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As Man continues to search for new discoveries in space, and answers to some of life’s
biggest questions – such as are we alone in the universe? – our desire to understand
more about our place in the universe has led to us gaining a better understanding of
the Solar System. In this book we take a closer look at the star that lies at the centre of
our Solar System. Discover the impact the Sun has on our lives and everything
around us, and nd out how this ball of hot plasma formed. Read about the eight
planets that make up our Solar System, whether you want to learn why Saturn has
rings, how life formed on Earth, if we could live on Mars, or why Neptune looks so
blue. On top of that, you can nd out about four of the most interesting moons of the
Solar System; Ganymede, Europa, Titan and our very own Moon. See what rolesthese satellites play, and why they are so important. Packed with essential guides and
incredible illustrations, this book will help bring the Solar System to life!
Welcome to the
SolarSystem
BOOK OF THE
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Imagine Publishing LtdRichmond House33 Richmond Hill
BournemouthDorset BH2 6EZ
+44 (0) 1202 586200Website: www.imagine-publishing.co.uk
Twitter: @Books_ImagineFacebook: www.facebook.com/ImagineBookazines
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Distributed in the UK & Eire by Imagine Publishing Ltd, www.imagineshop.co.uk. Tel 01202 586200
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DisclaimerThe publisher cannot accept responsibility for any unsolicited material lost or damaged in the
post. All text and layout is the copyright of Imagine Publishing Ltd. Nothing in this bookazine maybe reproduced in whole or part without the written permission of the publisher. All copyrights are
recognised and used specifically for the purpose of criticism and review. Although the bookazine hasendeavoured to ensure all information is correct at time of print, prices and availability may change.
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All About Space Book of the Solar System © 2014 Imagine Publishing Ltd
ISBN 978-1909758483
bookazine series
Part of the
SolarSystem
BOOK OF THE
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ContentThe Sun The planets The moons10 The SunExplore the star keeps us all alive22 Solar ares
A look at how these can pose a real risk
28 The hole in the SunFind out more about NASA's discovery
30 Solar maximumRead about the activity of the Sun
134 The MoonEarth's only satellite explained
146 GanymedeDiscover the most planet-like moon
156 EuropaCould this moon be capable ofsupporting life?
166 TitanExplore one of Saturn's 63 moons
42 MercuryLearn about the planet closest to the Sun
52 VenusExplore Earth's twin planet
64 EarthFind out more about our home planet
76 MarsCould there be life on Mars?
88 JupiterUncover amazing facts about this gas giant
100 SaturnRead about how Saturn's rings formedand much more
112 Uranus Explore the solar system's
forgotten planet
122 Neptune Discover all you need to know about thefrozen planet
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10 All about the Sun Explore the star keeps us all alive
22 Deadly solar ares A look at the Sun's deadly activity
28 The hole in the Sun Find out more about NASA's discovery
30 Solar maximum Read about the activity of the Sun
Discover the star at the centre of our Solar System
The Su
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“A solar flare is a suddenincrease in the brightness on
the surface of the Sun
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10
The Sun
1010
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The Sun
The vast nuclear furnace that we know as theSun is responsible for dictating the seasons
climate and characteristics of every planet inthe Solar System. Here, we take an in-depth
look at this source of power that has astoundehumanity since the dawn of existenc
THE
SUN
All About…
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The Sun
Layers of the Sun
Scutum-Centarus arm
The Sun
Outer arm
rion spur
Perseus arm
Our Solar System is located in the outerreaches of the Milky Way galaxy, which hasroughly 200 billion stars
SpiculesThese supersonic jets ofhot plasma form in theSun’s interior and rise to aheight of around 5,000km(3,000 miles) above theSun’s photosphere
Coronal mass
ejectionsA coronal mass ejection(CME) is a burst of plasmaand magnetic fields,known as stellar wind,being thrown into spacefrom the Sun’s corona
FaculaeProduced byconcentrations ofmagnetic field lines,these bright spotsappear on the Sun’schromosphere inregions where asunspot will form
GranulationThe Sunoften appearsgranulated inimages becauseof convectioncurrents in itsphotosphere andchromosphere
ProminencesThese large loopsof energy extendoutwards from theSun’s corona. Theycan range over700,000km(430,000 miles),approximately theradius of the Sun
SunspotThese dark spots on the surfaceof the Sun are caused by intensemagnetic fields and are usuallyaccompanied by a solar flare or CME
PhotosphereThe visible surface of theSun, the photosphere,has a temperature of5,530°C (9,980°F)and is made mostly ofconvection cells,giving it a granulatedappearance
ChromosphereThis thin layer about 2,000km(1,240 miles) thick sits just above thephotosphere and is the area wheresolar flares and sunspots are visible
Radiative zoneThis area is full of electromagnetic
radiation from the core that bouncesaround as photon waves. It makes up
about 45 per cent of the Sun
Inner coreMost of the Sun’s fusion poweris generated in the core, which
extends outwards from thecentre to about a quarter of the
Sun’s radius
CoronaThe outer
‘atmosphere’of the Sun.
It is madeof plasma,
extends
millions ofkilometres
outwards andhas a higher
temperaturethan the inner
photosphere
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14
The Sun
14
Like the Earth, the Sun has an atmosphere, but the two are very different. TheSun’s can be incredibly volatile with powerful magnetic activity that causesphenomena referred to as solar storms here on Earth
Solar storms are violent outbursts
of activity on the Sun that interfere
with the Earth’s magnetic field and
inundate our planet with particles.
They are the result of outpourings
of energy from the Sun, either in theform of a Coronal Mass Ejection (CME)
or a solar flare. The former is a release
of a large amount of material, mostly
plasma, from the Sun while the latter
is a sudden release of electromagnetic
radiation commonly associated with a
sunspot. While no direct connection
has been found between CMEs and
solar flares, both are responsible for
Solar stormscausing solar storms on Earth. The
reason why these two events occur
is due to the Sun’s atmosphere and
its turbulent interior, with all of its
components playing a part in bathing
our planet in bursts of energy.The lowest part of the atmosphere,
the part directly above the Sun’s
radiative zone, is the photosphere.
This is the visible part of the Sun that
we can see, it is 300400 kilometres
(180240 miles) thick and has a
temperature of about 5,530 degrees
Celsius (9,980 degrees Fahrenheit).
This produces a white glow although
from Earth this usually appears yellow
or orange due to our own atmosphere.
As you travel through the
photosphere away from the Sun’s
core the temperature begins to drop
and the gases become cooler, in turnemitting less light. This makes the
photosphere appear darker at its outer
edges and gives the Sun an apparently
clearly defined outer boundary,
although this is certainly not the case
as the atmosphere extends outwards
much further.
Once you pass through the
photosphere you enter the
chromosphere, which is about 2,000
kilometres (1,240 miles) thick. The
temperature rises to about 9,730
degrees Celsius (17,540 degrees
Fahrenheit), surpassing that of the
photosphere. The reason for this isthat the convection currents in the
underlying photosphere heat the
chromosphere above, producing shoc
waves that heat the surrounding
gas and send it flying out of the
chromosphere as tiny spikes of
supersonic plasma known as spicule
The final layer of the Sun’s
atmosphere is the corona. This huge
Solar wind and the Earth
Solar windAside from solar flares the Sunis continually emitting radiationand particles in all directions inthe form of solar wind
Solar flareThe formation of a pair of sunspotson the Sun’s surface creates amagnetic field line loop, which canin turn snap and send a violenteruption of material spewing out
MagnetosphereAs these particles travel towardsEarth they encounter themagnetosphere of our planet andtravel along the magnetic field lines
AuroraParticles from the Sun can exciteand heat particles at the poles ofEarth, forming fantastic displaysof light known as the auroraborealis and aurora australis in thnorth and south respectively
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16
The Sun
16
Our Sun may be a great distance away
but its f luctuations and perturbations
are still felt here on Earth.
Every 11 years the Sun moves from
a period of low activity, known as a
solar minimum, to a period of high
activity, known as a solar maximum,
and back again. When it is at itsmost active the Sun is even more
violent than usual, with a greater
number of sunspots appearing on
its surface and therefore more solar
flares emitted into space. During its
minimum point it is still a raging
inferno firing material into space but,
by comparison, it is much quieter
and sunspots, and therefore solar
storms, are rare.
