Value of a Dual-Polarized Gap-Filling Radar in Support of Southern California Post-Fire Debris-Flow Warnings

被引:18
|
作者
Jorgensen, David P. [1 ]
Hanshaw, Maiana N. [2 ]
Schmidt, Kevin M. [2 ]
Laber, Jayme L. [3 ]
Staley, Dennis M. [4 ]
Kean, Jason W. [4 ]
Restrepo, Pedro J. [5 ]
机构
[1] NOAA, NSSL, WRDD, Norman, OK 73072 USA
[2] US Geol Survey, Menlo Pk, CA 94025 USA
[3] NOAA, Natl Weather Serv, Oxnard, CA USA
[4] US Geol Survey, Cent Reg Geol Hazards Team, Denver, CO 80225 USA
[5] NOAA, Natl Weather Serv, Off Hydrol Dev, Silver Spring, MD 20910 USA
关键词
RAINFALL RATE ESTIMATION; BAND POLARIMETRIC RADAR; RECENTLY BURNED AREAS; C-BAND; DIFFERENTIAL REFLECTIVITY; ATTENUATION; PRECIPITATION; ALGORITHM; WSR-88D; PROTOTYPE;
D O I
10.1175/JHM-D-11-05.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A portable truck-mounted C-band Doppler weather radar was deployed to observe rainfall over the Station Fire burn area near Los Angeles, California, during the winter of 2009/10 to assist with debris-flow warning decisions. The deployments were a component of a joint NOAA-U.S. Geological Survey (USGS) research effort to improve definition of the rainfall conditions that trigger debris flows from steep topography within recent wildfire burn areas. A procedure was implemented to blend various dual-polarized estimators of precipitation (for radar observations taken below the freezing level) using threshold values for differential reflectivity and specific differential phase shift that improves the accuracy of the rainfall estimates over a specific burn area sited with terrestrial tipping-bucket rain gauges. The portable radar outperformed local Weather Surveillance Radar-1988 Doppler (WSR-88D) National Weather Service network radars in detecting rainfall capable of initiating post-fire runoff-generated debris flows. The network radars underestimated hourly precipitation totals by about 50%. Consistent with intensity duration threshold curves determined from past debris-flow events in burned areas in Southern California, the portable radar-derived rainfall rates exceeded the empirical thresholds over a wider range of storm durations with a higher spatial resolution than local National Weather Service operational radars. Moreover, the truck-mounted C-band radar dual-polarimetric-derived estimates of rainfall intensity provided a better guide to the expected severity of debris-flow events, based on criteria derived from previous events using rain gauge data, than traditional radar-derived rainfall approaches using reflectivity rainfall relationships for either the portable or operational network WSR-88D radars. Part of the reason for the improvement was due to siting the radar closer to the burn zone than the WSR-88Ds, but use of the dual-polarimetric variables improved the rainfall estimation by similar to 12% over the use of traditional Z-R relationships.
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页码:1581 / 1595
页数:15
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