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The diagnostic analysis combines WSR-88D national radar and echo top mosaics
(provided by NOAA with mosaics created and distributed by UNISYS) and
cloud-to-ground lightning (provided by Global Atmospherics Inc). The Convective
Hazard Detection field is depicted based on a 6 level intensity scale. The
6 levels fundamentally correspond to VIP level (see images above and to the right).
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Forecasts are
determined by applying a stratiform-convective partitioner (Steiner et.al. 1985) and
an elliptical filter (Wolfson et al. 1998) to the hazard detection field. These
filters eliminate stratiform return and small-scale perishable features that are not
a hazard to aviation or are not likely to persist for 1 hour, respectively.
Extrapolations are performed based on the Thunderstorm Identification Tracking and
Nowcasting (TITAN, Dixon and Wiener 1993) algorithm.
Click on the above image to plot forecast polygons (blue shapes).
The NCWF forecast product does well with long lived
mature systems. However, the initiation, growth, and dissipation of these systems, as well as
shorter lived isolated storms, are not well forecast. Work on automated methods
to forecast the growth and dissipation of storms is on going.
This
training module is broken into 7 categories. For information on:
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setting
up your browser - click on "Setup".
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how
to use the web page - click on "Navigation".
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steps
taken to create hazard field - click on "Hazard field".
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how
forecasts are produced - click on "Forecast".
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how
to interpret performance image - click on "Performance".
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what
to do when things don't work - click on "Help".
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frequently asked questions - click on "FAQ".
Also, a quick reference to the product can be viewed by clicking on "Reference".
To view the "Aeronautical Information Manual" click
on "AIM".
Click
on the "Intro" link (left menu) to return to this introduction page.
Click
on the "NCWF" logo (top left) to return to NCWF Javascript page.
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