Cycles are observed by monitoring
the frequency and position of
sunspots on the Sun. When the Sun
reaches the end of its cycle, new
sunspots will appear near the equator.The beginning of the next cycle
will see su nspots appear at higher
latitudes on the surface of the Sun.
Solar cycles have been observed for
centuries, but a standardised method
of counting them was not devised
until 1848 when Johann Rudolf Wolf
started counting sunspots on the solar
disk and calculated the Wolf number,
which is still u sed today to keep track
of the solar cycle. Cycles vary in their
intensity. From 1645 to 1715 there
were few sunspots present on the
Sun, a period known as the Maunder
Minimum. The number of sunspots
has been relatively more uniformthis century, with cycles having an
average period of 10.5 years. The Sun
also has a 22-year magnetic cycle
where, every 22 years, its magnetic
field flips from pole to pole. This
doesn’t have a noticeable effect on
the Solar System, but indicates when
the solar maximum of the current
cycle has been reached. However,
the reason for these cycles remains
a mystery. No one yet has any clear
understanding as to why the Sun has
periods of varying activity.
Our Sun is ever-changing,affecting all life on Earth andour natural environmentThe solar cycle
10 years of the SunThese X-ray images were taken by Japan’s
Yohkoh Solar Observatory and show the changesin the Sun’s corona over a ten-year cycle between
30 August 1991 and 6 September 2001
19911993At the start of this solarcycle there were about 200sunspots on the surface ofthe Sun per month
19941996As the Sun’s activity began towane, the number of sunspots pyear dropped from about 100 pmonth in 1994 to 75 in 1996
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The Sun
How we understand solar cycles“Sun-Earth interaction is complex, and we haven’t yet
discovered all the consequences of solar cycle variation
on Earth’s environment. We saw a large amount of
geomagnetic activity driven by recurring fast solar wind
streams during the recent solar minimum. A surprising
departure from the consistently low activity we’d come
to expect from previous minima, especially considering
the record low level of sunspots. These new observations
deepen our understanding of how solar quiet intervals
affect the Earth and how and why this might change
from cycle to cycle.”
The Scientist’s view
Solar cycles have been observed forcenturies, but a method of counting
them was not devised until 1848”
Sarah Gibson, UCAR, @AtmosNews
The Sun by
numbersFantastic figures and surprisingstatistics about our nearest star
The Sun’s percentage of massof the entire Solar System
99.86%
5%Lessthanof stars inthe Milky Way are brighter orlarger than the Sun
1
millionEarthsWould fit insidethe Sun
498second
How long it takes light to travel from the S
164 watts Is the amouof energy every squaremetre of the Earth’s surfareceives. That’s the equivaof a 150-watt table lamp every square metre of the Earth’s surface
100 BILLIONTons of dynamite wouldhave to be detonated everysecond to match the energproduced by the Sun
19992001The Sun’s activity increased againto a solar maximum, with up to 175sunspots appearing per month
19971998The Sun reachedits period of solar
minimum betweenthese years, fallingto almost zerosunspots per month
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18
The Sun
The Solar and Heliospheric Observatory was launched inDecember 1995 and is helping us explore the Sun
The Solar and Heliospheric
Observatory, also known as SOHO, was
launched on 2 December 1995. It was
built in Europe by pri me contractor
Matra Marconi Space, which is now
EADS Astrium. The spacecraft is
operated jointly by the ESA and NASA.
It studies the Sun in depth, all the way
from its deep core to its outer coronaand its solar wind.
SOHO is made of two modules,
the Service Module and the Payload
Module. The former provides SOHO
with power, while the latter houses all
of the instruments on the spacecraft.
Overall, there are 12 instruments on
board SOHO, nine of which a re run
by Europe a s well as t hree from t he
United States.
SOHO is located near to Lagrangian
point 1, which is a point between the
Earth and the Sun about 1.5 million
kilometres (930,000 miles) from
our planet. It is the point where thegravitational attraction of the Sun and
the Earth cancel out, so a telescope
such as SOHO can remain in a stable
orbit to observe the Sun. SOHO is
one of the only telescopes currently
capable of detecting incoming solar
flares that could be potentially
hazardous to satellites and other
electronics on Earth.
Of the 12 instruments on board
SOHO one of the most interesting is
the Large Angle and Spectrometric
Coronagraph (LASCO), which
studies the Sun’s corona bycreating an artificial solar eclipse.
The LASCO instrument has been
largely responsible for inadvertently
discovering many comets near the
Sun, with over 1,800 found to date.
SOHO has three primary objectives
that it has been carrying out since
its launch. One of these was to
investigate the outer regions of the
Sun, specifically the corona.
At the moment it is st ill u nknown
why the corona is hotter than the
photosphere and chromosphere of
the Sun, so it is hoped that SOHO
might help to provide the answer inthe future. SOHO has also been used
to observe the solar wind, and also
to study the interior structure of the
Sun through a process known
as helioseismology.
The SOHO mission
Take atour of
SOHOSOHO is made up
of two modules.The Service
Module formsthe lower portion,while the Payload
Module sits above
On the scale of solar flares, X-class storms are most powerful. SOHO took this image onNovember 2003 showing the most powerful ever recorded, which reached X28
Payload ModuleThis sits on top of the
Service Module and housesall 12 of the instruments on
board the spacecraft
Service ModuleThe Service Module
provides power,telecommunications,
thermal control anddirection to the spacecraft
MalfunctionIn 1998 SOHO suffered
a major malfunction thatalmost rendered it unusable.
However, some smartthinking enabled scientists
to regain control of thetelescope, although it nowoperates without the help
of its gyroscopes, theonly three-axis stabilised
spacecraft to do so
SOHOprojectscientistBernhard
Fleck tells us whystudying the Sun isimportant to Earth
Interview
1. Understand life“The Sun provides the energy for alllife on Earth. It seems quite naturalthat we are curious to know moreabout the star from which we live.”
2. Understand climate“Solar radiation is the dominantenergy input into the terrestrialecosystem. The Sun provides a
natural influence on the Earth’satmosphere and climate. Tounderstand mankind’s roles inclimate change, the Sun’s impactmust be understood.”
3. Predict space weather“Our Sun is very dynamic andproduces the largest eruptionsin the Solar System. These solarstorms can reach our planet andadversely affect technologies suchas satellites and power grids. Spaceweather becomes increasinglyimportant as our society dependsmore on modern technologies.”
4. Learn about stars“If we want to understand theuniverse, we have to understandthe evolution of galaxies. Tounderstand galaxies, we need tounderstand the evolution of starsthat make up the galaxies. If wewant to understand stars, we betterunderstand the Sun, the only starwe can resolve in great detail.”
5. Stellar physics lab“The Sun lets us study basic physicalplasma processes under conditionsthat can’t be reproduced on Earth.”
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The Sun
The SOHOspacecraft hassurvived 17years in space,15 more thanits initialmission length
“SOHO is located near to Lagrangian 1 which is a point between the Earth
and the Sun about 1.5 million km(930,000 miles) from our planet
LASCOSOHO’s Large Angle andSpectrometric Coronagraph(LASCO) produces detailedimagery of the solar corona bycreating an artificial eclipse
Solar panelsSOHO’s only source of energyis from the Sun, but as it is inorbit around it it has a large
supply of energy
AntennasSOHO transfers data back toEarth at a rate of between40Kbits/s and 200Kbits/s usinits high and low gain antennas
Solar and
HeliosphericObservatory (SOHO)
MissionProfile
Mission dates: 02/12/9512/12/14
Details: SOHO is a joint project
between the ESA and NASA. It
was designed to study t he origin
of the solar wind, the outer
atmosphere of the Sun and its
internal structure. SOHO has
found over 1,800 comets to date
and discovered that quakes on t
Sun’s surface are caused by solar
flares. It has also made the most
detailed map of features on the
solar surface.
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20
The Sun
Humanity has been fascinated by theSun for thousands of years and evenprimitive records still prove useful.Discover more about the past, presentand future of studying the SunObservations of the Sun have
been used for both scientific andreligious observations for millennia.
Civilisations have used the Sun
to keep an accurate count of days,
months and years since at least
300BC, while scientists such as Galileo
studied the Sun through telescopes to
discern some of its characteristics.
At the Chankillo archaeological site
in Peru can be found the oldest solar
observatory in the Americas, a group
of 2,300-year-old structures used to
track the motion of the Sun known
as the Thirteen Towers. These towers
provide a rudimentary solar calendar
through which the Sun can be traced.The towers, each between 75 and
125 square metres (807 and 1,345
square feet) in size, run from north
to west along a ridge along a low hill.
