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NPOL: GPM Precipitation Science Research Facility

Quasi-Vertical Profile

A quasi-vertical profile (QVP) is a conical scan at 20.0 degrees elevation. The reflectivity, differential reflectivity, correlation, and differential phase are azimuthally averaged by range bin, and are presented in a height-versus-time format. A height of 10 km is approximately 30 km range from NPOL (see figure). Per Ryzhkov et al. 2016, the temporal evolution of microphysical processes that govern precipitation is a key benefit to this methodology. Through this technique, NPOL will be monitoring characteristics and behavior of the melting layer, regions of dendritic growth, riming, and snow aggregation with high vertical resolution. Comparisons with vertically looking remote sensors such as the Micro-Rain-Radar (MRR) and the GPM Dual-Frequency Precipitation Radar (DPR) will be performed for validation within the atmospheric column.
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Reference:
Ryzhkov A.V., P. Zhang, H. Reeves, M. Kumjian, T. Tschallener, S. Tromel, and C. Simmer, 2016: Quasi-Vertical Profiles - A new way to look at polarimetric radar data. J. Atmos. Oceanic Technol., 33, 551-562.


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