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| Introduction |
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StormLab 4.0 represents
a revolutionary upgrade to our flagship Doppler radar software,
continuing our goal to provide affordable, state-of-the-art
weather software for your PC. StormLab turns any Internet connection
into an automated and full customizable display system for National
Weather Service Doppler weather radar. You will
have real-time access to reflectivity, velocity, storm
relative velocity, VAD Wind Profiles, precipitation estimates, storm
cell data, and MUCH more, including new high resolution Level 2
data. StormLab's full-featured interface includes looping, panning,
zooming, and overlays of geographic and weather data! StormLab
is also fully GIS compatible, allowing users to display radar
data right down to street level. Complete GPS integration allows
mobile storm spotters or those on everyday travel to see their
current position plotted right on the radar scope. Whether it's the
color of the radar data or the size of cities, everything is
customizable using an intuitive and easy-to-use graphical interface.
StormLab 4.0 is perfect for on-air presentation, but at a fraction
of the cost of typical TV radar display software. Why settle for
anything less than software written by meteorologists. |
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| StormLab
Control Panel |
When you
first start StormLab from the desktop icon, you will see
the main StormLab control panel. This window serves as the
main interface from which you can load real-time or archived
<LINK HERE> radar data already stored on your PC. Once
radar data has been loaded, this control panel can be
minimized.
On many of the StormLab windows, you will
note this icon . Clicking it will bring you to a designated
help page just like this one! Also, many features in the
software are exclusive to the Supercharged version. The help
documents will denote such features with this icon.
You can load radar data
with StormLab right out-of-the-box, but remember that StormLab
is highly customizable to your liking. We'll discuss enhancing StormLab a
bit further down, but do note the Setup <LINK HERE> menu option
at the top of the control panel which will be used
for this purpose. Another new featuretoV4.0istheabilitytobookmark<LINKHERE> radar data that you
view most often. These can even be automatically launched at
startup, making StormLab a completely hands-off solution for
those users in using the software as a weather/security
monitoring tool. More on this later. Let's first take a look
at the control panel and see how easy it is to view National
Weather Service Doppler radar data. |
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| Viewing Live Radar Data |
On the left
hand side of the control panel is a tree containing every
Doppler radar site, organized by state. To find the site closest to you, a map is available by
clicking the "Find Nearest Radar" option under the Help menu.
Selecting a radar site will place a checkmark along side it
while turning the text bold so that you know it is active
(see pictured example). In addition to individual Doppler
Radar data, StormLab also provides access to a national and
regional overviews (courtesy of WeatherUnderground) as well as
Canadian radar imagery. Both of these data sets will load
simply by clicking the appropriate link from the left hand
listing.
Step 1.) Left click
and highlight a radar site
Once you select a
radar site, next select how many images you would like in your
loop. The time span of this loop depends on the mode the radar is
operating in (4 to 10 minutes between each scan), with the
default value (12 frames) covering an average of an hour's
worth of radar data.
Step 2.) Select the number of
images you would like in your loop (or check the Single Frame
box).
Next, you will need to select a radar
product. StormLab provides the full suite of radar products
generated by each Doppler radar site. You will note there
are many many more products than you're used to seeing on TV or the
Internet, so we'll describe each one briefly below. This data
is free to you and there is no charge to access it through StormLab.
You will also notice a second radio button labeled "Level 2 (Hi-Res)
data". For those of you who have upgraded to StormLab
Supercharged, you will also have optional access to hi
resolution Level 2 radar data, which provides users
with better spatial, vertical and data resolution. Subscription
or other service based feeds are required to access Level 2 data,
with StormLab fully able to integrate and display these
data.
Step
3.) Left mouse click the radar product you wish to display.
Radar Product
Choices:
Reflectivity - This is the product
that is most commonly displayed on TV or the Internet, usually at
the base, or 0.5 degrees tilt. As the radar spins around, it sends
out thousands of energy pulses. Reflecitivty is simply the amount
of energy returned back to the radar from whatever it hits in
the air -- rain, hail, snow, dust, and even insects. The higher the
water/ice content in the object, the more power that gets returned
to the radar. Units are logarithmic (dBZ) and various scales may be
used to display these values depending on whether the radar is in
clear air or precipitation/storm mode. Reflecitivty imagery is
usually color coded so that cool colors refer to light
precipitation, and hot colors (reds, purples) infer very heavy
rainfall or hail. Please note that the radar has no ability to
determine between rain or snow. Radar imagery color coded by
precipitation type is often wrong, and estimated based on surface
weather reports and current air temperatures. You'll note that
StormLab provided several vertical tilts for reflectivity data since
the radar also scans the sky vertically to give meteorologists a
3-dimensional view of storms. The lowest tilt (0.5 degrees) is what
is most commonly displayed, although higher tilts are used by
National Weather Service meteorologists to look for things like
developing hail or downbursts.
Composite
(Reflectivity) - Same as above, except instead
of viewing the reflectivity at one vertical elevation, this
image displays the MAXIMUM reflectivity value detected by the
radar for a given location (regardless of the elevation). Basically,
if you were standing 30 miles east of the radar, and above you, the
radar sampled dBZ values of 5, 25, 30, 34, 52, 40, 37, and 22 at
different heights...the image would display 52 dBZ for the composite
reflectivity at your location. Used to show the most intense storms
and hail cores aloft. Used by radar operators as more of a "catch
all" as it is the last product received per volume scan (one
complete radar sweep of the atmosphere). This image is also
accompanied for the Storm Cell Attributes Table. Click here for more
info.
