We all know that the Sun is overwhelmingly important to life
on Earth, but few of us have been given a good description of our star and its
variations.

The Sun is an average star, similar to millions of others
in the Universe. It is a prodigious energy machine, manufacturing about
4.0E023 kilowatts of energy per second. In other words, if the total output of
the Sun was gathered for one second it would provide the U.S. with enough
energy, at its current usage rate, for the next 9,000,000 years. The basic
energy source for the Sun is nuclear fusion, which uses the high temperatures
and densities within the core to fuse hydrogen, producing energy and creating
helium as a byproduct. The core is so dense and the size of the Sun so great
that energy released at the center of the Sun takes about 50,000,000 years to
make its way to the surface, undergoing countless absorptions and re-emissions
in the process. If the Sun were to stop producing energy today, it would take
50,000,000 years for significant effects to be felt at Earth!
The Sun has been producing its radiant and thermal energies
for the The Sun has been producing its radiant and thermal energies for the past
four or five billion years. It has enough hydrogen to continue producing for
another hundred billion years. However, in about ten to twenty billion years the
surface of the Sun will begin to expand, enveloping the inner planets (including
Earth). At that time, our Sun will be known as a red giant star. If the Sun were
more massive, it would collapse and re-ignite as a helium-burning star. Due to
its average size, however, the Sun is expected to merely contract into a
relatively small, cool star known as a white dwarf.
It has long been known that the Sun is neither featureless
nor steady. (Theophrastus first identified sunspots in the year 325 B.C.) Some
of the more important solar features are explained in the following sections.
Sunspots

Sunspots, dark areas on the solar surface, contain transient,
concentrated magnetic fields. They are the most prominent visible features on
the Sun; a moderate-sized sunspot is about as large as Earth. Sunspots form and
dissipate over periods of days or weeks. They occur when strong magnetic fields
emerge through the solar surface and allow the area to cool slightly, from a
background value of 6000 degrees C down to about 4200 degrees C; this area
appears as a dark spot in contrast with the Sun. The darkest area at the center
of a sunspot is called the umbra; it is here that the magnetic field strengths
are the highest. The less-dark, striated area around the umbra is called the
penumbra. Sunspots rotate with the solar surface, taking about 27 days to make a
complete rotation as seen from Earth. Sunspots near the Sun’s equator rotate
at a faster rate than those near the solar poles. Groups of sunspots, especially
those with complex magnetic field configurations, are often the sites of flares.
Over the last 300 years, the average number of sunspots has
regularly waxed and waned in an 11-year sunspot cycle. The Sun, like Earth, has
its seasons but its year equals 11 of ours. The last solar minimum was in 1996,
and the next maximum is expected in 2001.

Coronal holes are variable solar features that can last for
months to years. They are seen as large, dark holes when the Sun is viewed in
x-ray wavelengths. These holes are rooted in large cells of unipolar magnetic
fields on the Sun’s surface; their field lines extend far out into the solar
system. These open field lines allow a continuous outflow of high-velocity solar
wind. Coronal holes have a long-term cycle, but it doesn’t correspond exactly
to the sunspot cycle; they holes tend to be most numerous in the years following
sunspot maximum. At some stages of the solar cycle, these holes are continuously
visible at the solar north and south poles.
Prominences
Solar prominences (seen as dark filaments on the disk) are
usually quiescent clouds of solar material held above the solar surface by
magnetic fields. Most prominences erupt at some point in their lifetime,
releasing large amounts of solar material into space.
Flares


Solar flares are intense, temporary releases of energy. They
are seen at ground-based observatories as bright areas on the Sun in optical
wavelengths and as bursts of noise at radio wavelengths; they can last from
minutes to hours. Flares are our solar system’s largest explosive events which
can be equivalent to approximately 40 billion Hiroshima-size atomic bombs. The
primary energy source for flares appears to be the tearing and reconnection of
strong magnetic fields. They radiate throughout the electromagnetic spectrum,
from gamma rays to x-rays, through visible light out to kilometer-long radio
waves.
Coronal Mass Ejections

