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Ulysses HISCALE Data Analysis Handbook

 

Appendix 9  Geometric Factor Study for the Deflected and Unscattered Electrons of HISCALE (Buckley MS Thesis)

 

A9.2  Chapter 2 - The Geometric Factor and Fluxes

 

Space scientists are interested in particle fluxes for a given particle type at a given energy and location in time and space.  This integral flux J is therefore a function of energy E, particle type a, position x, and time t.

 

Raw data comes in the form of R counts/second.  Space scientists need to convert these count rates into particle fluxes.  Part of this conversion involves the geometric factor G.  The raw count rate R is related to the intensity I of the particle stream by G, the gathering power of the telescope involved: 

 

R =GI

 

For a telescope which is able to distinguish a single particle species over a given energy passband DE, we have for I isotropic that G = G, hence

 

R = GI0,      I0 Isotropic intensity.

 

 

Figure A9-3 Calculating G for simple geometries.

 

Figure A9.3

 

To calculate this G for a simple geometry, imagine that you have a telescope with a detector near the bottom, as in Figure A9-3.  The detector has surface area S, and is broken up into surface elements ds.  An excellent formulation in calculating G for simple geometries is given by J. D. Sullivan2

 

Equation 1

 

where Ω is the domain of solid angle ω, which is determined from the telescope geometry, dω=dϕdcosθ, and dσ•r is the effective element of area looking into ω.

 

So, roughly speaking we can think of G as being an area times an effective solid angle Ω:

 

G=ΔAΔΩ

 

 

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Updated 8/8/19, Cameron Crane

QUICK FACTS

Manufacturer: ESA provided the Ulysses spacecraft, NASA provided the power supply, and various others provided its instruments.

Mission End Date: June 30, 2009

Destination: The inner heliosphere of the sun away from the ecliptic plane

Orbit:  Elliptical orbit transversing the polar regions of the sun outside of the ecliptic plane