Velocity - The most
important feature of Doppler radar is the 'Doppler', or its ability
to detect the air motion in areas of precipitation. Doppler
radar can detect winds blowing toward or away from the radar, called
Radial Velocity. like reflectivity, this product is available at
several elevation slices. NOTE: The radar can again only detect that
portion of the wind which is blowing along the radar beam. For
example, if you are looking due south from the radar, and the wind
was blowing from the west or east at even 80 mph, the radar would
see 0 knots because the wind is blowing perpendicular to the beam.
Also note that the radar beam extends higher and higher the farther
you go from the radar. Novice users often mistake high winds aloft
(fairly common) for strong winds at the surface. Velocity imagery
can take years of experience to master and can fool even the most
experienced.
SRM
- Stands for "Storm Relative Motion". Same as above except
the average movement of the storms (or a value entered by the
National Weather Service radar operator) is subtracted out. By
subtracted out the forward storm motion, the wind field relative to
a storm of interest can be observed. This is used to detect storm
scale rotation or other features which could signify the onset of
very large hail, a downburst, or possibly a
tornado.
Precipitation - A great benefit of
Doppler radar is its ability to estimate fallen precipitation, in
order to fill in the holes left by observation networks, automated
rain gages, and other sources of data. Measured in inches, Doppler
Radar can estimate precipitation that has fallen over the past hour,
three hours, and storm total. Note the beginning and ending times on
the storm total imagery. The radar requires several hours of no
precipitation before resetting, and areas that receive a lot of
rainfall can have this image piling up for days if not weeks! Also
note that precipitation can be severely overestimated due to storms
which contain hail and the freezing level, as partially melted ice
returns an extremely high reflectivity.
Layer Reflectivity
Maximum - More of a use for pilots, this product
is a coarse resolution image (4km grid) which provide the maximum
reflectivity at different layers in the atmosphere: lower, middle
and upper. Similar to the composite reflectivity, but broken
down into 3 layers and of a poorer resolution.
VIL
- Vertically Integrated Liquid. A coarse resolution image
that is basically a measure of the total estimated liquid in a
vertical sense, in units kilograms per square meter. Most used to
identify storms with heavy rainfall or the possibility large
hail. Can also be used in combination with other products to predict
the onset of downbursts.
Echo Tops
- Simply an image depicting the estimate of storm
cloud tops. Note that depending on the tilt of the radar beam and
distance from the radar, these can be over or under-estimated
on the order of 5-10,000 feet or more. Very useful in detecting
severe storms that amass to great heights.
88D Text
Message - In the event of a radar outage,
software upgrade, or other significant mode change, the NWS in
charge of that radar will send out a message explaining the problem
or change. |
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Viewing
Level 2 Radar
Data |
New to StormLab 4.0, and
an exclusive feature to the Supercharged version, is real-time
access to hi-resolution Level 2 radar data. In addition to the
stanard resolution products provided at no charge to StormLab
users, we are now offering display capabilities for higher
resolution data available through subscription or university
data services (e.g. http://www.allisonhouse.com)
Level 2
data is essentially the raw data from the National Weather
Service Doppler radars, providing you will a full suite of
elevation tilts as well as improved data resolution. For
example, Level 2 reflectivity data will be displayed at 0.5
dBZ intervals and Level 2 velocity data will be displayed at 1
knot intervals with a 0.25km spatial resolution (as opposed to
1km in the standard velocity products). You will also notice
the slider bar in the example to the right for storm motion
and speed. StormLab 4.0 provides a unique capability where the
user can generate storm relative velocity imagery and change
the storm motion on-the-fly!
One data is displayed you
will have full access to switch among the available elevation
tilts and all four data types (reflectivity, velocity, storm
relative velocity and spectrum width) |
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| Bookmarks |
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New to
StormLab 4.0 is the ability to bookmark your most often loaded
radar sites. The window to the left will appear by clicking
the Modify Bookmarks option from the "Bookmark" menu on the StormLab Control
Panel.
Using the pull-down menus at the button, select
the radar site, product and loop size you wish to bookmark. If
you'd like this product to automatically load when you start
StormLab, check the Auto-Load on Startup box. When you're all
set, click the Add button.
Double click a row in the
grid at the top to make edits or delete an entry. You can also
use the arrow buttons to re-order your bookmarks.
Click the "X" in the top right to exit the editor. | |
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| Viewing Archived Data |
The data you
view in StormLab is saved to your hard drive (and can be
purged through the Program Settings section of the Setup
window).
In addition, radar data can be downloaded from
the National Climatic Data Center website and converted to
StormLab using a conversion utility available for purchase.
StormLab has a unique ability to view stored data as
well as current data, making it a great tool for those doing
research, analysis, or even putting together a movie or
montage to go with your storm chase video!
To view or
download archived data, simply click the Archive Viewer tab on the StormLab
control panel. Data are organized in folders by the 4-letter
radar site identifier and the product type. Files are then
stored with a date/time stamp in Greenwich Mean Time. For
example, the first highlighted file to the right
200705282348.keax in the keax Reflecitivty1 folder is the 0.5
degree reflecitivty product for keax (Kansas City, MO), stored
at 2348 GMT (648PM CDT) on May 28th, 2007.
To view
archived data, simply select the files you wish to view and click "Load" |
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