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These correspond to the “click” and “tweek” sounds in the audio sample. A zoom-in a radio atmospheric is shown in the bottom left panel. There are also a set of short horizontal lines between 10 and 15 kHz. These are the `Alpha’ navigation beacons. The solid horizontal lines between 18 and 30 kHz are VLF transmitter signals, although they are too high in frequency to hear in the audio. These transmitter signals are nominally used for communications. The top right panel shows a zoom-in of a transmitter called NWC, in Australia, which is clearly detected at Stanford, and the communication signal can be seen as up and down modulation of the frequency. However, these transmitter signals act as a diagnostic of the lower ionosphere, since their propagation to long distances is dependent on ionospheric reflection. The bottom right panels shows an example of two of these VLF transmitters tracked at Stanford for a 3-day period. Both the amplitude (top) and phase (bot) of the signal show a clear daily variation, reflecting the drastic changes to the lower ionosphere from daytime to nightime. This is an example of ionospheric remote sensing using VLF transmitter signals. Where Do You Collect ELF/VLF Data? We have receivers all over the world, on all seven continents, for a wide variety of experiments. 1 milyon lira kefaletle tahliye edildi (1) Orhan Üngan ismi son olarak suç çetesinin başı Sedat Peker'in ortaya attığı Burhan Kuzu ile alakalı iddialarda slots yer aldı.