From an observation point to the west
of the ridge the Sun can be seen to
rise and set at different points along
the ridge, which allowed ancient
civilisations to track the number of
days it takes the Sun to move from
tower to tower.
Much later, in 1612, the renowned
Italian astronomer Galileo Galilei
(15641642) used his telescope to
make one of the first observations of
sunspots on the surface of the Sun. In1749 daily observations began at the
Zurich Observatory and, since 1849,
continuous observations have been
made to count the number of sunspots
“Civilisations have used theSun to keep an accurate
count of days, months andyears since at least 300BC
present on the Sun’s surface at any
one time.Fast forward to today and, aside
from SOHO, one of the primary
telescopes used to observe the sun
is the Japanese Hinode spacecraft.
Hinode is a telescope in sun-
synchronous Earth orbit, which allows
for nearly continuous observation
of the Sun. It was launched on 22
September 2006 and was initially
planned as a three-mission study of
the magnetic fields of the Sun, but its
mission has since been extended as it
continues to operate nominally.
Another important Sun-observ ing
telescope is the Solar DynamicsObservatory (SDO), launched by NASA
in 2010. The goal of the SDO is to
study the influence of the Sun near
Earth, predominantly how the Sun’s
magnetic field is responsible for the
solar wind once it is released into the
heliosphere. It should help scientists
further understand the Sun’s influence
on the Solar System.
In the future, NASA’s Solar Probe
Plus will be the closest spacecraft to
Observing
the Sunthe Sun, approaching to within just 8.5
solar radii (5.9 million km, 3.67 millionmiles, 0.04 AU) after its launch in
2018. It will probe the outer corona of
the Sun in unprecedented detail, while
also becoming the fastest spacecraft of
all time in the process at up to 200km
per second (120 miles per second).
Apart f rom million dollar telescopes,
many amateur astronomers around
the globe today observe the Sun either
for entertainment or educational
benefit. Using specially designed
glasses people can look at the Sun
from Earth, although caution must be
taken to limit time spent looking at
the Sun and it should never be lookedat with the naked eye. Other methods
of solar observation include using a
telescope to produce a trace of the
Sun, a method similar to that used b Aristotle and his ca mera obscura in
the 4th Century BC. Again, precautio
must be taken here, as under no
circumstances should the Sun be
directly observed through a telescop
Whatever the method, and whatev
the mission, observations of the Sun
have been a long tradition and will
continue to be so for the foreseeable
future. Astronomical events such as
planetary transits and solar eclipses
provide amateur astronomers with
opportunities to see extraordinary
solar phenomena, while agencies
throughout the world will continue tstudy the Sun and learn more about
how the fantastic star works.
The history ofobserving the Sun
400BCThe world’s oldest solarobservatory, the Thirteen Towersof Chankillo, is built in Peru totrack the motion of the Sun.
350BCAristotle uses a cameraobscura to project animage of the Sun andobserve a partial eclipse.
1612Galileo Galilei uses histelescope to make one of thefirst observations of sunspotson the surface of the Sun.
Solar eclipses are apopular time to view theSun but using the correct
viewing equipment is veryimportant for safety
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The Sun
1749Daily observations of theSun begin at the ZurichObservatory in Switzerland.
1849New observatoriesaround the world allowcontinuous observationsof sunspots to be made.
2006The Japanese telescopeHinode is launched to studythe magnetic fields andatmosphere of the Sun.
2010NASA launches the SolarDynamics Observatory, itsprimary goal being to study theinfluence of the Sun near Earth.
2018NASA’s new Sun-observitelescope Solar Probe Pllaunch and become the cspacecraft to the Sun.
Different ways toobserve the SunOn Earth we perceive the Sun to
be a yellow ball of gas in the sky but, like anything as hot as the
Sun, it is actually closer to being
white hot when viewed from
space. There are several telescopes
currently observing the Sun but
the large majority of our images com
from the STEREO telescope andthe SOHO observatory, both in orbit
around the Sun. By viewing the Sun
different wavelengths we can study i
different characteristics and see som
of its main features in a different ligh
UltravioletImages of the Sun in ultraviolet light arebetween wavelengths of about 19.5 and 30.4nanometres. Such an image of the Sun is at thelower end of this scale, and allows us to seewhere the lower part of the corona and upperpart of the chromosphere combine. The lightin this image comes from active regions in theSun’s chromosphere.
X-rayLight with a wavelength shorter than tennanometres (ten billionths of a metre) is knownas X-ray light. X-rays are emitted from the Sun’scorona, the hottest visible layer of the Sun’satmosphere. The visible areas of brightness areplaces where more X-rays are being emitted,around areas of increased activity on theSun’s surface.
VisibleVisible light images commonly refer to thoseviewing the Sun in white light, which showsthe true colour of the white-hot Sun. In visiblelight images we can see the Sun’s photosphere,which is about 6,000 degrees Celsius (10,832degree Fahrenheit) and therefore appearswhite-hot. Here, we can see dark spots on thesurface of the Sun, known as sunspots.
InfraredInfrared light is responsible for more thanhalf of the Sun’s power output, typicallyaround wavelengths of 1,080 nanometres.Infrared images show features of the Sun’schromosphere and corona. The dark featureson the image are areas where the gas is moredense, absorbing more infrared light than inother areas.
A telescope witha digital screencan be used tosafely observethe Sun
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22
The Sun
What would become of the Earth if a large solar storm was directed our way,and would we be able to survive such an event? We take a look at how theSun’s activity has threatened life on Earth before, and how it might again
SOLAR FLARESDEADL
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Deadly solar flare
The Earth is under constant threat from a whole
host of things in space, from asteroids to comets.
However, the one thing that is essential to life on
our planet, the Sun, may also be the most dangerous
threat of all to life as we know it. “[A large solar
flare] would certainly have a widespread ubiquitous
footprint all the way around the world,” said JoeKunches from the National Oceanic and Atmospheric
Administration’s (NOAA) Space Weather P rediction
Center (SWPC), which provides solar weather
forecasts to satellite operators and agencies across the
globe. “The question is, how deep would the effects
be, and how long would it take to recover from that?”
The Sun is a volatile and dangerous ball of gas
that, while it is the heart of our Solar System, also
has the potential to wreak havoc on not only our
world but the other planets and moons as well. It is a
constantly churning furnace of energy that releases
radiation into its surroundings. As our closest star it
is the perfect laboratory to observe how such stars
behave, and indeed we have been studying the Sun
for centuries to try to further our understanding of it.
While the Sun is constantly emitting energy andradiation, it goes through a period of cycles that tend
to govern how active it is at any given time. The
solar magnetic activity cycle has a period of 11 years,
and at its peak it significantly increases detectable
changes and emissions from the Sun including
sunspots and solar flares. It is at these times, during
a solar maximum, that the Earth’s infrastructure
is under greatest threat. In the last few decades
organisations like the SWPC have used a multitude of
observatories both in space and on Earth to monitor
these cycles and to predict when a large solar event
could endanger our planet.
“There have been plenty of cases of serious
damage to satellites,” said Kunches. “It happens
mostly when the Sun is active and very eruptive atthe peak of the solar cycle, and right now we’re at the
peak of the current solar cycle, although this one has
been pretty uneventful.” However, based on previous
experiences, Kunches knows that the SWPC cannot
take anything for granted. “During the last solar
maximum era, around Halloween in 2003, there was
a two-week episode of very turbulent space weather
conditions,” he said. “There were documented cases
of satellite failures, and some total failures.”
A solar flare is a sudden increase i n brightness
on the surface of the Sun. It occurs when built-up
magnetic energy in the solar atmosphere is released,
resulting in a huge emission of energy equivalent to
millions of 100-megaton nuclear bombs exploding
simultaneously. This energy is usually the result ofclosely occurring loops of magnetic force extending
out from the Sun’s surface and, if they ‘snap’, a burst
of solar wind combined with magnetic fields known
as coronal mass ejections (CME) will be emitted. A
solar flare itself is an ejection of clouds of electrons,
ions and atoms, with a CME usually following the
flare. Solar flares and CMEs both usually result
from the collapse of magnetic field loops, but the
relationship between the two is not fully understoo
The breaking of a magnetic field loop is usually
indicated by the appearance of sunspots, visibly
dark areas on the Sun occurring in pairs. The reason
for 11-year solar cycles, when these emission events
increase, is still under debate.
