
Simulations of Polarimetric, X-Band Radar Signatures in Supercells. Part I: Description of Experiment and Simulated ρhv Rings
Author(s) -
Jeffrey C. Snyder,
Howard B. Bluestein,
Daniel T. Dawson,
Youngsun Jung
Publication year - 2017
Publication title -
journal of applied meteorology and climatology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.079
H-Index - 134
eISSN - 1558-8432
pISSN - 1558-8424
DOI - 10.1175/jamc-d-16-0138.1
Subject(s) - radar , polarimetry , x band , physics , meteorology , storm , weather radar , observable , convective storm detection , convection , computational physics , geology , remote sensing , computer science , optics , scattering , telecommunications , quantum mechanics
With the development of multimoment bulk microphysical schemes and polarimetric radar forward operators, one can better examine convective storms simulated in high-resolution numerical models from a simulated polarimetric radar perspective. Subsequently, relationships between observable and unobservable quantities can be examined that may provide useful information about storm intensity and organization that otherwise would be difficult to obtain. This paper, Part I of a two-part sequence, describes the bulk microphysics scheme, polarimetric radar forward operator, and numerical model configuration used to simulate supercells in eight idealized, horizontally homogenous environments with different wind profiles. The microphysical structure and evolution of copolar cross-correlation coefficient (ρ hv ) rings associated with simulated supercells are examined in Part I, whereas Part II examines Z DR columns, Z DR rings, and K DP columns. In both papers, some systematic differences between the signature seen at X and S bands are discussed. The presence of hail is found to affect ρ hv much more at X band than at S band (and is found to affect Z DR more at S band than at X band), which corroborates observations. The ρ hv half ring is found to be associated with the presence of large, sometimes wet, hail aloft, with an ~20-min time lag between increases in the size of the ρ hv ring aloft and the occurrence of a large amount of hail near the ground in some simulations.