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Geomagnetic Field “Real Time” Monitoring

In the picture above an example of a geomagnetic storm detection.

With the equipment described in the posts : Fluxgate Magnetometer, Geomagnetic Field we have created a small geomagnetic observatory and in this page we insert the real-time data read by the system and some analysis examples.
The sensor has been positioned, parallel to the East-West direction, inside a cellar, away from anthropic disturbances, such as moving cars. The data is collected by a Datalogger consisting of a Raspberry PI system. The python application that reads the data, also performs a first processing of the same and produces the graphs showing the trend of the magnetic field intensity.

Original Signal

The following graph shows the trend of the signal measured directly by the sensor with a rate of one measurement per second. No processing or filter was applied to the signal.
Generally there is a certain “noise” in the order of about 10 nT due to both the characteristics of the sensor and the residual anthropic disturbances.

Daily Trend

Signal Filtered Low Pass Cutoff 0.01 Hz

The graph below shows the signal after it has been filtered with a low-pass butterworth filter with a cutoff frequency of 0.01 Hz which corresponds to a period of 100 s. In this way we clean the signal from high frequency statistical variations.
The filtering was carried out thanks to the features present in the python scipy library, as shown in the following python code extract.

#---------------------------ooo0ooo---------------------------
# Function butter_lowpass
#-------------------------------------------------------------
# Utility statistica filtro passa-basso
#---------------------------ooo0ooo---------------------------
def butter_lowpass(cutoff, fs, order=5):
nyq = 0.5 * fs
normal_cutoff = cutoff / nyq
b, a = butter(order, normal_cutoff, btype='low', analog=False)
return b, a

#---------------------------ooo0ooo---------------------------
# Function butter_lowpass_filter
#-------------------------------------------------------------
# Utility statistica filtro passa-basso
#---------------------------ooo0ooo---------------------------
def butter_lowpass_filter(data, cutoff, fs, order=5):
b, a = butter_lowpass(cutoff, fs, order=order)
y = lfilter(b, a, data)
return y

#-------------------------------------------------------------------
# Data could be filtered in order to eliminate high freq noise
# Filter requirements.
order = 6
fs = 1.0       # sample rate, Hz
cutoff = 0.01  # desired cutoff frequency of the filter, Hz
    
# Get the filter coefficients so we can check its frequency response
#b, a = butter_lowpass(cutoff, fs, order)
    
# Filter the data
filtData = butter_lowpass_filter(data, cutoff, fs, order)
#--------------------------------------------------------------------

Daily Trend

Temperature of the FGM Sensor

The response of the FGM sensor is dependent, to a greater or lesser extent depending on the model, by temperature variations. For this reason, the temperature of the sensor is also measured and acquired, so as to ensure that it remains constant throughout the measurement period.

Daily Trend

Influence of Solar Activity on Geomagnetism

The geomagnetic field is not constant but is subject to numerous variations both periodic and non-periodic.
The long-term variations, which occur on a time scale greater than 5 years (secular variations), are caused by the dynamics inside the Earth, while the short-term variations, much more intense, have an external origin and manifest themselves on a scale time of seconds, minutes or days.
The latter are mainly produced by electric currents due to charged particles moving in the magnetosphere and in the ionosphere.
These variations include periodic ones (called regular variations) due to the rotation and orbital movements of the Earth, the Moon and the Sun
and those transients caused by the interaction of the solar wind with the magnetosphere.

Quiet Sun

In the event that there are no phenomena due to intense solar activity, the trend of the geomagnetic field follows a trend with characteristic daily variations with a periodicity of 24 hours.
The phenomenon begins with the electromagnetic radiation emitted by the Sun. In addition to illuminating and heating one side of the earth, this radiation also heats the ionosphere causing convection. The convection moves the charged particles through the earth’s magnetic field creating a dynamo action that guides the ionospheric electric currents above the equator and up to medium latitudes. These currents produce a magnetic field which, seen from space, appears fixed on the side of the earth’s day. The rotation of the earth brings a site on the surface inside and outside of this magnetic field creating a 12-hour variation and then a 24-hour cycle.

The graph shown below faithfully reproduces this cyclical trend.

Geomagnetic Storms

The “real-time monitoring” of the geomagnetic field also aims to identify the so-called Geomagnetic Storms.
These are irregular and sudden variations in the intensity and direction of the earth’s magnetic field, usually accompanied by other geophysical phenomena (eg the polar auroras). The intensity and direction of the field, while fluctuating in an apparently disordered manner, vary, during a storm, according to well-defined temporal trends.
Two phases are distinguished: the initial phase, with a duration of 1 to 10 hours, in which the horizontal component (H) of the magnetic induction undergoes an increase of 10 ÷ 50 nT, and the main phase, of the duration of one or more days, when H first decreases, reaching a minimum (generally, of 100 ÷ 200 nT below the normal level), and then slowly recovers, returning to the original values.
Magnetic storms are produced by clouds of plasma expelled by the Sun; explosive phenomena, such as solar flares, produce an abrupt start to the storm. Due to the impact of the fast plasma cloud, the magnetosphere is abruptly compressed, so that the magnetic field on the earth’s surface increases (initial storm phase).
In the bands of radiation that surround our planet, charged particles are subsequently injected; this has the effect of intensifying the so-called ring current, produced by the longitudinal motion of the trapped particles. Since this current circulates, in the equatorial plane, in the sense that it goes from east to west, the magnetic field that it produces inside is opposite to the geomagnetic one: hence the decrease of H observed in the main phase of the storm. The particles injected into the radiation bands are then gradually dispersed, so that the intensity of the ring current returns to ordinary values ​​and the storm ends.

Magnetic storms have significant effects on the terrestrial environment, in particular disturbing effects for radio communications, especially in the high-frequency band.

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