Author Topic: ESA - Swarm updates  (Read 40234 times)

Offline bolun

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Re: ESA - Swarm updates
« Reply #20 on: 02/22/2018 06:28 pm »
https://www.esa.int/Our_Activities/Observing_the_Earth/Swarm/Swarm_trio_becomes_a_quartet

Swarm trio becomes a quartet

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With the aim of making the best possible use of existing satellites, ESA and Canada have made a deal that turns Swarm into a four-satellite mission to shed even more light on space weather and features such as the aurora borealis.

In orbit since 2013, ESA’s three identical Swarm satellites have been returning a wealth of information about how our magnetic field is generated and how it protects us from dangerous electrically charged atomic particles in the solar wind.

Canada’s Cassiope satellite carries three instrument packages, one of which is e-POP.  It delivers information on space weather which complements that provided by Swarm. Therefore, the mission teams began looking into how they could work together to make the most of the two missions.

To make life easier, it also just so happens that Cassiope’s orbit is ideal to improve Swarm’s readings.

And now, thanks to this international cooperation and formalised through ESA’s Third Party Mission programme, e-POP has effectively become a fourth element of the Swarm mission. It joins Swarm’s Alpha, Bravo and Charlie satellites as Echo.

Image credit: Canadian Space Agency, 2018

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Offline bolun

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Re: ESA - Swarm updates
« Reply #22 on: 02/12/2019 03:08 pm »
Magnetic north on the move

Driven largely by the churning of fluid in Earth’s core, which generates the magnetic field, the magnetic north pole has always drifted. Around 50 years ago, the pole was ambling along at around 15 km a year, but now it is charging ahead at around 55 km a year, leaving the Canadian Arctic heading towards Siberia.

Related article: Swarm helps pinpoint new magnetic north for smartphones

https://www.esa.int/spaceinimages/Images/2019/02/Magnetic_north_on_the_move

Image credit: DTU Space

Offline bolun

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Re: ESA - Swarm updates
« Reply #23 on: 05/05/2019 08:55 am »
Simulation of the magnetic field in Earth’s core

Earth’s core as modelled in the numerical geodynamo simulation as part of research into geomagnetic jerks and rapid hydromagnetic waves published as the cover story in Nature Geosciences, May 2018. The magnetic field lines (orange) are stretched, twisted and folded by the turbulent convection producing shear of electrically conducting fluid (red and blue). Hydromagnetic waves are triggered when the shear is misaligned with field lines, and propagate along these lines to the surface of the core where they can focus and cause geomagnetic jerks.

Related article: Swarm helps explain Earth's magnetic jerks

https://www.esa.int/spaceinimages/Images/2019/05/Simulation_of_the_magnetic_field_in_Earth_s_core

Image credit: Julien Aubert, IPGP/CNRS/CNRS Photothèque

Offline bolun

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Re: ESA - Swarm updates
« Reply #24 on: 05/15/2019 07:13 pm »
https://www.esa.int/Our_Activities/Observing_the_Earth/Swarm/Tug-of-war_drives_magnetic_north_sprint

Tug-of-war drives magnetic north sprint

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Unlike our geographic North Pole, which is in a fixed location, magnetic north wanders. This has been known since it was first measured in 1831, and subsequently mapped drifting slowly from the Canadian Arctic towards Siberia.

One of the practical consequences of this is that the World Magnetic Model has to be updated periodically with the pole’s current location. The model is vital for many navigation systems used by ships, Google maps and smartphones, for example.

One of the many areas of research using information from Swarm focuses on explaining why the pole has picked up such a pace – and a subject being discussed at this week’s Living Planet Symposium.
 
Between 1990 and 2005 magnetic north accelerated from its historic speed of 0–15 km a year, to its present speed of 50–60 km a year. In late October 2017, it crossed the international date line, passing within 390 km of the geographic pole, and is now heading south.

In fact, recently, the World Magnetic Model had to be updated urgently because of the speed at which the pole is moving.

