Training Guide in Surface Weather Observations - Multiple Choices
Training Guide in Surface Weather Observations - Multiple Choices
Training Guide in Surface Weather Observations - Multiple Choices
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8.2.2.2 24-Hour Precipitation Amount<br />
The 24-hour precipitation amount, 7R24R24R24R 24,<br />
is <strong>in</strong>cluded <strong>in</strong> the 1200 UTC report (or other<br />
designated time) whenever more than a trace of precipitation (water equivalent) has fallen <strong>in</strong> the past 24<br />
hours. The amount of precipitation is coded us<strong>in</strong>g the tens, units, tenths, and hundredths of <strong>in</strong>ches. For<br />
example, 10.45 <strong>in</strong>ches of precipitation (water equivalent) <strong>in</strong> the past 24 hours would be coded 71045;<br />
0.10 <strong>in</strong>ches of precipitation (water equivalent) <strong>in</strong> the past 24 hours would be coded 70010. If more than<br />
a trace (water equivalent) has fallen and the amount cannot be determ<strong>in</strong>ed, the group is coded 7////. If<br />
only a trace or no precipitation occurred <strong>in</strong> the past 24 hours, the group is omitted.<br />
8.2.2.3 Snow Depth on the Ground<br />
The total snow depth on the ground group, 4/sss, is coded <strong>in</strong> the 0000 and 1200 UTC observation<br />
whenever there is more than a trace of snow on the ground. It is also coded <strong>in</strong> the 0600 and 1800 UTC<br />
observations if there is more than a trace of snow on the ground and more than a trace of precipitation<br />
(water equivalent) occurred with<strong>in</strong> the past 6 hours. Report snow depth to the nearest whole <strong>in</strong>ch,<br />
round<strong>in</strong>g up when one-half-<strong>in</strong>ch <strong>in</strong>crements are reached. For example, a snow depth of 0.4 <strong>in</strong>ches would<br />
be considered a trace amount, the group would be omitted; a snow depth of 33.5 <strong>in</strong>ches would be coded<br />
4/034.<br />
Snow depth on the ground is taken by measur<strong>in</strong>g the total depth of snow on exposed ground by means<br />
of a permanently mounted snow stake or by tak<strong>in</strong>g the average of several depth read<strong>in</strong>gs at or near the<br />
normal po<strong>in</strong>t of observation with a measur<strong>in</strong>g stick. When us<strong>in</strong>g a measur<strong>in</strong>g stick, make sure the stick<br />
is pushed vertically <strong>in</strong>to the snow until the bottom rests on the ground. Do not mistake an ice layer or<br />
crusted snow as “ground.” The measurement should reflect the average depth of snow, sleet, and glaze<br />
ice on the ground at your usual measurement site (not disturbed by human activities). Measurements<br />
from rooftops, paved areas, and the like should not be made.<br />
When strong w<strong>in</strong>ds have blown the snow, take several measurements where the snow was least affected<br />
by drift<strong>in</strong>g and average them. If most exposed areas are blown free of snow while others have drifts, try<br />
to comb<strong>in</strong>e visual averag<strong>in</strong>g with measurements to make an estimate.<br />
8.2.2.4 Water Equivalent of Snow on the Ground<br />
The water equivalent of snow on the ground group, 933RRR, is coded each day <strong>in</strong> the 1800 UTC report<br />
if the average snow depth is 2 <strong>in</strong>ches or more. This group is the water equivalent of snow (i.e., snow,<br />
snow pellets, snow gra<strong>in</strong>s, ice pellets, ice crystals, and hail) on the ground. The water equivalent is<br />
coded us<strong>in</strong>g the tens, units, and tenths of <strong>in</strong>ches, us<strong>in</strong>g three digits. If the water equivalent of snow<br />
consists entirely of hail, the group shall not be coded. A water equivalent of 4.7 <strong>in</strong>ches of snow would<br />
be coded 933047; a water equivalent of 17.3 would be coded 933173.<br />
This measurement is made by tak<strong>in</strong>g a “snow core” of the snow on the ground with the use of the<br />
overflow can of your station’s 8-<strong>in</strong>ch non-record<strong>in</strong>g ra<strong>in</strong> gauge. Use the follow<strong>in</strong>g procedure to obta<strong>in</strong><br />
this measurement:<br />
a. F<strong>in</strong>d an area where drift<strong>in</strong>g is m<strong>in</strong>imal. This will usually be a flat area away from obstructions<br />
such as trees and build<strong>in</strong>gs, although obstructions at some distance can help drift<strong>in</strong>g.<br />
8-4