Also, I have heard of a 6am or 9am, etc. sun sync orbit. Does this mean
that that local time (described above with respect to the equator) is
always 6am or 9am, etc?
Yes. Because the Earth is not a perfect sphere it tugs on a satellite
differently at the equator than at the pole. This causes the line of nodes
(where the orbit passes through the equator) to move with respect to an
inertial reference. (This is impossible with a perfect sphere or point mass)
The rate at which the nodes move is dependant on the semi-major axis (the
average of the closest and farthest distances from the earth) and the
inclination of the orbit.
A sun synchronous orbit rotates the line of nodes at a rate of 360 degrees/
year which makes the relationship between the line of nodes and the the line
between the sun and earth constant.
The period of the orbit (dependant on the semi-major axis) may vary as long
as the correct inclination is selected to keep the regression of the nodes
at the sun synchronous rate. You are correct in that you will pass over
the earth at the same local time, but it is not necessary to pass over that
spot of the earth on every orbit if the period of the orbit and the rotation of
the earth are not the same. (This is in contrast to the geo-synchronous orbit
where the period of the orbit must the the rotation rate of the earth)
>Also, I have heard of a 6am or 9am, etc. sun sync orbit. Does this mean
>that that local time (described above with respect to the equator) is
>always 6am or 9am, etc?
The local time is a reference to the angle between the orbit plane and the
earth-sun vector which dictates what the local time is below the satellite,
and there is no restrictions on that from a pure orbit mechanics point of
view.
--
ss8...@den.mmc.com - Rick Cooper, Lockheed Martin
-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-
"If you don't want to go around in circles, you have to
be somewhat eccentric." - Equations of Orbital Motion
Pretty much. It isn't quite perfect: You need some fuel for station
keeping, since the orbit is only synchronous if you neglect perturbations
from the Moon, etc. And even so, the local time of day at the
equator crossing will vary by plus of minus 15 minutes or
so, over the course of a year, since the Earth's orbit isn't
perfectly circular. (The difference, by the way, is the
same as the "equation of time" used to correct sun dials
for the non-circularity of the Earth's orbit.)
>Also, I have heard of a 6am or 9am, etc. sun sync orbit. Does this mean
>that that local time (described above with respect to the equator) is
>always 6am or 9am, etc?
That's exactly what it would mean. 6 AM sounds a bit early, but
early morning (and late afternoon) are good sun angles for
some observations. Usually, the height of an object on the
surface is estimated from the length of the shadows it
casts. That means seeing a place at a constant time of
day is convenient (hence the use of a sun synchronous
orbit) and the accuracy of the measurement depends on
the length of the shadows. Ideally, you want a time of
day when there is enough light to see things, but when
the sun angle is low enough that they cast long shadows.
That's early morning and late afternoon.
Frank Crary
CU Boulder
**********
You can also set up sun synchronous orbits that will have no eclipses...
makes things much easier for satellite batteries (load shed when you lose
the sun, emergency cycles only, high depth of discharge) and a bit easier
for thermal cycling.
Satellite batteries are heavy...
Eric The Kouba
The one reason for a SSO (Sun Synchronous Orbit) is - as you say - to
observe the Earth surface at the same local time. However, there is
another argument as well, which is to facilitate the design of the
spacecraft. because its orientation towards the sun is (almost) the same
during the entire mission.
Instead of talking of the local time on the ground track, another
possibility is to say that the angle between the orbital plane and the
axis Earth-Sun remnains the same. This facilitates the way to imagine it
in inertial space. This angle can then directly be translated in a local
time.
However, these issues are explained in any basic Mission Analysis and
Design handbook.
--joachim fuchs
////
(o o)
------------------------------oOO--(_)--OOo-------------------------
Joachim Fuchs European Space Agency
ESA/ESTEC-JPP Earth Observation Preparatory Programme
email: jfu...@eoppsun.estec.esa.nl
tel: +31-71-565-5296
snail: POBox 299, 2200 AG Noordwijk, The Netherlands
And from the Sun! Solar perturbations are particularly troublesome because
the orbit, fairly obviously, tends to be in resonance with them. The major
effect is a slow drift of the inclination.