ESA’s Swarm mission is not only being used to keep track of magnetic north, but scientists are using its data to measure and untangle the different magnetic fields that stem from Earth’s core, mantle, crust, oceans, ionosphere and magnetosphere.

Our magnetic field exists because of an ocean of superheated, swirling liquid iron that makes up the outer core. Like a spinning conductor in a bicycle dynamo, this moving iron creates electrical currents, which in turn generate our continuously changing magnetic field.

Tracking changes in the magnetic field can, therefore, tell researchers how the iron in the core moves.

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Research is showing that changes in the pattern of core flow between 1970 and 1999 elongated the Canadian lobe, significantly weakening its signature on Earth's surface, causing the pole to accelerate towards Siberia.

Simple models taking account of this process and describing future geomagnetic change predict that over the next decade the north magnetic pole will continue on its current trajectory and will travel a further 390–660 km towards Siberia.


Online jacqmans

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Re: ESA - Swarm updates
« Reply #25 on: 07/09/2021 02:16 pm »
Swarm yields new insight into animal migration
09/07/2021

Using measurements from ESA’s Earth Explorer Swarm mission, scientists have developed a new tool that links the strength and direction of the magnetic field to the flight paths of migrating birds. This is a huge step forward to understanding how animals use Earth’s magnetic field to navigate vast distances.

These days, it is almost unimaginable for us to set off on a long journey without being equipped with some form of satellite navigation, or at least a map. Migratory animals, however, manage to cross entire oceans and continents, navigating with exceptional skills of their own. In spite of decades of research, we still do not understand fully how these remarkable animals are able to find their way – although it has been suspected that Earth’s magnetic field lines are among the cues that guide them.

Recent advances in GPS and the miniaturisation of tracking devices have allowed ecologists to tag migratory animals, from birds to whales, to understand how they travel from A to B. However, while animal tracking data are now common, little investigation has been made into how animals respond to real geomagnetic conditions, since the magnetic field changes continuously across the globe, particularly during geomagnetic storms.

Until recently, there was no way to assess accurately the strength of the magnetic field at the time and location that animals pass by, which would allow ecologists to study how they use this natural force for navigation.

However, a new tool allows ecologists, for the first time, to compute the strength and direction of the magnetic field along animal migratory paths.

https://www.esa.int/Applications/Observing_the_Earth/Swarm/Swarm_yields_new_insight_into_animal_migration
Jacques :-)

Offline bolun

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Re: ESA - Swarm updates
« Reply #26 on: 07/14/2022 06:37 pm »
https://twitter.com/esaoperations/status/1547562942672936965

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What’s worse than dealing with deadly #SpaceDebris and violent #SpaceWeather?

Dealing with both at the same time!

@esa_swarm has dodged a potential collision at short notice, right in the middle of its 10-week climb to escape the Sun’s wrath:

https://esa.int/Space_Safety/Swarm_dodges_collision_during_climb_to_escape_Sun_s_wrath

Offline bolun

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Re: ESA - Swarm updates
« Reply #27 on: 10/10/2022 07:45 pm »
Again  :o

https://twitter.com/esa_swarm/status/1579381331884404736

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"Collision avoided! 💥 In the wee small hours this morning Swarm-Alpha was moved out of harm's way - space debris in the form of a rocket body 🚀 that has been threatening our inner duo  🫣  Thanks to the hard work of the @esaoperations Space Debris Office for guiding us clear!

Offline bolun

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Re: ESA - Swarm updates
« Reply #28 on: 11/07/2022 04:51 pm »
https://twitter.com/esa_swarm/status/1589565513541517312

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Collision avoided! 💥 No fireworks for Swarm Charlie this weekend thanks to the timely work of the space debris office, flight dynamics team & more @esaoperations, who swerved us out of the way of a small spacecraft early on Sunday morning 🚀 It’s busy up there!

