June 26th 2003
On 25 June, two convective lines began to develop over
north-central and southwest Oklahoma. The more northern line evolved into a
squall line, producing locally heavy amounts of rainfall. These lines moved
southeastward across Oklahoma between 20 GMT 25 June and 13 GMT 26 June. A new
region of convective cells developed over southwest Oklahoma during the later
morning hours of 26 June, producing light rainfall.
VCP 45b (set #1) - EL=0.5 deg
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VCP 45b (set #1) - EL=1.45 deg
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VCP 45b (set #1) - EL=2.4 deg
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LONG STAGGERED PRT |

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MEDIUM STAGGERED PRT |

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SHORT STAGGERED PRT |

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VCP 45b (set #2) - EL=0.5 deg
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UNIFORM PRT |

Reflectivity |

Velocity |

Spectrum Width |
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LONG STAGGERED PRT |

Reflectivity |

Velocity |

Spectrum Width |
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MEDIUM STAGGERED PRT |

Reflectivity |

Velocity |

Spectrum Width |
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SHORT STAGGERED PRT |

Reflectivity |

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Spectrum Width |
VCP 45b (set #2) - EL=1.45 deg
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UNIFORM PRT |

Reflectivity |

Velocity |

Spectrum Width |
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LONG STAGGERED PRT |

Reflectivity |

Velocity |

Spectrum Width |
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MEDIUM STAGGERED PRT |

Reflectivity |

Velocity |

Spectrum Width |
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SHORT STAGGERED PRT |

Reflectivity |

Velocity |

Spectrum Width |
VCP 45b (set #2) - EL=2.4 deg
|
UNIFORM PRT |

Reflectivity |

Velocity |

Spectrum Width |
|
LONG STAGGERED PRT |

Reflectivity |

Velocity |

Spectrum Width |
|
MEDIUM STAGGERED PRT |

Reflectivity |

Velocity |

Spectrum Width |
|
SHORT STAGGERED PRT |

Reflectivity |

Velocity |

Spectrum Width |