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Re: (meteorobs) Distance for simultaneous meteor observation



birger.andresen@fesil.no wrote:
>
> Definitions :
>   s = distance [km] ALONG the earth surface from where
>         the meteor is at zenith (the "zenith location").
> 
>   h = height [km] of the meteor (typical 80-120 km) at the
>         "zenith location".
> 
>   r = earth radius (approx 6378 km)
> 
>   A(rad) = Angel [radians] above the horizon at which you see
>         the meteor at s km away from the "zenith location".
> 
>   A(deg) = Same as A(rad), but in degrees (360 deg = full circle)
> 
> Calculations :
> 
>                                h cos(B) - (r - r cos(B))
>      A(rad) = arctan ---------------------------------------
>                                 r sin(B) + h sin(B)
> 
>   where B = s / r
> 
>      A(deg) = A(rad) * 260 / (2 Pi)   ; Pi = 3.141592
> 
> Examples :
> 
>     Meteor height = h = 80 km :
>        In the horizon at s = 1000 km,
>        30 deg above the horizon at s = 135 km
>        45 deg above the horizon at s = 80 km
> 
>     Meteor height = h = 100 km :
>        In the horizon at s = 1120 km,
>        30 deg above the horizon at s = 166 km
>        45 deg above the horizon at s = 97 km
> 
>     Meteor height = h = 120 km :
>        In the horizon at s = 1225 km,
>        30 deg above the horizon at s = 200 km
>        45 deg above the horizon at s = 116 km
>

Birger,

The formula you present seems to be a trigonometric identity to my
formula. The difference is my formula (reproduced again, below) shows
the distance of the meteor, "s" (which = my 'd') as a function of the
observed altitude angle "A", rather than the other way around, as in
your formula.

Also, I use the earth radius r=6367km, as the mean of the equatorial and
polar radii. 6378km is the equatorial radius only.

Mike.

--------------------------distance formula------------------------------
d = distance from observer to meteor sub-earth point (which is the point
on the earth directly below the meteor). (d is measured along the earth
surface in km)

A = altitude of meteor as seen by observer (degrees).

h = height of meteor above the earth surface (km).

R = radius of the earth (km).

we get:

d = (pi/180) * R * [ARCCOS(COS(A)/(1+h/R)) - A]
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