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It's getting busier. This is the 6th time we’ve had to move one of the Swarm satellites out of harm’s way this year, and the 22nd time we’ve had to call in a collision avoidance manoeuvre operation 🫣 That’s compared to 13 in the whole of 2021.
« Last Edit: 11/07/2022 04:53 pm by bolun »

Online jacqmans

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Re: ESA - Swarm updates
« Reply #29 on: 06/12/2024 01:55 pm »
Swarm helps discover Steve's long-lost twin
03/06/2024

Ever since aurora chasers discovered Steve, a mysterious ribbon of purple light in the night sky, scientists have wondered whether it might have a secret twin. Now, thanks to a photographer’s keen eye, and data from ESA’s Swarm satellites, we may have found it.

Steve was a sensation when scientists stumbled across it a few years ago, thanks to the eagle eyes and excellent photography of the Alberta Aurora Chasers Facebook group.

But its mauve hue and fleeting appearance meant it couldn’t be a feature of the aurora borealis, commonly known as the northern lights, which comes in shades of green, blue and red and can last for hours. So, what could it be?

Fortunately, ESA’s trio of magnetic-field monitoring Swarm satellites were perfectly placed to help investigate.

It turned out that Steve was a fast-moving stream of extremely hot gas called a sub-auroral ion drift. Or, to give Steve its full name, a strong thermal emission velocity enhancement.

https://www.esa.int/Applications/Observing_the_Earth/FutureEO/Swarm/Swarm_helps_discover_Steve_s_long-lost_twin
Jacques :-)

Offline AndrewM

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Re: ESA - Swarm updates
« Reply #30 on: 12/02/2024 11:53 pm »
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Approximately 41 000 years ago, Earth’s magnetic field briefly reversed during what is known as the Laschamp event. During this time, Earth’s magnetic field weakened significantly—dropping to a minimum of 5% of its current strength—which allowed more cosmic rays to reach Earth’s atmosphere.

Scientists at the Technical University of Denmark and the German Research Centre for Geosciences used data from ESA’s Swarm mission, along with other sources, to create a sounded visualisation of the Laschamp event. They mapped the movement of Earth’s magnetic field lines during the event and created a stereo sound version which is what you can hear in the video.
The soundscape was made using recordings of natural noises like wood creaking and rocks falling, blending them into familiar and strange, almost alien-like, sounds. The process of transforming the sounds with data is similar to composing music from a score.


Online jacqmans

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Re: ESA - Swarm updates
« Reply #31 on: 01/22/2025 11:55 am »
Swarm detects tidal signatures of our oceans
22/01/2025

A study using data from ESA’s Swarm mission suggests that faint magnetic signatures created by Earth’s tides can help us determine magma distribution under the seabed and could even give us insights into long-term trends in global ocean temperatures and salinity.

Swarm is a constellation of three satellites that study Earth’s geomagnetic field. This magnetic field that extends from Earth’s interior into space is thought to be produced largely by an ocean of liquid iron in the planet’s outer core. Other sources of magnetism include magnetised rocks in the crust.

And although we might not normally think of oceans as generating magnetism, the salty sea water is a moderate electrical conductor. This means that as tides flow across Earth’s magnetic field, they generate weak electric currents, which in turn induce small magnetic signals – that can be detected from space.

With its satellites flying at an altitude between 462 km and 511 km, Swarm measures Earth’s magnetic field more accurately than ever before. It can detect faint tidal signatures and distinguish them from other stronger magnetic field sources from Earth’s interior.

“This study shows that Swarm can provide data on properties of the entire water column of our oceans.” says Anja Strømme, ESA’s Swarm Mission Manager.

Swarm’s data can also provide insights into the distribution of magma, which could in future support better understanding of events such as the Hunga-Tonga volcanic eruption of 2022.

The study of these signatures made the front cover of the world’s oldest scientific journal, Philosophical Transactions of the Royal Society A, and was conducted by a team from the University of Cologne and the Technical University of Denmark.

