Abstract
Ground-based very low frequency (VLF) transmitter waves (3 - 30 kHz) can cause the precipitation loss of high-energy electrons in Earth's radiation belts. Although the propagation and attenuation of aabrtificial VLF waves have been studied for more than half a century, it is not clear whether solar extreme ultraviolet (EUV) radiations can modify the VLF wave intensity in inner radiation belt and slot region (L ~ 1.1 - 3R(E)). Here, by analyzing satellite observations and quantitative calculations, we find that the enhanced solar EUV radiations cause global attenuation of the artificial VLF waves radiated from low-latitude transmitters (λ < 44.2° or L < 1.8 R(E)), whereas those waves radiated from middle-latitude transmitters (λ > 44.2° or L > 1.8 R(E)) weaken slightly around noon. Under high solar EUV radiations, the large attenuation of artificial VLF waves in the low L region is due to enhanced collisional damping of ionospheric plasmas at low latitudes.