Modeling the meteor head echo using Arecibo radar observations

2008 ◽  
Vol 70 (13) ◽  
pp. 1621-1632 ◽  
Author(s):  
Lars Dyrud ◽  
Diego Janches
Keyword(s):  
2009 ◽  
Vol 27 (5) ◽  
pp. 1961-1967 ◽  
Author(s):  
J. Hinrichs ◽  
L. P. Dyrud ◽  
J. Urbina

Abstract. We present results of simulated radar observations of meteor trails in an effort to show how non-specular meteor trails are expected to vary as a function of a number of key atmospheric, ionospheric and meteoroid parameters. This paper identifies which geophysical sources effect the variability in non-specular trail radar observations, and provides an approach that uses some of these parameter dependencies to determine meteoroid and atmospheric properties based upon the radar meteor observations. The numerical model used follows meteor evolution from ablation and ionization to head echo plasma generation and through formation of field aligned irregularities (FAI). Our main finding is that non-specular meteor trail duration is highly sensitive to the presence of lower thermospheric winds or electric fields and the background ionospheric electron density. In an effort to make key predictions we present the first results of how the same meteoroid is expected to produce dramatically different meteor trails as a function of location and local time. For example, we show that mid-latitude trail durations are often shorter lasting than equatorial trail observations because of the difference in mid-latitude wind speed and equatorial drift speed. The simulated trails also account for observations showing that equatorial nighttime non-specular meteor trails last significantly longer and are observed more often than daytime trails.


2013 ◽  
Vol 31 (3) ◽  
pp. 473-487 ◽  
Author(s):  
G. Stober ◽  
C. Schult ◽  
C. Baumann ◽  
R. Latteck ◽  
M. Rapp

Abstract. The ECOMA (Existence of Charge state Of meteoric smoke particles in the Middle Atmosphere) sounding rocket campaign was conducted during the Geminid meteor shower in December 2010 in order to explore whether there is a change of the properties of meteoric smoke particles due to the stream. In parallel to the rocket flights, three radars monitored the Geminid activity located at the launch site in Northern Norway and in Northern Germany to gain information about the meteor flux into the atmosphere. The results presented here are based on specular meteor radar observations measuring the radiant position, the velocity and the meteor flux into the atmosphere during the Geminids. Further, the MAARSY (Middle Atmosphere Alomar Radar System) radar was operated to conduct meteor head echo experiments. The interferometric capabilities of MAARSY permit measuring the meteor trajectories within the radar beam and to determine the source radiant and geocentric meteor velocity, as well as to compute the meteor orbit.


2007 ◽  
Vol 66 (12) ◽  
pp. 1133-1141
Author(s):  
S. Ye. Yatsevich ◽  
V. B. Yefimov ◽  
I. A. Kalmykov

2006 ◽  
Vol 84A ◽  
pp. 295-304 ◽  
Author(s):  
Sundararajan SRIDHARAN ◽  
Toshitaka TSUDA ◽  
Takuji NAKAMURA ◽  
Robert A. VINCENT ◽  
EFFENDY

2021 ◽  
Vol 12 (6) ◽  
pp. 573-584
Author(s):  
Xinzhe Yuan ◽  
Weizeng Shao ◽  
Bing Han ◽  
Xiaochen Wang ◽  
Xiaoqing Wang ◽  
...  

Author(s):  
A Ghaleb ◽  
S Even ◽  
R Garello ◽  
B Chapron ◽  
N Pinel ◽  
...  

1968 ◽  
Vol 33 ◽  
pp. 343-351
Author(s):  
B.A. McIntosh

There are many problems in deducing the meteor mass distribution from radar echo observations. Some of these are reviewed in this paper, particular emphasis being placed on the effects of electron attachment and of equipment parameters on the statistics of long-duration echoes.


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