The study and detection of these solar phenomenhas been carried out for decades by various
observatories and telescopes. These include the
space-based Solar Dynamics Observatory (SDO) and
the Solar and Heliospheric Observatory (SOHO), the
InsideSDOThere are a multitude of
telescopes and observatori
constantly observing the
Sun, but NASA’s Solar
Dynamics Observatory
(SDO) is currently able toget some of the highest-
resolution images of our
Solar System’s central star
from its orbit around the
Earth. Launched on 11
February 2010, the SDO’s
main goal is to understand
the influence of the Sun
on Earth and surrounding
space by measuring in
several wavelengths
simultaneously.
MassAt launch the SDOweighed 3,100kg(6,800lb), withthe instrumentsweighing 300kg(660lb), thespacecraft itself1,400kg (3,090lb)and the fuel1,400kg (3,090lb)
Extreme UltravioletVariability Experiment (EVE)EVE measures the extreme ultraviolet emissionof the Sun to understand the relationshipbetween its ultraviolet and magnetic variations
Solar arraysThe solar panelsspan 6.25m(20.5ft) andsupply 1,540watts of powerto the SDO at anefficiency of 16%
Helioseismicand MagneticImager (HMI)
The HMI producesdata that helps to
determine howactivity inside
the Sun producesvisible effects on
its surface
Atmospheric ImagingAssembly (AIA)The AIA allows for continualobservations of the entireSun in seven extremeultraviolet channels from atemperature of 20,000 to20 million Kelvin
“We rely on infrastructure that is knownto have sensitivities to space weather”
Joe Kunches, far right, is part of the SWPCteam that provides space weather forecasts
for satellite operators around the world
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24
The Sun
It takes about 60 hours for theEarth to feel the effects of asolar flare or CME
former run by NASA and the latter run jointly by ES
and NASA. “In the satellite world there are at least te
spacecraft that provide real-time information to the
SWPC,” said Kunches. “Then in addition to that ther
are ground-based observatories, and also ground-
based sensors like mag netometers. If you put a roun
number on it there would be about 50 to 100 senso
contributing to the real-time information stream tha
we tap into here.”
The work of the SWPC, and other similar
organisations, is hugely important in protecting
ourselves from the Sun. Although predicting the
occurrence of world-changing solar events is
important, it is largely everyday satellite operators
that rely most on the solar weather predictionorganisations in ensuring that their spacecraft rema
operational and continue to provide the service the
are intended to. They use regular bulletins from
places like the SWPC to know when to prepare for
a solar event. However, contrary to popular belief,
satellites are not shut down if a solar storm is
incoming because the danger of a satellite failing if
is turned off and on is fairly high. Some instrument
can be turned off and ground teams can prepare for
the worst but, as Kunches put it, “you can’t run and
you can’t hide.”
The SWPC is able to produce accurate forecasts fo
up to the next 27 days detailing what sort of activity
the Sun is expected to go through. If a solar flare or
CME is seen by one of the many active telescopes,
it takes about 60 hours for the Earth to feel theeffects of such an event. However, as Kunches
explained, just detecting the event is not enough.
The SWPC must track the emission as it makes its
way towards Earth to discern when it will arrive an
how powerful it will be, with the latter known as th
magnitude. “Ten years ago we could get the timing
down to plus or minus 12 hours,” said Kunches. “No
we’ve cut that in half, but it’s not easy being accurat
It’s 150 million kilometres (93 million miles) from th
Sun to the Earth and a lot can happen in-between.”
While working out the timing of an incoming
solar flare is becoming more accurate, it is the size
of such an event that proves the most troublesome.
Inside asolar flare
ProminenceA loop of plasmaextends fromthe Sun’s surfaceinto its hot outeratmosphereduring a solarflare event
Magnetic fieldThe prominence has twocontact points with the Sunas it flows along the magneticfields created inside the Sun
CharacteristicsA coronal mass ejection(CME) usually followsa flare, containing abillion tons of matter andtravelling at millions of
kilometres per hour
RadiationThe flare releasesradiation acrossthe entireelectromagneticspectrum, from radiowaves to X-rays
TemperatureInside a solar flare thetemperature can reachanywhere from 10 milliondegrees Kelvin to 100million degrees Kelvin
The SWPC is one of nineNational Centers forEnvironmental Prediction, but the only one dedicated tospace weather forecasting
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Whathappenswhen
a solarflare hitsEarth?
ObserversA variety ofobservational spacecrincluding the SDO,STEREO and SOHO areused to predict whenthe Sun will erupt andhow powerful theeruption will be
SpacecraftelectronicsHard X-rays from anincoming solar flare candamage the internalelectronics of spacecraftand prevent instrumentsfrom working
Telephone mastEven cell phones are not adverseto the effects of solar flares, asthe increased activity can preventdevices communicating withtelephone masts
GPS failureIncreased solar activity can prevent GPSnavigation satellites operating functionallyand, as most are in a similar orbit, one is notable to provide backup for another
PipelinesTelluric currents, thosefound in long pipelines,can be affected by solarflares when systemsdesigned to protect pipelines
from corrosion areoverloaded
AircraftIn the event of increased solaractivity aircraft must avoidflying near the poles and athigh latitudes to ensure thatcommunications aren’t affecte
AtmosphereSoft X-rays from X-class flarescan increase the ionisation ofthe atmosphere so that, whileit might produce fantasticauroras, it also interferes withradio communication
Orbital decayIncreased ionisation ofthe atmosphere causedby solar storms canincrease the drag onsatellites, decaying theirorbit, as was the casewith NASA’s Skylabspace station in 1979
Power gridIncreased solar activity cancause geomagnetic storms,which have been known toknock out power grids toentire cities in the past
International Space StationRadiation risks for astronauts onthe ISS are minimal, but for futureastronauts travelling to deep spacelocations like Mars they could bemore severe
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26
The SunThe Sun
How asolar flareinteracts
with Earth
EmissionA solar flare sendsa stream of chargedparticles and radiationtowards Earth
“The hardest thing for us to predict is the magnitude,”
said Kunches. “There’s a key element that plays into
the magnitude, how disturbed the Earth’s magnetic
field is going to get, and that’s the strength of the
embedded magnetic field that’s contained within the
CME. Think of a hurricane; if the weather forecasters
knew the direction of it, and they had some sense of
how fast it was moving, but they had no idea of the
strength of the eye of the storm, it’d be very difficult
to know how much of an impact it was going to have
as it made landfall, and that’s kind of analogous to
what we have in space weather forecasting.”
Solar flares are classified in magnitude according
to the number of watts per square metre they carry,
and their frequency. A-class flares are the most
frequent and the least powerful, increasing in powerthrough B, C, M and finally X. The latter are the ones
that are the most dangerous to Earth. The magnitude
of a solar storm will determine how much of an
impact it will have on Earth.
The largest recorded geomagnetic solar storm
caused by a solar flare was the Carrington Event
in 1859. Observed by British astronomer Richard
Carrington, the storm was noticeable around
the world. Auroras reached as far south as the
Caribbean, while it was reported that residents of the
northeastern US could read a book by the light of the
aurora. Of most concern, however, was that telegraph
offices all over Europe and North America failed,
with some throwing sparks or catching fire. This led
to much speculation about the effects a similar stor
would have in the modern world, where electronics
are a much more integral part of our lives.
In March 1989 that question was answered when
large CME coupled with a solar flare caused a sever
geomagnetic storm on Earth. Although it temporari
knocked out some satellites and spacecraft, the wor
effects of the storm were felt in Québec, Canada.
The variations in the Earth’s magnetic field, coupled
with Québec’s location on a large rock shield that
prevented the flow of current through the Earth,
tripped the circuit breakers in the power grid of the
Hydro-Québec power station and knocked the statio
offline, sending 6 million people into a blackout
lasting nine hours.The geomagnetic storm of 1989 served as a
reminder that solar flares can cause widespread
damage, and since then numerous power stations
have taken measures to ensure such an event does
not occur again. “In the past few decades, the grid
has undergone major changes to make it more robu
and better able to neutralise the geomagnetic effect
of solar storms,” a spokeswoman for the Hydro-
Québec power station told us. “Since 1989, solar
activity has not disrupted the performance of Hydr
Québec’s transmission system.”
