2014
DOI: 10.1175/waf-d-13-00044.1
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Examination of a Real-Time 3DVAR Analysis System in the Hazardous Weather Testbed

Abstract: Forecasters and research meteorologists tested a real-time three-dimensional variational data assimilation (3DVAR) system in the Hazardous Weather Testbed during the springs of 2010-12 to determine its capabilities to assist in the warning process for severe storms. This storm-scale system updates a dynamically consistent three-dimensional wind field every 5 min, with horizontal and average vertical grid spacings of 1 km and 400 m, respectively. The system analyzed the life cycles of 218 supercell thunderstorm… Show more

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Cited by 13 publications
(6 citation statements)
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“…The AOD is a major optical parameter for aerosol particles and a key factor affecting global climate (Holben et al, 1991(Holben et al, , 2001Smith et al, 2014;Srivastava and Bhardwaj, 2014). For most of the snow samples collected in the afternoon at the Aqua-MODIS (13:30 LT) overpass time, the averaged spatial AOD distribution was derived from the Aqua-MODIS satellite "Aerosol" product during the sampling period across northern 15…”
Section: The Spatial Distribution Of Aod 10mentioning
confidence: 99%
“…The AOD is a major optical parameter for aerosol particles and a key factor affecting global climate (Holben et al, 1991(Holben et al, , 2001Smith et al, 2014;Srivastava and Bhardwaj, 2014). For most of the snow samples collected in the afternoon at the Aqua-MODIS (13:30 LT) overpass time, the averaged spatial AOD distribution was derived from the Aqua-MODIS satellite "Aerosol" product during the sampling period across northern 15…”
Section: The Spatial Distribution Of Aod 10mentioning
confidence: 99%
“…Considering the lower computational cost of a single deterministic run, cloud‐resolving horizontal grid spacing (1–1.5 km) was chosen for the deterministic system. The 3DVAR analysis system has been tested during the HWT Experimental Warning Program (EWP) from 2011 to 2013, and evaluations demonstrated an overall improved skill in analyzing storm‐scale structures along with the timing and location of the most intense storm‐scale objects in the forecast domain (Gao et al ., 2013; Calhoun et al ., 2014; Smith et al ., 2014). These developments and associated improvements, however, were mainly achieved by the systematic assimilation of radar radial velocity and reflectivity data.…”
Section: Introductionmentioning
confidence: 99%
“…To assess the potential value of the weather-adaptive, real-time analysis system to warning operations, it was formally tested and evaluated by forecasters who participated in the NOAA Hazardous Weather Testbed (HWT) spring experiments from 2011 to 2013. During this period, many severe weather events were successfully detected and analyzed automatically by this 3DVAR system (Gao et al 2013;Smith et al 2014;Calhoun et al 2014). The analyzed storm structures not only matched quite well with synthesized reflectivity fields from multiple radars, but the most intense storms corresponded with the location and time of the National Weather Service (NWS) local storm reports.…”
Section: Introductionmentioning
confidence: 78%
“…Forecast evaluation is conducted with quantitative metrics and subjective evaluation. The quantitative metrics include the neighborhood equitable threat score (nETS; Gilbert 1884; Clark et al 2010) and frequency bias for the composite reflectivity that is verified against observations obtained from NSSL Multi-Radar Multi-Sensor System (MRMS; Smith et al 2016). The subjective comparisons are performed with the NWS local storm reports for the tracks of the updraft helicity (UH) between 2 and 5 km above ground level (Kain et al 2008(Kain et al , 2010 and the MRMS observations for reflectivity, respectively.…”
Section: Introductionmentioning
confidence: 99%