This means that you can have this right from the get-go in your weapon loadout. Part of the epiphany I had which turned around my Far Cry 2 gaming experience was realizing that the M1903 sniper rifle becomes available in the weapon shop as soon as you finish the training mission. The M1903 sniper rifle as it appears in the armory
It just seemed the 'normal', natural thing to do in a first person shooter. When I first ran through Far Cry 2, I was adamantly clinging to the idea of having an assault rifle (G3-KA4, AK47, whatever.) in my primary weapon slot. If all you carry are close combat anti-personnel weapons, e.g., assault rifles, submachine guns and machine pistols, of course your Far Cry 2 gaming experience is going to narrow right down to one kind of combat which will get very repetitive very quickly. Building a balanced weapon loadout means carrying a variety of weapons that can deal with a variety of situations. And first of all, by weapon loadout, I'm referring to the weapons you are currently carrying. In general, the geophone and magnetometer/infrasound system are useful to record high- and low-frequency seismic waves, respectively.There are over two dozen weapons ultimately available in Far Cry 2 and the assortment is spread out over three weapon groups: Primary, Secondary and Special. This suggests that the mechanisms for detecting seismic waves of the QuakeFinder system and seismometers are different. However, the energy of co-seismic geophone fluctuations (also magnetometer pulsations) yields an exponential decay to the distance of a station to the epicenter, while the energy of the seismic waves is inversely proportional to the square of the distance. The spectrum centering around 2.0 Hz of the co-seismic geophone fluctuations is similar to that of the seismic waves.
The magnetometers register high-frequency pulsations, like seismic waves, and superimpose with low-frequency variations, which could be caused by the magnetometer shaking/tilting and/or the underground water level change, respectively, upon the arrival of seismic waves. There are no obvious charges in the positive/negative ions, the temperature, and the humidity, while the magnetometer, the geophone, and infrasound data detect clear co-seismic signatures, similar to seismic waves recorded by seismometers.
Each QuakeFinder system consists of a 3-axes induction magnetometer, an air conductivity sensor, a geophone, and temperature/relative humidity sensors. This paper utilizes 10 stations of co-located seismometer, QuakeFinder/infrasound to observe co-seismic signatures triggered by the 6 February 2016 M 6.6 Meinong Earthquake.
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