That, however, does not mean we are safe from
a future huge outburst from the Sun. “We are so
“Right now we’re at the peakof the current solar cycle,although this one has beenpretty uneventful”Joe Kunches, Space Weather Prediction Center
Classifying solarradiation storms
Minor
50 per 11-year solar cycle
25 per cycle
10 per cycle
3 per cycle
Less than 1 per cycle
Moderate
Strong
Severe
Extreme
A minor solar radiation storm causesminimal impact on high-frequency (HF)
radio in the polar regions, but otherwisecauses no damaging effects.
A moderate storm affects navigation at thepolar caps and may, in rare instances, causeproblems in satellites, but poses no threatto humans.
During a strong storm astronauts areadvised to seek shelter, while satellitescould lose power and instrument usage. HFradio will degrade at the poles.
Astronauts and passengers on planes maybe exposed to radiation, while satellitescould experience orientation problems. HFradio blackout at the poles.
Astronauts and aeroplane passengersexposed to high radiation. Satellites maybe rendered useless. HF communicationsblackout in polar regions.
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The Sun
MagnetosphereThe magnetic field lines ofthe Earth’s magnetosphere
divert most of the solarwind around the Earth
InteractionThe incoming sola
particles excitethose in our ownatmosphere, causiauroras at the pole
IonisationThe incoming particles canalso ionise the atmosphere,which can have hazardouseffects on satellites,communications and more
TrappedSome of the chargedparticles are trapped
and guided by theEarth’s magnetic field
Solar space observatories
SOHOThe Solar and Heliospheric Observatory (SOHO)
launched on 2 December 1995 to observe the Sun
from a position between the Earth and the Sun, the
L1 Lagrange point, and it continues to operate today.
A joint project between ESA and NASA, it is currently
the main source of data for space weather predictors.
ACENASA’s Advanced Composition Explorer (ACE) has
been in space since 2 5 August 1997, with its main
goal being to study the composition of solar wind.
Like SOHO it is located at L1, and it is expected to
continue operations until around 2024 when its fuel
will be depleted.
STEREOThese twin spacecraft, known as the Solar
Terrestrial Relations Observatory (STEREO),
launched on 26 October 2006 and, through
their respective solar orbits, they are able to get
stereoscopic images of the entire Sun. This has
proven useful for detecting solar flares.
way to deflect solar flares and not much we can do
a particularly powerful one interacts with the Earth
While we can estimate when a storm will arrive,
determining its power as it travels from the Sun to
the Earth will be of most importance for the future
of predicting solar storms in order to try to minimis
the effects of a large solar flare. “The next big step t
be taken is in the science to better understand the
information that’s available to us now,” said Kunche
“I think that’s the challenge of the next generationof space scientists, to try and understand better tha
we do now which of all the remarkable features we
see back at the Sun are going to be the ones that
really impact the systems we depend on.”
reliant on satellite-based technology, like GPS-based
applications, and you look at them and they’re all
very similar,” Kunches said. “One really couldn’t be a
backup for a nother because they all f ly at about the
same orbits. And then you get to the electrical power
grids and how interconnected they are, and if you
get induced currents that cause transformers to be
damaged and the ripple effects from those could be
quite strong. We rely on infrastructure that is known
to have sensitivities to space weather.” And while the general public may not have much
of an interest in space weather, a large solar storm
would certainly be noticeable to the layman on
Earth. “I think everyone would agree that if you had
a Carrington-like event there’s no doubt that normal
citizens, who have no awareness of space weather
and really don’t care about it, would wake up in
the morning and they would see that something
is different,” said Kunches. “They would find that
something, be it their electricity or their television or
their cell phone, is not available as they wish it to be.”
With space weather prediction agencies like the
SWPC we are able to prepare for the worst when
it comes to solar storms but, ultimately, if a hugeemission event were to occur we don’t have much
of a defence. In extreme cases we can power down
equipment, and prepare our electronic infrastructure
to deal with an increase in energy, but there is no
Deadly solar flare
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The Sun
28
The Sun
NASA spots an enormous coronal hole opening upand expanding above the surface of the SunThis image was taken by NASA’s Solar Dynamics
Observatory in mid-June last year. It shows the
electromagnetic activity of the Sun in extreme ultraviolet,
with the colder regions in blue. There’s a remarkabledifference between the hot, dense atmosphere in the
southern hemisphere and the north, which is considerably
cooler. This is because a huge coronal hole has opened
up in the Sun’s atmosphere, around 650,000 kilometres
(400,000 miles) in diameter, or the distance of more than
50 Earths wide.
In this region, solar winds can emerge at furious
velocities, typica lly up to around 800 kilometres per
second (500 miles per second), which is about twice the
speed of solar winds in the regions where the coronal hole
isn’t present. It kicks up a hell of a lot of dust in its wake
too, carrying material from the Sun far out into the Solar
System in every direction.
The holein the Sun As d ramatic as this sounds, coronal holes are actually
a regular part of the Sun’s 11-year cycle, growing larger
and moving closer to the poles the nearer to the solar
maximum we get. The most recent solar maximumoccurred towards the end of 2013, when we saw such huge
coronal holes converging.
During this peak, the Sun’s increase in activity
can affect normal weather patterns on Earth,
telecommunications can be disrupted and solar flares
can get particularly large. In addition, early in 2014 the
Sun’s magnetic field weakened to zero and then flipped,
with mag netic north becoming ma gnetic south and
vice versa , creating solar storms. Incredibly, a huge
solar storm during the maximum of 1859 resulted in the
aurora borealis stretching way beyond its normal limits,
and for a period could be seen as far south as Italy and
the Caribbean.
The Sun, shot in UV in 2010, several years earlier in itscycle and showing no substantial coronal hole
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The hole in the
As it approaches solar maximum, the Sunmagnetic field is about to completely fl
while a huge coronal hole (the big blue patcopens up in its northern hemisphe
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The Sun
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Our local star might seem to be an unchanging ball of blazing light, but in reality its uppe
layers are seething with extreme activitythat varies in a period of around 11 years, and
whose influence reaches as far as Earth
Solar maximum
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“There is acuriosity that is
part of humannature thatmakes us wantto understandhow the Sunand otherstars work”Dr Giuliana de Toma
The Sun is the dominant force
shaping conditions on Earth and
throughout our Solar System – a
brilliant ball of gas powered by
nuclear fusion in its core, whose
influence reaches out across billions
of kilometres. Radiation at both visibleand invisible wavelengths provides
heat and light to the planets, and from
the point of view of a casual observer,
seems more or less constant –
certainly seasonal changes as a planet
moves around its orbit and changes its
orientation and distance from the Sun
have a far greater influence over its
climate than any slight fluctuations in
the Sun’s behaviour.
But nevertheless, these changes
are real – and while they do little
to change the Sun’s heating effect
on Earth, they can be spectacularly
violent in other ways, threatening
orbiting satellites, distant spaceprobes and even reaching down to
the surface of the Earth itself. The
Sun is unpredictable and can produce
extreme outbursts at any time, but in
general, the frequency and intensity
of these events varies in a ‘solar cycle’
of around 11 years. The cycle, as we
shall see, is fundamentally driven
by the Sun’s changing magnetic
field and, through improving their
understanding of it, astronomers hope
to learn more about the deep structure
of all stars.
Dr Giuliana de Toma, a solar
physicist at the National Centerfor Atmospheric Research (NCAR)
in Boulder, Colorado, has made a
career of studying the Sun’s cyclical
behaviour. She puts it this way:
“There is a curiosity that is part of
human nature that makes us want to
understand how the Sun and other
stars work. The Sun is a very special
star, not only because the life on Earth
depends on it, but because the Sun is
the only star that we can observe in
detail. What makes the Sun (and other
active stars) very interesting is the
presence of a magnetic field. One of
the great challenges in solar physics is
to understand, and ultimately predict,
solar magnetic activity.”The solar cycle was first identified
in 1843 by German astronomer
Heinrich Schwabe – the result of a
17-year project to map the number and
size of dark spots on the bright disc
of the Sun. A few years later, Swiss
astronomer Rudolf Wolf used historical
records of these dark sunspots to
trace Schwabe’s cycle back as far as
1745, confirming a period of around 11
years with distinct peaks in sunspot
numbers (solar maxima) separated by
intervening minima.
