Unique observation of a long-lasting meteor trail of about half an hour duration is described. The trail resulted from a burning meteor from the Leonid storm flux in the middle latitudes over eastern Siberia. We describe three-dimensional morphological characteristics of both the meteor and the long-lasting trail using data from wide-angle CCD cameras. Additionally, we present the meteor and the trail radiolocation characteristics obtained with a meteor radar and ionosonde. The background dynamics of the upper atmosphere at the height where the long-lasting trail developed were observed using data from the meteor radar and Fabry-Perot interferometer. The obtained results allowed the conclusion that the dynamics of a long-lasting trail are c...
Using data from the Sodankylä Geophysical Observatory (67°22′N, 26°38′E, Finland) meteor camera from...
Non-specular, vertically upward transit, fast-moving radar echoes are observed in the summer polar u...
A meteoroid entering the atmosphere produces a transient plasma that due to ambipolar diffusion expa...
A spectacular, well-observed Leonid meteor of visual magnitude -14.3 appeared on 17 November 1998 an...
We analyze the results of a rare long-lived quasisymmetric ellipsoidal-annular meteor trail recorded...
A long‐lived meteor trail has been observed at wavelengths of 572.5 nm, 557.7 nm, 630.0 nm, 865.5 nm...
Despite decades of research, many questions remain about the global flux of meteoroids at Earth, the...
Abstract. We present results of simulated radar observations of meteor trails in an effort to show h...
We discuss using high solar cycle atmospheric conditions as sensors for observing meteors and their ...
Studies of transitionally dense meteor trails using radars which employ specularly reflecting inter...
In November 1998 the earth passed through a maximum in the cometary material responsible for the yea...
An experiment on spatial domain interferometry observations of meteor trail irregularities at a low-...
Meteoroids entering the atmosphere burn up due to friction and form ionized meteor trails at altitud...
From a single image of a persistent trail left by a -1.5 magnitude Leonid meteor on November 17, 199...
The radar detection of meteor trails is discussed with reference to the equipment used, the methods ...
Using data from the Sodankylä Geophysical Observatory (67°22′N, 26°38′E, Finland) meteor camera from...
Non-specular, vertically upward transit, fast-moving radar echoes are observed in the summer polar u...
A meteoroid entering the atmosphere produces a transient plasma that due to ambipolar diffusion expa...
A spectacular, well-observed Leonid meteor of visual magnitude -14.3 appeared on 17 November 1998 an...
We analyze the results of a rare long-lived quasisymmetric ellipsoidal-annular meteor trail recorded...
A long‐lived meteor trail has been observed at wavelengths of 572.5 nm, 557.7 nm, 630.0 nm, 865.5 nm...
Despite decades of research, many questions remain about the global flux of meteoroids at Earth, the...
Abstract. We present results of simulated radar observations of meteor trails in an effort to show h...
We discuss using high solar cycle atmospheric conditions as sensors for observing meteors and their ...
Studies of transitionally dense meteor trails using radars which employ specularly reflecting inter...
In November 1998 the earth passed through a maximum in the cometary material responsible for the yea...
An experiment on spatial domain interferometry observations of meteor trail irregularities at a low-...
Meteoroids entering the atmosphere burn up due to friction and form ionized meteor trails at altitud...
From a single image of a persistent trail left by a -1.5 magnitude Leonid meteor on November 17, 199...
The radar detection of meteor trails is discussed with reference to the equipment used, the methods ...
Using data from the Sodankylä Geophysical Observatory (67°22′N, 26°38′E, Finland) meteor camera from...
Non-specular, vertically upward transit, fast-moving radar echoes are observed in the summer polar u...
A meteoroid entering the atmosphere produces a transient plasma that due to ambipolar diffusion expa...