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Page updated October 28, 2007
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How to use the Waterfall Chart
The Spectrum Monitor Waterfall Charts provide a visual assessment of propagation
conditions in the HF band as observed in Alaska at the HAARP site.
Measurements are made throughout the day using a spectrum analyzer and the
strength of received signals is plotted as progressively brighter colors on a chart
where frequency is along the "y" axis and time of day is along the "x" axis.
The chart normally shows several bands of bright colors corresponding to strong
international broadcast stations operating in various frequency ranges, such as
the 41 meter or the 25 meter band. On days when these bands are missing or when
the bands contain "cooler colors" ionospheric propagation conditions are poor,
possibly due to a geomagnetic storm. The onset of such a storm can often be seen
in the chart as the abrupt termination of a color band into the blue background.
An example of a minor absorption event (or fade-out) is seen in the chart at
approximately 1100 UTC. The fade-out lasts only for a short time and propagation
returns to normal after about 1130 UTC. On such occasions, it is interesting to
compare the HF waterfall chart with other data such as the HAARP Riometer and
Magnetometer charts.
The higher frequencies (in the upper part of the chart) are usually devoid
of signals during the low part of the sunspot cycle since higher frequencies need
a higher degree of ionization to propagate. When frequencies above 20 Mhz are
present in the chart, it is indicative of increased solar activity.
Other interesting aspects of the chart are explained in the following notes from
the chart above:
- Higher frequencies require greater ionization. As solar activity increases,
additional signal should appear in this region.
- There are superfluous, constant signals present in the data. They are due to
local sources at or near the HAARP site, such as computer clock oscillators.
- Vertical white space results from gaps in the data, usually caused by
power failures.
- The white line drawn on the chart shows the trend for strong signals to
move toward shorter time intervals as the frequency decreases. This is a
consequence of the effect of the "D" layer which absorbs or attenuates lower
frequencies. The "D" layer disappears during the evening hours and, in the chart
above (for May 29, 1997), the sun is below the horizon for only a brief period of time.
- Strong signals are observed in the upper part of the standard AM broadcast
band (up to 1600 kHz). These signals originate, for the most part, in the
northwestern US and reach the HAARP site through multiple sky wave reflections. The
effect of the "D" layer on these signals is quite pronounced.
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