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<h2 class="hd hd-2 unit-title">Changing Orbital Altitude</h2>
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<h2>4.5.1 Changing Orbital Altitude</h2>
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<p>Now that we have seen how the energy of an orbit is related to its size and shape, in the next video Prof. Hoffman explains how that relationship can be used to change a spacecraft's orbital altitude, whether to reach a destination further away or to return to Earth at mission's end.</p>
<!--<p><span style="color: #ff0000;"><strong>Text blurb draft: Now that you have seen how the energy of an orbit relates to its size and shape, this video will explain how we can use that relationship to change a spacecraft's orbital altitude, whether to reach a destination further away or to return to Earth at mission's end.<br /></strong></span></p>-->
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<h2 class="hd hd-2 unit-title">The Hohmann Transfer</h2>
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<h2>4.5.2 The Hohmann Transfer</h2>
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<p style="text-align: center;"><em><span style="font-family: 'Open Sans', Verdana, Arial, Helvetica, sans-serif;">Illustrated examples of using the Hohmann Transfer to change orbital altitude in order to reach Mars (left) or Venus (right) (Image credit: <a href="http://www2.jpl.nasa.gov/basics/bsf4-1.php">NASA/JPL</a>)</span></em></p>
<p>In the previous video, we learned that an instantaneous change in velocity can change a spacecraft's orbit from a circular orbit to an elliptical one. However, this maneuver alone is not sufficient to change orbital altitude, since the spacecraft will eventually return to the initial point where the change in velocity occurred. Instead, we have to go one step further to "circularize" the elliptical orbit by performing a Hohmann Transfer. As Prof. Hoffman explains in the following video, the Hohmann Transfer uses two velocity changes at different locations to move a spacecraft between two circular orbits of varying sizes.</p>
<!--<p><span style="color: #ff0000;"><strong>Text blurb draft: In the previous video, you saw how an instantaneous change in velocity can change a spacecraft's orbit from a circular orbit to an elliptical orbit. If the spacecraft remains in space, however, it will return to the point where the change in velocity occurred. In this video, Prof. Hoffman will explain how the Hohmann Transfer uses changes in velocity at two locations to transfer a spacecraft between circular orbits.<br /></strong></span></p>-->
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<h3 class="hd hd-2">Video: Changing Orbital Altitude, Part 2 of 2</h3>
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<h2 class="hd hd-2 unit-title">Changing Orbital Inclination</h2>
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<h2>4.5.3 Changing Orbital Inclination</h2>
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<p>In addition to changing the size and shape of an orbit, it is also often desirable to change the orientation of an orbit in space while preserving the same size and shape. To do this, we turn our discussion to the topic of orbital inclination. In the next video, Prof. Hoffman lists the six parameters that can be used to exactly describe an orbit and the position of an object within it, and explains why it takes a (perhaps surprisingly) large amount of energy in order to change an orbit's inclination.</p>
<!--<p><span style="color: #ff0000;"><strong>Text blurb draft: In the previous videos, we saw how a spacecraft can change the size and shape of its orbit. It is also often desirable to change the orientation of an orbit in space while preserving its size and shape. In this video, Prof. Hoffman describes six quantities that can be used to describe an orbit and the place of an object in it, and the (perhaps surprisingly) large amount of energy needed to change the inclination, or tilt, of one's orbit.<br /></strong></span></p>-->
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<h3 class="hd hd-2">Video: Changing Orbital Inclination, Part 1 of 2</h3>
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<h2 class="hd hd-2 unit-title">The Influence of Launch Location</h2>
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<h2>4.5.4 The Influence of Launch Location</h2>
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Explain how the latitude of a launch site affects orbital inclination and the amount of payload that can be put into orbit " type="button" id="LD">MO 4.8</button></p>
<p><span style="line-height: 25.6000003814697px;">Now that we understand why it is extraordinarily difficult to </span><span style="line-height: 25.6000003814697px;">change orbital inclination, we discuss the implications of this challenge for launching spacecraft into orbit. As we will see, not all launch sites are created equal. In the next video, Prof. Hoffman addresses how the location of a launch site influences </span><span style="line-height: 25.6000003814697px;">the \(\Delta V\) required to achieve orbit, as well as the change in inclination needed to reach geostationary orbit.</span></p>
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<!--<p><span style="color: #ff0000;"><strong>Text blurb draft: Now that you have seen how difficult it is to change one's orbital inclination, in this video, Prof. Hoffman will explain how the location of one's launch site influences the change in inclination needed to achieve geostationary orbit, and even the \(\Delta v\) needed to reach orbit in the first place.<br /></strong></span></p>-->
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<h3 class="hd hd-2">Video: Changing Orbital Inclination, Part 2 of 2</h3>
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The Influence of Launch Location
4.5.4 The Influence of Launch Location
Now that we understand why it is extraordinarily difficult to change orbital inclination, we discuss the implications of this challenge for launching spacecraft into orbit. As we will see, not all launch sites are created equal. In the next video, Prof. Hoffman addresses how the location of a launch site influences the ΔV required to achieve orbit, as well as the change in inclination needed to reach geostationary orbit.
