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Refractivity During IHOP_2002. Tammy M. Weckwerth (NCAR/ATD), Crystalyne R. Pettet (NCAR/ATD), Frédéric Fabry (McGill University), ShinJu Park (McGill University) and James W. Wilson (NCAR/ATD). Intercomparisons. Fixed and mobile surface stations AERIBAGO SRL Aircraft. Intercomparisons.
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Refractivity During IHOP_2002 Tammy M. Weckwerth (NCAR/ATD), Crystalyne R. Pettet (NCAR/ATD), Frédéric Fabry (McGill University), ShinJu Park (McGill University) and James W. Wilson (NCAR/ATD)
Intercomparisons • Fixed and mobile surface stations • AERIBAGO • SRL • Aircraft
Intercomparisons Mean Bias Stn-Radar = 1.68 N units
Intercomparisons Bias is not related to propagation effects since it’s not diurnally dependent Bias is worse at higher humidities
Surface Station Intercomparisons • Excellent correlations • Radar has negative bias
Mobile Mesonet comparisons Correlation = 0.81
AERIBAGO comparisons Correlation=0.89 Correlation=0.75 Correlation=0.42
UWKA comparisons Correlation drop occurs between 358 m leg (0.96) and 673 m leg (0.74) Correlation=0.93
Summary • Radar Refractivity may be a proxy for water vapor during the warm season. • Radar Refractivity shows excellent correlation with surface station and aircraft refractivity. • Radar Refractivity has a low bias vs fixed surface stations • Vertical depth represented appears to be lower levels of the ABL (<~300 m?). • Horizontal resolution is approximately 4 km (although it sometimes appears better).
Ongoing Work • Evaluate accuracy of low-level refractivity retrieval • Fixed and mobile mesonets • Plan to: Add GPS intercomparisons • Plan to: Add DRI MMR intercomparisons • Evaluate layer over which refractivity retrieval is representative • Aircraft in situ measurements • SRL intercomparisons • AERI intercomparisons • Plan to: Add Sounding & Dropsonde comparisons • Plan to: Add horizontal and vertical pointing airborne DIAL • Plan to: Add TAOS intercomparisons • Possibly add: MIPS profiling radiometer intercomparisons • Plan to: Evaluate two more days in detail
2 km 11 km Correlation=0.88
S-Pol Refractivity Retrieval dryline dryline cool/moist • Variations in q, T and p • Boundary detection • Advection • Pettet et al., next; • Fabry and Park, 1700 warm/dry
Refractivity: One Day After Heavy RainfallAircraft in-situ data Northern edge of aircraft track Ts=45 deg C, Theta60=307 K, q60 = 8.5 g/kg warm/dry Southern edge of aircraft track Ts=32 deg C, Theta60=306.2 K, q60 = 11 g/kg cool/moist
warm/dry cool/moist
Surface station comparisons Correlation = 0.99
Correlation = 0.92 Correlation = 0.98