While it may appear superficially
solid, the Sun’s visible surface, or
photosphere, is in fact a layer a fewhundred kilometres deep marking the
region where the Sun’s gases finally
become transparent a nd allow l ight
and other radiations to escape into
space – temperatures in this region
average approximately 5,500 degrees
Celsius (9,930 degrees Fahrenheit),
but sunspot regions are up to 2,000
degrees Celsius (3,630 degrees
Fahrenheit) cooler, and so appear dark
in comparison.
“Sunspots are regions of strong
magnetic fields that appear dark when
the Sun is observed in visible light,”
says Dr de Toma. “At solar maximumsunspots are more numerous than
at solar minimum. Larger and more
complex sunspots are more commonly
seen near solar maximum.”
But while you might think that
dark spots on the Sun’s surface would
cause its overall energy output to
fall, the opposite is actually the case:
“The Sun’s radiative output peaks at
solar maximum. This seems counter-
The violent SunThe terms solar flare and coronal
mass ejection (CME) are often used
interchangeably, but in reality
they refer to distinctly separate
phenomena. A flare is a huge release
of energy created when magnetic
field lines looping through the solar
corona reconnect or ‘short-circuit’at a lower level. The event heats the
surrounding electrically charged
plasma up to 10 to 20 million degrees
Celsius (18 to 36 million degrees
Fahrenheit) causing it to emit intense
radiation across the electromagnetic
spectrum, and also accelerating
subatomic particles such as protons
and electrons to speeds close to that
of light. These particles escape the
Sun still travelling at tremendous
speed, and give rise to ‘radiation
storms’ as they pass the planets.
Hot spotsPlages and faculae are
bright, hot regions causedby concentrations of
magnetic field around theedge of emerging sunspots
Cutting looseThe CME is preceded by a
magnetic reconnection eventin which the loop of magnetic
field short-circuits closer tothe solar surface, leaving its
upper regions isolated
Rapid expansionFreed from their magnetic
ties to the Sun, gasesin the filament expand
rapidly, blowing outacross the Solar System at
hundreds or thousands ofkilometres per second
While flares have been studied
for over 150 years, CMEs were first
conclusively detected in 1971. They
are usually associated with flares, an
are thought to be generated when
loops of magnetic field ‘cut loose’
by a magnetic reconnect ion, and
the filament material within them,expand violently outwards. CMEs
form billowing clouds of relatively
dense material within the general
‘solar wind’ of particles flowing
out from the Sun, but compared
to radiation storms they travel at
comparatively sedate speeds of a few
hundred kilometres per second. As
a result, they may take days to reach
Earth, but when they do, the magne
field still carried within them can
interact with Earth’s own magnetism
to cause major geomagnetic storms.
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The Sun’s magnetic fieldThe Sun’s magnetic field is believed
to form beneath its visible surface
– specifically in the ‘convective
zone’ extending down to about 0.7
solar radii, where bulk movements
of charged gas bring heat to the
surface. Details of this mechanism,
known as the solar dynamo, are not
certain, but at the start of a cycle it is
capable of generating a fairly orderly
magnetic field whose poles roughly
align to the Sun’s axis of rotation.
Over time, though, the solar interior
experiences ‘differential rotation’,with equatorial regions rotating faster
than high latitudes. As a result, the
magnetic field becomes distorted,
and interactions between different
regions force magnetic loops, the
focus of sunspots and flares, out of
the surface. As the cycle progresses,
some of the magnetic field starts to
cancel out across the equator, while
part is carried towards the poles
where it plays a role in reversing the
magnetic field for the next cycle.
N
S
N
S
N
S
Active centresAs the magnetic field becomes morecomplex, neighbouring field lines startto interact and magnetic loops arepushed out of the photosphere, whilethe overall dipole field becomes weakand more complex.
Differential twistingEquatorial regions of the Sun completeone rotation every 25 days, whilethose at high latitudes may take 30days or more. This differential rotationgradually pulls the Sun’s magnetic fieldout of shape.
TIME TIME
Orderly fieldAt the beginning of a solar cycle, theSun’s magnetic field has a clear andfairly orderly ‘dipole’ arrangement,with magnetic field lines entering andemerging from the Sun’s visible surfaceat high latitudes.
Filament structureCMEs often begin life asfilaments – regions ofrelatively dense gas thatarc along loops of magneticfield in the corona
Magnetic rootsSites where the magnetic field
emerges from and re-entersthe Sun’s visible surface are
marked by sunspots (unseen atthis wavelength)
Solar maximumSolar maximum
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Effectson Earth
AurorasBrilliant northern and southern lightscovered the sky at high latitudes,making the night appear brighterthan a full Moon. Aurorae werevisible across the planet, almostdown to equatorial latitudes
SatellitesA variety of orbiting spacecraft wereaffected, as the storm blocked contact witgeostationary weather satellites for severahours. At lower altitudes, the Space ShuttDiscovery and other satellites reportedfaults and anomalies
Telegraph polesElectric currents induced in overhead wiresgave some telegraph operators electric shocks,while telegraph pylons threw sparks
Ground systemsElectric power networks were not yetin use, but flowing currents in telegraphwires caused some systems to continuesending and receiving signals evenwhen they were switched off
The stormAn enormous CME associated with the Carrington Event created a geomagneticstorm as it swept past Earth, creating strong electromagnetic fields and pushinghuge numbers of particles out of Earth’s radiation belts into the upper atmosphere.
The stormThe CME which caused the 1989 storm wareleased from the Sun on 10 March, a fewdays after a major flare. The storm passed
Earth on 13 March, causing aurorae thatcould be seen as far south as Florida
intuitive, but sunspots are surrounded
by bright features called faculae and
plages that make the Sun brighter at
solar maximum.”
Another aspect of the su nspot cycle,
meanwhile, gives rise to one of the
most iconic diagrams in all of science.
By recording not just the number
and size of sunspots, but also their
latitude on the surface of the Sun,
English astronomer Edward Maunder
discovered a steady drift in latitude
throughout each cycle, with spots first
appearing in small numbers at high
latitudes in each hemisphere, peaking
around mid-latitudes, and dying away
as the remaining spots converged on
the equator. The beautiful symmetric
pattern produced when sunspot
latitudes over a full solar cycle or more
are plotted on a graph is known as a
‘butterfly diagram’.
While sunspot activity is by
far the most obvious indication
of the solar cycle at work, it is far
from being the only one. Since the
beginning of the space age, new
technologies for studying the Sun at
invisible, high-energy wavelengths
such as the ultraviolet and X-rays
have revealed far more spectacular
outbursts that are also linked to
the cycle. “The magnitude of the
solar radiative variation over a solar
cycle is a function of wavelength. In
visible light, the change is very small,
but it is much larger in the shorter
wavelengths of ultraviolet and X-ray
radiation,” outlines Dr de Toma.
Much of this higher-energy radiati
is associated with solar flares – sudde
brightenings of the Sun’s sur face tha
typically last for just a few minutes
but can release enormous amounts
of energy – equivalent to a billion
megatons of TNT. They occur in the
solar corona – the Sun’s thin outer
atmosphere where gas is far more
tenuous than at the photosphere, but
temperatures can soar up to 2 million
degrees Celsius (3.6 million degrees
Fahrenheit), and are often seen
1859
1989
UtilitiesFluctuations in Earth’smagnetic field induced electriccurrents in the crust, which inturn tripped circuit breakersand caused blackouts inQuébec and elsewhere
How solar storms have affected ourevolving technology across history
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Ground systemsBeneath Earth’s protectiveatmosphere, ground-based electroniare mostly protected, and vital systemin aircraft and cars also have robustdesigns. However, power networks,by their nature, remain vulnerable topower fluctuations and surges
Hydro-Québec power gridThis major electricity network
covering much of eastern Canadasuffered a complete blackout
and could not be restarted fornine hours. It was particularly
vulnerable due to local geologyand the length of its power lines
ISSAstronauts on the InternationalSpace Station can expect to seetechnical glitches and anomaloureadings, but should be shieldefrom the worst of the radiation,since they are well within Earthmagnetic field
above active sunspot regions. Flares,
too, are thought to be connected to
changes in the Sun’s magnetic field,
specifically ‘reconnection events’ in
which a loop of magnetic field arcing
high into the corona ‘short-circuits’ at
a lower level to release an enormous
amount of energy and a burst of high-
energy radiation. Flares are also often
associated with huge releases of high-
speed subatomic particles known as
coronal mass ejections (CMEs – see
‘Solar flares vs coronal mass ejections’
boxout on page ww). Travelling at
millions of kilometres per hour, the
particles from a CME can reach Earth
within a couple of days.