Swarm gets better with age

The mission, launched in 2013, was only meant to fly for four years but is now in its 12th year. Anja adds: “This is one of the benefits of flying missions for longer than originally planned. So, by flying as long as the scientific output is of excellent quality and resources allow, you can tackle scientific questions that weren’t originally envisaged.”

Swarm is, however, slowly nearing the natural end of its lifespan as drag gradually brings the satellites physically closer to Earth. This has enabled the mission’s instruments – the satellites carry state-of-the-art sensors including magnetometers that measure the strength, magnitude and direction of the magnetic field – to capture faint signals that would be more difficult to detect from the higher orbits at the start of the mission.

https://www.esa.int/Applications/Observing_the_Earth/FutureEO/Swarm/Swarm_detects_tidal_signatures_of_our_oceans#msdynmkt_trackingcontext=be6c260f-a425-4e8c-a9b9-94233b81ad42
Jacques :-)

Online jacqmans

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Re: ESA - Swarm updates
« Reply #32 on: 10/14/2025 06:45 am »
Swarm reveals growing weak spot in Earth’s magnetic field
13/10/2025

Using 11 years of magnetic field measurements from the European Space Agency’s Swarm satellite constellation, scientists have discovered that the weak region in Earth’s magnetic field over the South Atlantic – known as the South Atlantic Anomaly – has expanded by an area nearly half the size of continental Europe since 2014.

Earth’s magnetic field is vital to life on our planet. It is a complex and dynamic force that protects us from cosmic radiation and charged particles from the Sun.

It is largely generated by a global ocean of molten, swirling liquid iron that makes up the outer core around 3000 km beneath our feet. Acting like a spinning conductor in a bicycle dynamo, it creates electrical currents, which in turn, generate our continuously changing electromagnetic field – but in reality the processes that generate the field are far more complex.

Swarm, an Earth Explorer mission developed under ESA’s Earth Observation FutureEO programme, comprises a constellation of three identical satellites that precisely measure the magnetic signals that stem from Earth’s core, mantle, crust and oceans, as well as from the ionosphere and magnetosphere.

Thanks to this exceptional mission, scientists are gaining more insight into the different sources of magnetism to help understand how and why the magnetic field is weakening in some places and strengthening in others.

The weak field South Atlantic Anomaly was first identified southeast of South America back in the 19th century.

Today, the South Atlantic Anomaly is of particular interest for space safety, as satellites passing over the region are faced with higher doses of incoming radiation. This can lead to malfunctions or damage to critical hardware, and even blackouts.

Published this month in Physics of the Earth and Planetary Interiors, the latest results from the Swarm mission reveal that while the South Atlantic Anomaly expanded steadily between 2014 and 2025, a region of the Atlantic Ocean southwest of Africa has experienced an even faster weakening of Earth’s magnetic field since 2020.

“The South Atlantic Anomaly is not just a single block,” says lead author Chris Finlay, Professor of Geomagnetism at the Technical University of Denmark. “It’s changing differently towards Africa than it is near South America. There’s something special happening in this region that is causing the field to weaken in a more intense way.”

This behaviour is linked to strange patterns in the magnetic field at the boundary between Earth’s liquid outer core and its rocky mantle, known as reverse flux patches.

Prof. Finlay explains, “Normally we’d expect to see magnetic field lines coming out of the core in the southern hemisphere. But beneath the South Atlantic Anomaly we see unexpected areas where the magnetic field, instead of coming out of the core, goes back into the core. Thanks to the Swarm data we can see one of these areas moving westward over Africa, which contributes to the weakening of the South Atlantic Anomaly in this region.”

https://www.esa.int/Applications/Observing_the_Earth/FutureEO/Swarm/Swarm_reveals_growing_weak_spot_in_Earth_s_magnetic_field#msdynmkt_trackingcontext=6397c17e-3c3a-425a-baac-7c20e7870300
Jacques :-)

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