The probabilit y distribution for the e nvelo pe of t he received s ignal co mposcd of re fl ect ions from man y m eteor tra ils is d erived t heore ticall y. Both t he effects o f nu merou , s ma ll meteors a nd the residu al refl ections from infrequen t , large meteors are treated imu lt a neousl.v.
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Albert D. Wheelon (1960) studied this question.
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