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Published byDominick Mason Modified over 5 years ago
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Radar Refractivity: validation and application to forecasting
Crystalyne R. Pettet, Tammy M. Weckwerth, and James W. Wilson—NCAR/ATD Frédéric Fabry and ShinJu Park—McGill University
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Validation
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Sfc comparisons S-Pol N varies most strongly with moisture
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High correlation between S-Pol N and station N
Sfc comparisons High correlation between S-Pol N and station N
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S-Pol N compares favorably with areas of relatively constant mobile N
Mobile mesonets S-Pol N compares favorably with areas of relatively constant mobile N
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S-Pol N gradients are smoothed
Mobile mesonets S-Pol N gradients are smoothed
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UWKA S-Pol N gradient smoothed over ~10 km
S-Pol N compares favorably with areas of relatively constant UWKA N
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AERI—Atmospheric Emitted Radiance Interferometer
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AERI Transition between m from high to low r values
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P-3 If CBL is well-mixed, N represents at least half the depth of the CBL.
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AERI—diurnal and height differences
N bias is strongest at night and improves with mixing of CBL Strongest relationship occurs at low levels
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AERI—diurnal and height differences
Low levels—strong relationship from one hour after sunrise until 2 hours after sunset Increasing height—strong relationship begins later in the morning and drops off by 2200 UTC
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Soundings Similar results to AERI—lowest m
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SRL Strong correspondence between SRL mixing ratio magnitude, surface station mixing ratio, and S-Pol N
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Forecasting Utility
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Boundary development
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CI—10 June 2002
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CI— 10 June 2002
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CI—12-13 June 2002
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CI— June 2002
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Summary Radar refractivity shows excellent correlation with refractivity calculated from other datasets Vertical depth represented by radar refractivity is typically below m AGL, but may be dependent upon the extent of vertical mixing Horizontal scale of refractivity varies, and appears to be as high as 2 km at times and lower than 4 km at other times
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Summary Radar refractivity shows great promise as a potential nowcasting and forecasting tool
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For more information… Contact me at to get a pdf of the manuscript that has been submitted to JAM that this talk is based on.
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