Video: Changing Orbital Inclination, Part 2 of 2
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Video transcript
- Start of transcript. Skip to the end.
- Why did I choose 30 degrees?
- Well, here we get into an interesting question
- of where do we want our satellites ultimately
- to end up?
- Well, it turns out that a lot of satellites we
- want to put in geostationary orbit, which
- is 42,000 kilometers above the center of the Earth
- in the equatorial plane.
- So that as the Earth rotates and the satellites
- are going at the same rotational rate as the Earth,
- they appear to be motionless above one point on the Earth.
- But we launch from various places around the world.
- For instance, in the US, a lot of our flights
- go out of Cape Canaveral.
- In Russia, they go out of Kazakhstan, Baikonur.
- The Europeans have a launch site in Kourou in French Guiana.
- Let's take a look now at what happens
- when we launch out of Florida.
- I'm going to take my orbit and I'm
- going to put it right over Florida here.
- And of course, the plane of the orbit
- has to go through the center of the Earth.
- So that means that in this case, the northernmost point
- of our orbit-- this is assuming we fly directly to the east
- once we launch out of Florida.
- The northernmost point is going to be
- at the latitude of Cape Canaveral, which is
- about 28 and 1/2 degrees north.
- And the other side of the orbit is
- going to be 28 degrees south.
- Now I have a little bit of freedom when I launch.
- I don't have to launch due east.
- I could launch a little bit to the north, in which case
- for instance, if I want to fly to a high inclination
- near polar orbit, I'll fly to the north out of the Cape
- and I'll go into a much higher inclination orbit.
- What happens now if I want to get to a lower inclination
- orbit?
- Well, let's go back to an easterly trajectory.
- Now let's launch further to the south.
- Does that get me into a lower inclination orbit?
- No, not at all, because look what happens
- on the other side of the orbit.
- Its going to a higher northerly attitude.
- So no matter what I do, I could rotate,
- but the pivot point goes right around our launch site.
- And the net result is that by launching due east,
- I go into an orbital inclination which
- is inclined to the Equator at an angle equal to the latitude
- of my launch site, 28 and 1/2 degrees for Cape Canaveral.
- Any other launch azimuth to the north or south,
- and I go into a higher inclination orbit,
- and it doesn't matter whether I go to the north or the south.
- A lot of satellites that we launch ultimately
- are destined to become telecommunication satellites
- at geostationary orbits, which means
- that they have to be over the equator
- because the Earth is rotating.
- And out at 42,000 kilometers from the center of the Earth,
- the satellites will be in a circular orbit
- with the same period as the Earth's rotation,
- and so they will appear to be stationary.
- But you have to get from a 28 degree orbit
- to a 0 degree inclination orbit, and as we saw,
- that's incredibly expensive if we do it near the Earth
- where our orbital velocity is 7.9 kilometers per second.
- So here's how we do it.
- We actually go into what we call a geostationary transfer
- orbit using a Hohmann Transfer, which we now understand.
- We do a burn and we go out to apogee.
