Affiliation:
1. Department of Atmospheric Sciences, University of North Dakota, Grand Forks, North Dakota
2. School of Meteorology, University of Oklahoma, Norman, Oklahoma
Abstract
This study presents a new storm classification method for objectively stratifying three-dimensional radar echo into five categories: convection, convective updraft, precipitating stratiform, nonprecipitating stratiform, and ice-only anvil. The Storm Labeling in Three Dimensions (SL3D) algorithm utilizes volumetric radar data to classify radar echo based on storm height, depth, and intensity in order to provide a new method for updraft classification and improve upon the limitations of traditional storm classification algorithms. Convective updrafts are identified by searching for three known polarimetric radar signatures: weak-echo regions (bounded and unbounded) in the radar reflectivity factor at horizontal polarization ([Formula: see text]), differential radar reflectivity ([Formula: see text]) columns, and specific differential phase ([Formula: see text]) columns. Additionally, leveraging the three-dimensional information allows SL3D to improve upon missed identifications of weak convection and intense stratiform rain in traditional two-dimensional classification schemes. This study presents the results of applying the SL3D algorithm to several cases of high-resolution three-dimensional composites of NEXRAD WSR-88D data in the contiguous United States. Comparisons with a traditional algorithm that uses two-dimensional maps of [Formula: see text] are also shown to illustrate the differences of the SL3D algorithm.
Funder
National Science Foundation
Publisher
American Meteorological Society
Cited by
37 articles.
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