The first-ever quadruple launch towards Galileo constellation completion

On 17 November, four Galileo satellites are scheduled for the first-ever quadruple launch atop a single Ariane 5 rocket, as a step that brings the European navigation satellite system closer to completion.

For the time being, Galileo has 14 out of 24 operational satellites in orbit. Thursday’s launch will be the eighth so far for the European navigation system and will be the largest increase of any navigation satellite constellation from a single launch, bringing the number of satellites in space to 18. By 2020, the 24-satellite Galileo constellation is expected to be complete and along with a globally distributed ground network it will provide positioning, navigation and timing (PNT) services.

Illustration du vol VA 233 Ariane 5 ES avec les Galileo

Illustration du vol VA 233 Ariane 5 ES avec les Galileo

Until now, the Russian Soyuz rockets have been used to carry two satellites at a time. The quartet, though, this time will be carried into orbit through a specially modified Ariane 5 rocket using a new payload dispenser that will be able to release the satellites all at once into orbit. Although this is a great boost from European Space Agency to accelerate the constellation integration, there are various technical challenges regarding the almost simultaneous control over four independent satellites which increases the mission complexity.

The identical four 715 kg satellites are made by OHB System in Germany, while their navigation payloads are made by the British company Surrey Satellite Technology. The highly accurate timing required for precise PNT services is based on four atomic clocks that each Galileo satellite will carry: two Passive Hydrogen Maser clocks, and two Rubidium Atomic Frequency Standard (RAFS) clocks, which lead to a fourfold redundancy on each satellite in order to ensure stable operations over their whole lifetime.

Launch and Orbital Information

The launch of the four new satellites atop the Ariane 5 rocket is scheduled at 13:06 GMT (14:06 CET) on 17 November and will take place from Europe’s spaceport at Kourou, French Guiana. Although Galileo constellations’ operating orbital altitude is 23200 km, the target orbit of the quartet is actually 300 km below it, at 22900 km, allowing the four satellites to manoeuvre themselves up to the operating altitude. The reason behind this decision lies in two recent analyzed anomalies occurring in the rubidium atomic clocks aboard orbiting Galileo satellites. The ascent into this Medium Earth Orbit (MEO) will take approximately three and a half hours.

After the separation of the four satellites two by two and the placing of Ariane’s upper stage into a stable “graveyard” orbit, a combined team from ESA and CNES space agencies will take over in shifts and shepherd the Galileo satellites through their early orbits through a series of critical activities and manoeuvres. This task, however, cannot be done in a single step but rather in pairs due to its high complexity. During the manoeuvring of the first pair of satellites, there will be no activities for the second one, being in the phase known as “babysitting” and waiting for its turn.

The control of the satellites, after they get successfully onto their “drift” orbits using their onboard thrusters, will be handed over to the Galileo Control Centre in Oberpfaffenhofen, Germany, which is responsible for the satellites’ command and control for the whole of their operating lives. Except for the extensive health checks to be conducted, the tasks of the specialists include: 

  • Ensuring that each satellite has deployed its power-giving solar panels correctly and pointed towards the Sun, putting an end to their reliance on their onboard batteries and start using limitless solar power,
  • Establishing a viable data link via a network of ground stations, and
  • Switching the spacecrafts from Sun-pointing to a stable Earth-pointing mode. The satellites then will settle into their normal mode, with the navigation antenna pointing towards Earth and the solar arrays tracking the Sun.

Despite the mission’s complexity, everyone involved in the forthcoming launch has put a lot of effort in it and worked through numerous trainings and simulations to ensure that the launch will be successful and the Galileo satellites will arrive safe and sound into their nominal orbits, expected early in 2017.

If you are excited about the first-ever launch of the Galileo quartet as we are at Geoawesomeness, then you can visit the following link to watch the launch of Galileos 15-18: http://www.esa.int/Our_Activities/Navigation/Galileo/Launching_Galileo/Watch_the_launch_of_Galileos_15_18

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NASA time-lapse shows just how fast the Arctic sea ice is vanishing

Climate change is for real and it’s increasingly looking like a problem that is already going to affect the current generation in a big way. The latest time-lapse from NASA showing just how fast the Arctic sea ice has vanished in the last three decades is a chilling reality check about the state of our planet!

It’s not just that the ice is vanishing in the Arctic sea, the oldest and thickest ice has also continued to melt away, leaving the Arctic sea cap more vulnerable to the continued rise in temperature – both in our oceans and the atmosphere.

“Ice age is a good analog for ice thickness because basically, as ice gets older it gets thicker, This is due to the ice generally growing more in the winter than it melts in the summer.” – Walt Meier, sea ice researcher at NASA’s Goddard Space Flight Center

Arctic Sea Ice Is Vanishing

The time-lapse from NASA below, shows the annual change in the arctic sea ice age since January 1, 1984. It’s chilling to see how much of the artic sea cap has vanished in the last three decades.

 

https://www.youtube.com/watch?v=6ZAuRpK4tkc

Video Credit: NASA’s Scientific Visualization Studio/Cindy Starr

“What we’ve seen over the years is that the older ice is disappearing, This older, thicker ice is like the bulwark of sea ice: a warm summer will melt all the young, thin ice away but it can’t completely get rid of the older ice. But this older ice is becoming weaker because there’s less of it and the remaining old ice is more broken up and thinner, so that bulwark is not as good as it used to be.” – Walt Meier, sea ice researcher at NASA’s Goddard Space Flight Center. 

The video below is a slightly longer version of the time-lapse with much more detailed explanations.

Video Credit: NASA’s Scientific Visualization Studio/Cindy Starr

For more information, check out the article written by the NASA Science team (link).

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