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Dynamics cheat sheet

my dynamics notes - 12000.org

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magnitude of ⃗r<br />

period T<br />

mean satellite speed n<br />

r = a ( 1 − e 2)<br />

1 + e cos θ = h2 1<br />

µ 1 + e cos θ<br />

r cos θ = a (cos E − e)<br />

r = a (1 − e cos E)<br />

√<br />

T = 2 h πab = 2π a 3<br />

µ<br />

n = 2π<br />

T = √<br />

µ<br />

a 3<br />

eccentric anomaly E tan θ 2 = √<br />

1+e<br />

1−e tan E 2<br />

area sweep rate<br />

dA<br />

dt = h 2<br />

equation of motion ¨⃗r +<br />

µ<br />

r 3 ⃗r = 0<br />

(eq 4.2-14 Bate book)<br />

spherical coordinates relation cos(i) = sin(A z ) cos(φ) where i is the inclination<br />

and A z is the azimuth and φ is latitude<br />

2<br />

Notice in the above, that the period T of satellite depends only on a (for same µ)<br />

In the above, µ = GM where M is the mass of the body at the focus of the ellipse and G is the gravitational<br />

constant. h is the specific mass angular momentum (moment of linear momentum) of the satellite. Hence the<br />

units of h2<br />

µ<br />

is length.<br />

To draw the locus of the satellite (the small body moving around the ellipse, all what we need is the<br />

eccentricity e and a, the major axes length. Then by changing the angle θ the path of the satellite is drawn. I<br />

have a demo on this here<br />

See http://nssdc.gsfc.nasa.gov/planetary/fact<strong>sheet</strong>/earthfact.html for earth facts<br />

This table below is from my class EMA 550 handouts (astrodynamics, spring 2014)<br />

2 Image is from my class notes, page 7-9, EMA 550, Univ. Of Wisconsin, Madison by professor S. Sandrik<br />

67

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