Evolution of the Ionospheric Plasma Turbulence over Seismic and Thunderstorm Areas

S cientific linked the health of indi- studies which viduals with their soci al relationships have shown that active social s upport can at least in part explain

ISPED-Bordeaux School of Public Health, Bordeaux, France (CD); Bordeaux University Hospital, Public Health Department, Medical Information Service, Bordeaux, France (CD); Dalla

(i) Because most of the transient volcano-electro- magnetic signals on land are observed during the two months preceding an eruption (i.e. [ 48 , 49 ]), the time window on

Section 2 briefly describes the wave experiment which is a part of the scientific payload of DEMETER, the optical ex- periment in ´Snie˙zka observatory, and the lightning networks

In this paper we have presented the observation of U-shaped spectrum registered by the DEMETER satellite in the equatorial region of the upper ionosphere during nighttime, which

It is shown that the chorus elements with frequencies up to 2 kHz are emerging from a hiss band with an upper limit of 930 Hz and a lower limit close to the proton gyrofrequency

It is known that the number of earthquakes decreases when their magnitudes increase, and the choice of a low bound of 4.8 for the magnitude of earthquakes is the result of a

Extremely low frequency plasma turbulence recorded by the DEMETER satellite in the ionosphere over the Abruzzi region prior to the April 6, 2009, L’Aquila earthquake... Extremely