>...early morning (and late afternoon) are good sun angles for
>some observations. ... Ideally, you want a time of
>day when there is enough light to see things, but when
>the sun angle is low enough that they cast long shadows...
Actually, for observing the Earth's surface, a more fundamental issue
tends to be the desire to minimize cloud cover. Cloud cover generally
increases during the day, because solar heating makes the atmosphere more
active. On the other hand, the first little dose of heat early in the
morning also tends to "burn off" fog and low cloud. Overall, cloud cover
hits a minimum at about 10AM, which is why there's a tight little cluster
of remote-sensing-satellite orbits around 10AM.
--
Unix was a breakthrough. | Henry Spencer
Windows 95 is more like a smash-and-grab. | he...@zoo.toronto.edu
Unfortunately, if you want to stay out of the Van Allen belts, you can't
get a sun-synchronous orbit that is permanently eclipse-free. The problem
is that the sun-synchronous orbits precess around the Earth's axis, which
is not in the plane of the ecliptic, so they don't hold a truly constant
angle to the Sun. Around the summer and winter solstices, when one of
Earth's poles is in permanent shadow, sun-synchronous satellites which
pass that pole low on the spaceward side will pass through Earth's shadow.
All practical sun-synchronous orbits pass low on the spaceward side of
one pole or the other.
By launching just after the relevant solstice, you can arrange for a
satellite to be in permanent sun for about ten months, but that's all.
To get a truly eclipse-free sun-synchronous orbit, you have to go to higher
altitudes... up in the Van Allen belts where the radiation fries your
electronics rather quickly.
now this is a new one for me, but the reason i heard sun synchonicity
was desired was not measuring building heights (which can be measured
at any time of day given the known sun angle, but rather to minimize
shadow changes in the photo so as to maximize photo-analysts chances
of spotting new construction or new building features.
pat
--
Overbreeding leads to weakness, it is a slow death -- Major Katsunagi -
In article <Drv2F9.73G%spen...@zoo.toronto.edu> Henry Spencer
wrote:
>Date: Thu, 23 May 1996 13:49:57 GMT
>From: Henry Spencer <he...@zoo.toronto.edu>
>To: sci-spa...@agate.berkeley.edu
>Newsgroups: sci.space.tech
>Subject: Re: Sun Synchronous Orbit
>
<snipped>
>Actually, for observing the Earth's surface, a more fundamental
issue
>tends to be the desire to minimize cloud cover. Cloud cover
generally
>increases during the day, because solar heating makes the
atmosphere more
>active. On the other hand, the first little dose of heat early in
the
>morning also tends to "burn off" fog and low cloud. Overall,
cloud cover
>hits a minimum at about 10AM, which is why there's a tight little
cluster
>of remote-sensing-satellite orbits around 10AM.
>--
There may be a desire to actually study the cloud cover and then
afternoon orbits are used. NOAA generally flies two orbits, a
morning and an afternoon node crossing time, for the TIROS weather
satellites. The EOS projects in the Mission To Planet Earth
programs also include both morning and afternoon orbits. EOS-AM is
primarily concerned with Earth surface observations while EOS-PM is
looking at Earth radiation balance and other cloud cover effects.
I disagree. You can not do equally good height measurements at
any time of day. What's the length of a shadow at noon, on
the equator, on June 21? You'd need very good resolution to
measure the length of a nonexistent shadow... To get an
accurate measurement of height, you need shadows that are
much longer than the resolution of the image. How much
longer depends on the desired accuracy, but longer
shadows certainly help and that is a motive for sun-synchronous
orbits with early morning passes. As Henry pointed out, it
isn't the only reason as far as the Earth is concerned. I
guess I'm too used to thinking of observations of other planets...
Frank Crary
CU Boulder