19th Century scientists puzzled for
some time over the cause of the solar
cycle, but a key breakthrough came
in 1908, when US astronomer George
Ellery Hale made the link between
sunspots and powerful magnetic
fields. Since the Fifties, this has given
rise to a ‘solar dynamo’ theory that
describes how the Sun’s initially
smooth magnetic field, deep beneath
the visible surface, becomes twisted
during each solar cycle by its fluid
rotation, and eventually gives rise to
magnetic loops that push out throug
the photosphere and are associated
with sunspots, flares and other kinds
of activity (see ‘The Sun’s magnetic
The stormWe can expect any future geomagnetic storm to be preceded by one or morepowerful solar flares. Spacecraft such as NASA’s STEREO probes, viewing the Sunfrom different angles, should give a few days’ warning that a CME is on its way.
2014
SatellitesSince the 1989 storm, many lessons
have been learned about satellite design.Electronics are typically ‘radiation
hardened’ to reduce short circuits causedby particle strikes, but some satellites may
have to be shut down and restarted
” A direct hit by a powerful CME can causesignificant disruption to our planet’smagnetic field”
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field’ boxout on page 33). By the end
of the 11-year cycle, the Sun’s magnetic
field has been converted back to a
simple ‘dipole’ arrangement, but with
its north and south poles reversed, and
the cycle begins again.
However, a detailed understandingof the dynamo remains elusive,
since it relies on an accurate model
of the Sun’s interior. Such models
have only become possible in recent
years thanks to developments in the
field of helioseismology (using sound
waves on the Sun’s surface to map its
structure, just as geologists use seismic
waves to explore our own planet’s
inner layers) and, as a result, many
questions remain unanswered.
A direct hit by a powerful CME ca n
cause significant disruption to our
planet’s magnetic field. This kind of
event, known as a geomagnetic storm,
can send particles pouring into Earth’supper atmosphere where they cause
stunning displays of aurorae (northern
and southern lights). However,
the combination of high-energy
radiation and energetic particles can
also have more serious effects for
modern civilisation, affecting orbiting
spacecraft and even ground-based
power networks.
Perhaps the most famous
geomagnetic storm is the ‘Carrington
Event’ of 1859, associated with a
brilliant flare f irst spotted by Engl ish
astronomer Richard Carrington
on 1 September 1859. The ensuingcoronal mass ejection, travelling at
tremendous speed, reached the Earth
barely a day later, trig gering northern
lights that were visible as far south
as the Caribbean, and bright enough
for people at higher latitudes to read
newspapers in the middle of the
night. As the Earth’s magnetic field
warped under the onslaught, telegraph
systems around the world went
haywire as they were overloaded with
unexpected electric currents.
While both flares and CMEs can
occur throughout the solar cycle,
their frequency and average strength
rises significantly around the solarmaximum (the Carrington Event, for
instance, is acknowledged as the peak
of ‘Solar Cycle 10’). Despite the energies
A history of solar activityTracking solar activity prior to the
last couple of centuries is difficult.
Even after the invention of the
telescope, sunspot records were
patchy at first. Ironically, when
astronomers did begin to collect
consistent observations, it was during
the Maunder Minimum period of thelate 17th Century, when spots were
notably reduced. Long-term rises and
falls in solar activity are known as
grand maxima and grand minima –
the Maunder Minimum was followed
by a spike in activity duri ng the 18th
Century, and the short, sharp Dalton
Minimum between 1790 and 1830.
From 1900 to the present, activity
has been high, during a period called
the Modern Maximum that was at its
most intense in the late 20th Century.
Before 1610, solar activity is even
harder to track directly, since only
the very largest sunspot groups were
seen or recorded with the naked eye.
However in 1976, US astronomer
Jack Eddy demonstrated a direct
link between solar activity and the
quantity of radioactive carbon-14 in
Earth’s atmosphere. Since carbon-14 is
preserved in ancient tree rings, it can
be used as a proxy for solar activity,and studies using this method have
revealed a Medieval Maximum
around 1100 to 1250, bracketed by the
Oort Minimum in the 11th Century,
and the Wolf Minimum from around
1280 to 1340. Intriguingly, just as the
Maunder Minimum seems to coincide
with the ‘Little Ice Age’ across Europe
and North America, the Medieval
Maximum also coincides with a
period of mild North Atlantic climate
known as the Medieval Warm Period.
Could a decline from the current
Modern Maximum lead to another fall
in temperatures?
Maunder MinimumDuring the deepest part of theMaunder Minimum in the late 17thCentury, almost no sunspots wereseen, despite careful studies byexperienced observers such asGian Domenico Cassini.
Dalton MinimumThe Dalton Minimum, between around 1790 and
1830, was a relatively brief period of depressedsolar activity. Global temperatures at the time were
also cooler, but this may have been coincidental.
Modern MaximumThe Modern Maximumbegan around 1914and lasted throughoutthe rest of the 20thCentury, with peaks inthe Fifties and Nineties.The subdued activityseen in the currentSolar Cycle 24 may bea sign that it has nowcome to an end.
involved, Dr de Toma points out that
the total solar irradiance (TSI) – the
amount of solar radiative energy that
reaches the Earth’s upper atmospher
– varies by just 0.1 per cent over a so
cycle, but recent research has shown
that within this overall pattern, solaroutput at different wavelengths can
vary by much greater amounts.
Not all cycles are the same, and
some can be much stronger or
weaker than others. Occasionally,
the cycle can barely be detected at
all, as famously happened during
the ‘Maunder Minimum’, a period of
suppressed sunspot activity lasting
from around 1645 to 1715. This event
famously coincided with a so-called
‘Little Ice Age’ of severe winters acros
northern Europe and North America
and while it’s impossible to know if
TSI fell significantly more at this tim
researchers have recently shown thatlong-term fluctuations in the Sun’s
ultraviolet output could have triggere
changes to the regional climate.
So what of the current solar cycle?
Following strong and well-defined
cycles in the past few decades, Solar
Cycle 24, which officially began in
January 2008, has been somewhat
quiet, but also rather puzzling. High-
latitude spots were slow to appear in
the early months of the cycle, and aft
an active 2011, the Sun surprised mo
experts by slumping back into a lull
rather than building to an anticipated
peak in activity. However, some havespeculated that Cycle 24 might show
a double peak, with another burst of
activity in early 2014.
“This cycle is different from the
recent cycles,” explains Dr de Toma.
“During the space age we have seen
period of high solar activity, but Cycl
24 is a very weak cycle. Such weak
cycles have happened in the past,
but this is the first t ime we have the
opportunity to observe a weak cycle
with modern instrumentation.”
Another intrig uing feature
is that the Sun’s northern and
southern hemispheres seem to be
behaving rather differently: “Thetwo hemispheres are never perfectly
synchronised, but the hemispheric
difference in Cycle 24 is very
“The ensuing CME reachedthe Earth barely a day later,triggering northern lightsthat were visible as far southas the Caribbean”
These twoimages, with
October 2010on the left and
October 2012on the right,
show how theSun becomes
more active as itnears the peakof a solar cycle
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The solarcycle
19982000As the cycle continued,increasing numbers of bright,complex features appearedin each hemisphere, with theregions of activity graduallymoving towards the equator
2001Cycle 23 peaked between 2000 and2003. In March/April 2001, the Sunreleased huge CMEs and one of themost powerful flares ever recorded
20022004Centres of activity begin to
converge on the equator,forming a broad band of bright
features at low latitudes. TheSun’s overall magnetism starts to
lose its simple ‘dipole’ structure
20052006As masses of magnetisedgas meet at the equator,some start to cancel outand solar activity fadesaway. Other magneticmaterial is carried back tothe poles to regenerate anew dipole field
This sequence of images from NASA’s SOHspacecraft captures an entire solar cycle at extrem
ultraviolet wavelengths, highlighting hot featur
such as flares above the Sun’s visible surfa
19961997At the start of Solar Cycle 23, the Sun’sappearance was almost uniformly dark,with just a few bright hotspots of magneticactivity at relatively high latitudes
pronounced. Most of the activity at
the beginning of the cycle was in the
north, while now it is in the south.”
