 – 290 , https://doi.org/10.1016/0022-1694(70)90255-6 . 10.1016/0022-1694(70)90255-6 Neeck , S. P. , R. K. Kakar , A. A. Azarbarzin , and A. Y. Hou , 2014 : Global

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