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An evaluation of the Worldwide Lightning Location Network (WWLLN) using the National Lightning Detection Network (NLDN) as ground truth
[1] A performance assessment of the Worldwide Lightning Location Network (WWLLN) is presented using the National Lightning Detection Network (NLDN) as ground truth, over unprecedented time andExpand
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Predecessor Rain Events ahead of Tropical Cyclones
Abstract Twenty-eight predecessor rain events (PREs) that occurred over the United States east of the Rockies during 1995–2008 are examined from a synoptic climatology and case study perspective.Expand
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NOAA's Second-Generation Global Medium-Range Ensemble Reforecast Dataset
A multidecadal ensemble reforecast database is now available that is approximately consistent with the operational 0000 UTC cycle of the 2012 NOAA Global Ensemble Forecast System (GEFS). TheExpand
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Distant Effects of a Recurving Tropical Cyclone on Rainfall in a Midlatitude Convective System: A High-Impact Predecessor Rain Event*
Abstract Recent research has identified predecessor rain events (PREs), which are mesoscale regions of heavy rainfall that occur ∼1000 km poleward and downshear of recurving tropical cyclones (TCs).Expand
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An Analysis of Multiple Predecessor Rain Events ahead of Tropical Cyclones Ike and Lowell: 10-15 September 2008
AbstractAn analysis of three predecessor rain events (PREs) that occurred ahead of North Atlantic tropical cyclone (TC) Ike and east Pacific TC Lowell during 10–15 September 2008 is presented. TheExpand
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The Vertical Structure of Mesoscale Convective Vortices
Abstract Simulations of two cases of developing mesoscale convective vortices (MCVs) are examined to determine the dynamics governing the origin and vertical structure of these features. Although oneExpand
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Revisiting the 26.5°C Sea Surface Temperature Threshold for Tropical Cyclone Development
AbstractA high sea surface temperature is generally accepted to be one of the necessary ingredients for tropical cyclone development, indicative of the potential for surface heat and moisture fluxesExpand
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A Global Climatology of Baroclinically Influenced Tropical Cyclogenesis
AbstractTropical cyclogenesis is generally considered to occur in regions devoid of baroclinic structures; however, an appreciable number of tropical cyclones (TCs) form in baroclinic environmentsExpand
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Petascale WRF simulation of hurricane sandy: Deployment of NCSA's cray XE6 blue waters
TLDR
The National Center for Atmospheric Research (NCAR) Weather Research and Forecasting (WRF) model has been employed on the largest yet storm prediction model using real data of over 4 billion points to simulate the landfall of Hurricane Sandy. Expand
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The extratropical transition of tropical cyclones. Part I: Cyclone evolution and direct impacts
AbstractExtratropical transition (ET) is the process by which a tropical cyclone, upon encountering a baroclinic environment and reduced sea surface temperature at higher latitudes, transforms intoExpand
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