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<H2 align=3Dcenter>SUPPLEMENTAL INFORMATION...IN GREATER DEPTH</H2>
<H4 align=3Dcenter>To complement the Daily Summary for Thursday, 22 =
October 2009=20
</H4>
<H3 align=3Dcenter>INTERPRETING RADAR SUMMARY CHARTS</H3>
<HR>

<P>In the <I>DataStreme Atmosphere Project</I>, current radar imagery is =

available in several formats so we can better visualize where =
precipitation is=20
falling across the nation. You have become acquainted with one such =
product,=20
which is an overlay of the composite radar summary that is placed over =
the=20
surface analysis that you retrieve from the current "Isobars, Fronts, =
Radar=20
&amp; Data" link on the <I>DataStreme Atmosphere website</I>. This =
feature that=20
includes various color-coded regions on the surface analysis allows us =
to see=20
the precipitation areas and intensity for the entire coterminous U.S. =
Several=20
other charts are available that provide additional detail. A separate =
radar=20
summary chart, with a link identified as "Radar", or a radar summary =
with fronts=20
chart ("Radar &amp; Fronts") can be similarly accessed from the Radar =
portion of=20
the homepage. </P>
<H4>COMPONENTS OF THE RADAR SUMMARY CHART</H4>
<P>These various composite radar summary charts are prepared hourly at =
35=20
minutes past the hour from the data supplied by National Weather Service =
radar=20
reports originating from the national network of primary weather radar =
units.=20
</P>
<P>The intent of the national radar summary chart is to graphically =
depict the=20
large-scale distribution of precipitation. Precipitation intensities are =

indicated on the chart by color codes. Some adjustment of the data may =
be=20
needed, especially if precipitation echoes are reported by more than one =
radar=20
site. When applicable, current severe thunderstorm and tornado watch =
areas=20
("watch boxes") are plotted on the radar summary chart. </P>
<H5>ECHO INTENSITIES</H5>
<P>The reflectivity or intensity of the reflected radar signal depends =
upon=20
several factors to include the size, shape, density (the number of =
targets per=20
unit volume), and state (rain, snow or mixture) of the hydrometeor =
target.=20
Usually, the intensity of the reflected echo is assumed proportional to =
the rain=20
drop density, thus indicating the precipitation rate or intensity. </P>
<P>Contours of echo reflectivity, also known as "VIP levels" (for=20
<B><I>V</I></B>ideo <B><I>I</I></B>ntegrator and =
<B><I>P</I></B>rocessor), are=20
plotted on the radar charts as a color-coded display. The colors within =
these=20
contours provide an indication of the precipitation intensity and the =
size=20
depicts the areal extent of the detected precipitation. Based on =
empirical=20
studies, six standard VIP levels are related to the rainfall rate for =
the steady=20
"stratiform" precipitation typical of wintertime storms or warm frontal =
systems=20
and for showery "convective" precipitation of representative summertime =
storms=20
or cold front systems. </P>
<H5>RADAR INTENSITY LEVELS</H5>
<HR>
<PRE>        <B>COLOR     VIP       RAINFALL RATE       PRECIPITATION    =
INTENSITY  =20
                 LEVEL    [inches per hour]</B></PRE>
<HR>
<PRE>                       <B>STRATIFORM    CONVECTIVE</B>
        Blue       1     &lt; 0.1         &lt; 0.2      Light            =
-
        Cyan       2   0.1 to 0.5    0.2 to 1.1   Moderate
        Green      3   0.5 to 1.0    1.1 to 2.2   Strong           +
        Yellow     4   1.0 to 2.0    2.2 to 4.5   Very Strong     ++
        Magenta    5   2.0 to 5.0    4.5 to 7.1   Intense          X
        Red        6     &gt; 5.0         &gt; 7.1      Extreme         =
XX
        White                                     Unknown</PRE>
<HR>

<P>Typically, the blue colors indicate light rain or snow; the green =
colors=20
identify light thunderstorms/moderate rain showers; yellows identify =
moderate=20
thunderstorms, while the colors of magenta grading to red are reserved =
for the=20
severe thunderstorms that can cause flooding rains. On a local scale =
(not=20
possible on the national summary), an echo with red can also indicate =
highly=20
reflective water-coated hail. </P>
<HR>

<H5>SEVERE WEATHER WATCH AREAS</H5>
<P>The areas encompassed by an official severe weather watch issued by =
the Storm=20
Prediction Center are plotted on the radar summary chart. These areas =
appear=20
outlined by a rectangular "box", conforming to the map coordinates of =
the=20
affected area. Weather watch numbers associated with each box are placed =
in the=20
box. </P>
<P>The weather watch numbers are sequentially numbered throughout the =
year and=20
have a letter prefix to identify the type of watch: a letter "S" =
indicates=20
severe thunderstorm watch, while a "T" indicates tornado watch. As an =
example:=20
</P><PRE>    T335   A tornado watch, #335.     S336   A severe =
thunderstorm watch, #336.</PRE>
<H4>MAP INTERPRETATION</H4>
<P>The radar summary chart helps fill in the precipitation regions =
between=20
surface observation stations. Hence, the meteorologist can obtain an =
additional=20
perspective of precipitation types, intensities and movements that are =
not=20
provided by the conventional surface analysis. However, care must be =
exercised=20
and surface observations should be inspected, because radar summaries =
may=20
contain echoes of precipitation that does not reach the ground. This =
condition,=20
called "virga", may exist because the air would be too dry and =
evaporation of=20
the rain droplets has taken place. The inclusion of current severe =
weather watch=20
boxes on the chart helps identify regions having weather conditions that =
are=20
potentially conducive for severe weather. </P>
<HR>

<ADDRESS>Return to the <A=20
href=3D"http://www.ametsoc.org/amsedu/dstreme/learn/r_sum.html">Thursday =
Daily=20
Summary </A><BR><BR>Return to <A=20
href=3D"http://www.ametsoc.org/amsedu/dstreme/index.%20html">DataStreme =
Atmosphere=20
website </A></ADDRESS>
<P><I>Prepared by Edward J. Hopkins, Ph.D., email <A=20
href=3D"mailto:hopkins@meteor.wisc.edu">hopkins@meteor.wisc.edu</A> =
<BR>=A9=20
Copyright, 2009, The American Meteorological Society. =
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