Magnetic Observatory Viby
Viby (Sollentuna), Sweden · geographic coordinates: 59°27' N
17°54 E · geomagnetic coordinates (2017): 57.69°N, 106.22°E
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Online determination of auroral substorms
The primary mission of this magnetometer is to issue
timely alerts at times of likely occurrence
of visible or photographic aurora borealis at the location of the magnetometer - Stockholm, Sweden. Of course,
the magnetometer data also can be helpful for forecasting opportunities to observe aurora borealis elsewhere.
A primary determinator of magnetic disturbance usually is the magnitude of
change of the horizontal magnetic components. Besides that, for the Magnetometer Viby we implemented an online
determination of auroral substorms based on the speed of magnetic field
changes.
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A transparent way of displaying this activity analysis, based on flux change speed is given
by the plots: They analyze the size and speed of disturbances of the horizontal components.
In the upper plots, the evolution of the horizontal magnetic field components is plotted for the
last four hours, with rise and fall timescales of the disturbances color-encoded.
Rise/fall
times in excess of 40 nT/10 min are considered significant. Rise/fall times in excess of 80 nT/10 min
are considered to be caused by magnetic field disturbances connected to a possible occurrence of
aurora borealis.
Blue colors represent a fast rise of magnetic flux, red colors a fast drop of magnetic flux.
In the lower plots, the absolute magnitude of the disturbance speed is given in units of
nT per 10 minutes.
The Finnish Metereological Institute
employs a similar estimator for assessing the probability of visible auroras.
Disturbed geomagnetic conditions are assumed for changes larger than 0.3 nT s-1
at the station in Nurmijärvi (57.72N GCM). This corresponds to 180 nT/10 min in
our notation.
The corresponding threshold for the Sodankylä station (64.01N)
is 0.5 nT s-1.
Their bar plots
show the hourly maximal changes in the horizontal magnetic field
components.
Currently, for SAM Viby we use 180 nT/10 min and for SAM Haimhausen (43.51N GCM),
90 nT/10 min to characterize conditions as disturbed, however these thresholds are preliminary and subject to change.
Peak analysis
x_min at 13:23, -72 nT above last minimum
x_max at 13:44, 108 nT above last minimum
x_min at 14:19,-112 nT above last minimum
x_max at 14:39, 94 nT above last minimum
x_min at 14:54, -51 nT above last minimum
x_max at 15:25, 121 nT above last minimum
x_min at 16:27, -84 nT above last minimum
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Alerts based on the evolution of the horizontal magnetic field components
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For concurrent forecasts, the evolution of the horizontal magnetic field components is analyzed. Depending on the activity within the last hour, green/yellow/red alerts are displayed in plot.
Activity alert criteria assess the last 60 minutes: |
Quiet geomagnetic conditions |
Disturbed geomagnetic conditions |
Considerable geomagnetic activity |
Within the last hour, less than ΔB<80 nT, corresponding to <K3 |
Within the last hour, less than ΔB<140 nT, corresponding to K4 |
Within the last hour, ΔB>140 nT, corresponding to K5 |
The derivative of the magnetic field evolution, dB/dt characterizes the speed
of the magnetic flux change. Peaks hint at fast change, which is a
neccessary condition for the occurrence of aurora.
Depending on the activity within the last four hours, green/yellow/red alerts are displayed in plot.
Flux change speed alert criteria assess the last four hours: |
Quiet geomagnetic conditions |
Disturbed geomagnetic conditionsons |
Considerable geomagnetic activity |
Outburst less steep than ΔB<40 nT/10min |
Outburst less steep than ΔB<80 nT/10 min |
Outburst less steep than ΔB<180 nT/10 min |
Outburst steeper than ΔB>180 nT/10 min |
In the plot, also high values of the second derivative, d2B/dt2 are marked (by arrows).
These characterize high curvatures of the flux curves and thus a fast change from rising to falling wings,
prevalent in magnetic substorms, and may allow to identify a substorm earlier than just the first derivates.
The analysis of these features is still experimental and is not being used to issue aurora activity alerts.
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Current trend data for transfer to the SAM magnetometer network
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From about the year 2002 on, a pan-European magnetometer network emerged, based
on the SAM magnetometer design. To identify magnetic storm episodes,
a common analysis and alarm feature was implemented.
By a common analysis false alarms of individual stations
can be effectively avoided.
These data resemble dB/dt data with a step width of Δt=5 min.
The data format follows the format put forward by the German magnetometer
network at polarlichtinfo.de. This
webpage provides a central data analysis mainly for German SAM stations.
These data resemble ΔB/Δt data with a step width of Δt=5 min, which can be useful
for aurora borealis prediction as put
forward in a blog by Steve Marple
of Aurorawatch UK.
To facilitate an online analysis for central/northern Europe, recent magnetometer data is provided here.
These data describe te evolution of the horizontal components of the local magnetic field within the last
hour.
Haegersten FLC Magnetometer
59.28N 17.96E
se.gner.cc/sam/
09.08.25
K: 4 4 4 4 5 5 - -
14:49 - 15:49 UT
Min. X Y Z Trend
now +60 -46 +51 o
- 5 +62 -46 +47 o
-10 +73 -37 +29 o
-15 +75 -38 +12 o
-20 +73 -45 +0 o
-25 +71 -42 -12 o
-30 +62 -29 -13 o
-35 +27 -26 -14 +
-40 +12 -22 -9 +
-45 -19 -16 -2 +
-50 -40 -14 -2 ++
-55 -49 -17 -4 ++
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This document was produced:
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