GOES-15: The most important thing to know about GOES, the Global Observing-1 satellite.
article The GOES constellation is a three-ringed satellite that captures the entire sky.
It’s a satellite that’s a constellation, so it’s one of the biggest and most expensive satellites in the world.
The GOes constellation is very well understood by people because it’s a very precise system.
So when the GOES satellites launched, they went into a very controlled way of deploying them, because we had very good guidance.
So we had all the correct parameters, and they went in that way.
But then the satellites went in different ways and they were deployed in a very different way.
And we’re seeing this really, really, very interesting evolution now in terms of how the satellites are deployed and how they’re used.
That’s what we’re trying to understand.
So for the GOes satellites, the primary focus is to monitor the solar wind, the solar radiation.
That is the radiation that’s produced by the sun.
It does the most energy, and it’s very important to understand that because we can predict when that radiation will be coming in, and what that radiation is going to do to our planet.
So that’s the main focus.
Next up is the atmosphere.
So this is the most important satellite.
It will be the main piece of the puzzle for understanding what the atmosphere looks like.
So it will be a great place to watch.
Next is the Earth.
And it’s another piece of that puzzle.
And the next piece of this puzzle is the satellites.
The satellites are in a position to get a lot of information about the Earth, and that’s because we’ve got a lot more satellites.
And that’s going to be the key.
So next is the magnetosphere, the upper atmosphere.
And what we can see is that it’s really a very complicated picture, because the Earth is very small.
It has this little cloud of material that’s floating around, and there’s a little bit of it that’s spinning, and the Earth spins very fast, so there’s lots of little particles that are spinning and reflecting off the surface of the Earth that’s in the magnetospheric layer.
And they reflect a lot less sunlight than the Earth itself.
And there’s an additional layer of Earth that doesn’t reflect much sunlight at all.
So what we see on the satellites is that there’s this big mass of stuff that’s not reflecting as much sunlight as the Earth does.
And this is called the Earth-like plane.
So in the case of the GOEs, they’re looking at that plane.
We can see it as a thin line of cloud that’s swirling around the Earth like this.
And then we see the Earth at night.
And as we get deeper into the atmosphere, we see a lot brighter spots.
So then we get into the magneto-magnetic environment.
And these are the denser parts of the atmosphere where we get the most information about Earth’s magnetic field.
And when you have a lot on the surface, you get very strong magnetic fields.
So there’s really no way to know what’s there without looking down and looking at it.
So they’re really looking at the surface at night, and in the daytime you get the very strong magnetosphere.
And in the nighttime, there’s just a little layer of low density clouds.
And so the GOE satellites are looking at this layer of dense clouds that’s mostly ice, and so it does not reflect as much solar radiation as the magnetos, but it does reflect the sun’s light.
And also, it’s getting very hot, and a lot hotter than the surface.
And all of these things are really important for understanding the Earth’s atmosphere.
You know, the magnetoreception is actually quite different from what we do in the field, because there’s so much of the sun in the atmosphere at once.
So if we could do something like a satellite survey every 30 minutes, you could actually get a good sense of the different layers of the air.
But for the most part, we can only do that every day.
So a lot, a lot depends on what time of day it is.
So as you get closer to the Earth or you get out into space, we get very different information.
So the GOAs are looking right now at the magnetoclast layer, which is basically the polar layer.
But they are also looking right at the very top of the magnetogravitic layer, because that’s where all the ice is.
And a lot has changed in the past couple of decades.
So basically, we now know that there is a large change in the magnetic field in the polar regions.
And for example, we know that the north pole has shifted.
The north pole is really getting warmer.
And because of that, the polar magnet