- And now of course using Kepler's second law,
- we know that the velocity out at apogee
- is a lot smaller than the velocity at perigee.
- And so instead of having to change
- the 7.9 kilometers per second, it's a much lower burn.
- And so if you want to change your inclination
- and you're in an elliptical orbit, for goodness sakes,
- change it when you're far away near apogee
- and you're moving as slowly as possible.
- Now that was the situation for Cape Canaveral at 28 degrees.
- The European launch center at Kourou in French Guiana
- is only 6 degrees north of the Equator.
- And so when they are launching geostationary satellites
- for telecommunications purposes, they only
- have to change their inclination by 6 degrees
- whereas from Cape Canaveral we have to change it
- by 28 and 1/2 degrees.
- And the poor Russians launching from Kazakhstan-- they've
- got 51 degrees that they have to change if they want
- to go to geostationary orbit.
- So a couple of takeaway points.
- First of all, getting into geosynchronous orbit
- takes different amounts of propellant because
- of the inclination change that you
- have to make for different latitudes of launch sites.
- Also, remember geostationary orbit
- is the orbit that is economically useful right
- above the equator.
- Geosynchronous just means 24 hour period.
- Geostationary-- inclination of zero right above the equator.
- The second critical point: for a given latitude of a launch
- site, the minimum orbital inclination
- that you can fly into directly is
- equal to the latitude of a launch site.
- And the third point is if you want
- to get to geostationary orbit, you
- have to change your orbital inclination.
- And the higher the latitude of your launch site, the more
- inclination change you're going to have to make.
- Now there's one other factor where launch sites have
- a difference in their ability to get to orbit,
- and that's because the Earth is rotating.
- Every 24 hours we spin around, and if you calculate
- the velocity at the equator of the Earth, it's about half
- a kilometer a second.
- Compared to the roughly 8 kilometers a second
- that you need in orbit to have orbital velocity,
- that's a reasonable fraction and that makes a difference.
- And if you take off right from the Equator,
- you can count that extra half a kilometer
- per second you get from the Earth.
- I mean, that's as good as burning rocket fuel.
- In fact, it's a lot less expensive.
- The problem is you go to more northerly latitudes
- is that the eastward component of the Earth's rotation
- decreases as the cosine of your latitude.
- So by the time you get up to Cape Canaveral,
- that half a kilometer per second you get at the Equator
- has gone down to 4/10.
- And by the time you get up to the 51 degrees
- up in Kazakhstan, it's gone down to about 3/10
- of a kilometer per second.
- So this extra 100 or 200 meters per second,
- that makes quite a difference in terms
- of the amount of propellant you have to burn.
- Of course, if you're going into a polar orbit
- and you want to launch to the north,
- then you don't really care about the rotation of the Earth.
- But for an eastward trajectory where
- you're flying into a typical orbit or an orbit
- from which you're going to transfer
- to geostationary orbit, you do get a boost
- from the Earth's rotation.
- And the closer you order the equator,
- the bigger that boost is.
- So we've seen quite a bit, and just a brief review
- of where we've gotten to here.
- We looked at simple circular orbits,
- and we derived some relationships
- in speed, period, which we found actually duplicated
- some of Kepler's laws.
- Which applied of course not just to the simple circular orbits
- where we did the math, but to elliptical orbits in general.
- And we saw the very important relationship
- that the energy of the orbit varies
- with the semi-major axis, and a larger orbit
- has a larger energy.
- We looked at what's involved in changing orbits,
- using Hohmann Transfer to change the size of the orbit
- to go from one nearly circular orbit to either a larger
- or a smaller orbit.
- And we looked at the implication of orbital inclination.
- What it takes to change the inclination.
- Why it's so difficult to change the inclination once
- you are already in orbit.
- And therefore, the importance of the launch site
- in getting to orbits of general inclinations.
- And the fact that the closer you are to the equator--
- if you want to end up in an equatorial orbit,
- which is what we want for geostationary satellites--
- that you definitely have advantages.
- Both because of not having to change the orbital inclination
- so much, and because you get more of a boost
- from the rotation of the Earth.
- End of transcript. Skip to the start.
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