Indeed, the strange features of Cycle
24 illustrate the difficulty of making
predictions about the Sun’s behaviour,
as Dr de Toma points out: “Cycle 24
was the first time that physical models
of the Sun were used to predict a
solar cycle. Before that, the solar cycle
strength was usually predicted using
simple correlations between sunspot
numbers and other solar activity
proxies, or by extrapolating recent
solar behaviour into the future. Solarcycle models are still relatively simple,
and in spite of the progress in recent
years in modelling the solar cycle as
a hydromagnetic dynamo process,
we still do not have a realistic solar
dynamo model. This is an area where
I expect a lot of progress in the future,
both in terms of improving the models
and of obtaining new observations to
better constrain them.”
The weakness of Solar Cycle 24 has
even inspired some solar physicists
to suggest that we might be on the
Experts at the Space Weather Center at NASA’sGoddard Space Flight Center track solar
disruptions to predict their impact on Earth
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Weatheringstormsfrom spaceProfessor Mike Hapgood explainshow solar storms can affect Earth
What are the various ways solar
activity can influence Earth?Well space weather, like weather
on Earth, is very diverse. We have
geomagnetic storms that are caused
by the solar wi nd coming out from
the Sun, and they have a lot of
diverse effects all over the Earth
including changes to the upper
atmosphere, changes in the magneti
field that affect power grids, and
changes in the environment in near
Earth space that affect spacecraft
and so on. But we also have radiatio
storms – which are related, but a
Solar weather can have
an adverse effect on
satellites in Earth orbit
What is asunspot?Sunspots are dark patches of less
dense, relatively cool material.They form where loops of the solar
magnetic field emerge from and
re-enter the visible photosphere – the
magnetic field opens up a ‘clearing’
that can be up to 2,000 degrees
Celsius (3,630 degrees Fahrenheit)
cooler than its surroundings. For
this reason, spots or groups of spots
usually come in pairs, with a leading
and a trailing spot of opposite
magnetic polarities. The leading spots
in a given hemisphere always have the
same polarity as the general magnetic
field of the hemisphere itself, and lie
closer to the equator. A dark central
region known as the umbra shows
where the magnetic field lines emerge
vertically out of the photosphere, while
a less intense penumbra marks the
surrounding area where the magnetic
field lines are tilted and their cooling
influence is weaker.
Leading spotThe ‘leading’ sunspot liescloser to the equator andhas the same polarity to thehemisphere in which it lies.Magnetic field lines emerging
through the photosphereforce open a low-density‘clearing’ in the Sun’s gases
Trailing spotThe trailing spot is usuallysmaller than the leading spot,and often more complex instructure. Both spots aredepressed in relation to thesurrounding photosphere
Fine structureThe Sun’s photosphereis covered with fine cellscalled granules. Within thepenumbral region, they aredistorted by angled lines ofmagnetic field
Professor Mike Hapgood is headof the Space Environment Group
at the Rutherford AppletonLaboratory in Oxfordshire. As an
internationally recognised expert inthe eld of ‘space weather’, he has adeep interest in understanding the
practical impacts of solar activity onour planet and its technology.
INTERVIEW BIO
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quite different phenomenon – and
then there are also X-ray and radio
flashes – bursts of radiation that have
different effects. There’s a whole grab-
bag of environmental phenomena,
and these have all sorts of effects on various systems.
What are radiation storms?
These are particles that are
accelerated to very high speeds and
energies. What we call the ‘solar wind’
is the average flow of particles coming
out from the Sun, and while it might
be average, it can still be moving at
hundreds or thousands of kilometres
per second. But radiation storms
involve particles travelling very
close to the speed of light – almost a
thousand times faster. Light travels
from the Sun to the Earth in a little
over eight minutes, and radiationstorms are not much slower, while
the solar wind can take a day to three
days to reach the Earth. Because
they’re travelling much faster,
radiation storm particles can do more
damage – they can penetrate quite
deeply into spacecraft electronics, and
enter Earth’s atmosphere to produce
neutrons in the stratosphere. They
produce quite detectable levels of
radiation at aircraft altitudes, and
when there’s a really big burst we can
even detect it on the ground.
How much danger is there to
satellites in Earth orbit?
Geostationary satellites are by far the
most exposed – they’re orbiting in
the outer parts of Earth’s magnetic
field and get almost no protection,so they have to endure a lot of solar
radiation. The key is good design – on
computer chips for instance, a lot of
the challenge is about very careful
layout of the circuit, and maybe not
putting quite so much on the chip as
a whole. If you’re drawing all these
tiny electrical circuits what you don’t
want is a situation where a radiation
hit could cause a short circuit.
What influence can solar storms
have on ground-based electronics?
Well once again, the key is good
design – if the engineers are aware of
it, they can deal with it, and there’s alot of good work already being done.
For instance, aircraft are already very
robust to such issues, and even cars
are designed with this in mind – you
can hardly warn people not to drive
their cars today because there might
be a solar rad iation storm.
What about the risk of another
Québec-style incident?
Well that’s a very different effect, and
that comes from the geomagnetic
storms. Part of what they do is
cusp of a new long-term minimum
in sunspot numbers. In 2010,
astronomers from the National Solar
Observatory at Kitt Peak, Arizona,
reported evidence for a steady decline
in the strength of the magnetic fields
associated with sunspots over severaldecades, perhaps leading to a new
Maunder Minimum. Dr de Toma,
however, disagrees: “Solar activity has
been weak lately, but t his does not
make Solar Cycle 24 anomalous. We
had weak cycles before, for example
at the beginning of the 20th Century,
without going into a Maunder
Minimum. We still do not know how
and why the Sun went into a Maunder
Minimum, so we cannot predict one.”
What’s more, according to recent
research by Dr de Toma’s group at
NCAR and colleagues at California
State University, Northridge, the
sunspot claims may not stack up:“These observations are very accurate,
but the dataset suffers by serious
selection effects with only a very
few observations taken near the
beginning. Many have questioned
these results, and they have not been
confirmed by other observations.” Dr
de Toma herself was at the forefront of
one effort to crosscheck the evidence,
using detailed sunspot records from
the San Fernando Observatory dating
back to 1986 in a search for long-term
changes. “We did not find that spots
are becoming less dark over time,” sheexplains. “The original researchers
found a decrease in sunspot darkness
of about two per cent each year, but
we found a less than three per cent
change across the entire 27-year span
of the SFO observations.”
Nevertheless, it now seems quite
likely that the Sun does indeed have
longer activity cycles modulating the
11-year sunspot pattern. “There were
weak solar cycles at the beginning of
the 1800s and 1900s. We still do not
know for sure if there is a 100-year
modulation in solar activity, but this is
a very interesting idea.”
One thing is for certain, however– the Sun and its various cycles will
continue to influence everything from
technology to climate. We can do
nothing to influence our local star, so
we must learn to at least understand
it more accurately, and be prepared for
its occasional outbursts of violence.
disrupt the natural electric currents
that flow around the planet. It’s
the fluctuations in the current that
create changes in the magnetic
field, and that in turn can produce
electric currents through Earth’scrust. Those currents can get into
things like power grids through the
earth connections, and if they get
too big, they can upset the operation
of transformers. This can produce
heating, vibration and, in the worst
case, do serious physical damage –
but more li kely the grid collapse s
and they have to do a ‘black start’,
restarting the grid with the power
completely off. That’s something
that’s very heavily rehearsed, but
of course even having the grid off
for a few hours would be a major
disruption. The power grid is the
fundamental infrastructure of modernsociety, and if it’s not there then that’s
a real problem – but we should be able
to cope with other forms of heating
and lighting for a few hours.
Some people have warned about
the risk of a big event in the fairly
near future?
Well it’s always hard to predict – the
big events ca n happen any time in a
solar cycle and we prefer to talk abouonce-in-a-hundred-year risks. It’s not
a good idea to assume that you’re
safe from a major event just because
it’s solar minimum, though it might
be a bit less l ikely. Fortunately the
Sun’s been very quiet for most of the
past few years. On 23 July 2012 there
was a very la rge event, but that wen
off behind the Sun and there’s a lot
of research into what the effects on
Earth might have been if we had bee
in the way.
Finally, we guess that one positive
side effect of these major storms
for skywatchers would be somespectacular aurorae?
Well that’s certainly true – though
they might just have to watch them
with al l the lights out!
The Solar Max satellite, inoperation from 1980 to 1989
was one of the first spacecraft toclosely study solar cycles
“It’s not a good idea toassume that you’re safe froma major event just becauseit’s solar minimum”
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