The outer solar atmosphere, the corona, is structured by
strong magnetic fields. Where these fields are closed, often above sunspot
groups, the confined solar atmosphere can suddenly and violently release bubbles
or tongues of gas and magnetic fields called coronal mass ejections. A large CME
can contain 10.0E16 grams (a billion tons) of matter that can be accelerated to
several million miles per hour in a spectacular explosion. Solar material
streaks out through the interplanetary medium, impacting any planets or
spacecraft in its path. CMEs are sometimes associated with flares but usually
occur independently.
Between Sun and Earth
The region between the Sun and the planets has been termed
the interplanetary medium. Although once considered a perfect vacuum, this is
actually a turbulent region dominated by the solar wind, which flows at
velocities of approximately 250-1000 km/s (about 600,000 to 2,000,000 miles per
hour). Other characteristics of the solar wind (density, composition, and
magnetic field strength, among others) vary with changing conditions on the Sun.
The effect of the solar wind can be seen in the tails of comets which always
point away from the Sun.
The solar wind flows around obstacles such as planets, but
those planets with their own magnetic fields respond in specific ways. Earth’s
magnetic field is very similar to the pattern formed when iron filings align
around a bar magnet. Under the influence of the solar wind, these magnetic field
lines are compressed in the Sunward direction and stretched out in the downwind
direction. This creates the magnetosphere, a complex, teardrop-shaped cavity
around Earth. The Van Allen radiation belts are within this cavity, as is the
ionosphere, a layer of Earth’s upper atmosphere where photo ionization by
solar x-rays and extreme ultraviolet rays creates free electrons. Earth’s
magnetic field senses the solar wind its speed, density, and magnetic field.
Because the solar wind varies over time scales as short as seconds, the
interface that separates interplanetary space from the magnetosphere is very
dynamic. Normally this interface called the magnetopause lies at a distance
equivalent to about 10 Earth radii in the direction of the Sun. However, during
episodes of elevated solar wind density or velocity, the magnetopause can be
pushed inward to within 6.6 Earth radii (the altitude of geosynchronous
satellites). As the magnetosphere extracts energy from the solar wind, internal
processes produce geomagnetic storms.
Solar Effects at Earth
Some major terrestrial results of solar variations are the
aurora, proton events, and geomagnetic storms.
Aurora
The aurora is a dynamic and visually delicate manifestation
of solar-induced geomagnetic storms. The solar wind energizes electrons and ions
in the magnetosphere. These particles usually enter Earth’s upper atmosphere
near the polar regions. When the particles strike the molecules and atoms of the
thin, high atmosphere, some of them start to glow in different colors.
Aurorae begin between 60 and 80 degrees latitude. As a storm
intensifies, the aurorae spread toward the equator. During an unusually large
storm in 1909, an aurora was visible at Singapore, on the geomagnetic equator.
The aurorae provide pretty displays, but they are just a visible sign of
atmospheric changes that may wreak havoc on technological systems.
Proton Events
Energetic protons can reach Earth within 30 minutes of a
major flare’s peak. During such an event, Earth is showered energetic solar
particles (primarily protons) released from the flare site. Some of these
particles spiral down Earth’s magnetic field lines, penetrating the upper
layers of our atmosphere where they produce additional ionization and may
produce a significant increase in the radiation environment.
Geomagnetic Storms
One to four days after a flare or eruptive prominence occurs,
a slower cloud of solar material and magnetic fields reaches Earth, buffeting
the magnetosphere and resulting in a geomagnetic storm. These storms are
extraordinary variations in Earth’s surface magnetic field. During a
geomagnetic storm, portions of the solar wind’s energy is transferred to the
magnetosphere, causing Earth’s magnetic field to change rapidly in direction
and intensity and energize the particle populations within it.
Disrupted Systems
Communications
Many communication systems utilize the ionosphere to reflect
radio signals over long distances. Ionospheric storms can affect radio
communication at all latitudes. Some radio frequencies are absorbed and others
are reflected, leading to rapidly fluctuating signals and unexpected propagation
paths. TV and commercial radio stations are little affected by solar activity,
but ground-to-air, ship-to-shore, Voice of America, Radio Free Europe, and
amateur radio are frequently disrupted. Radio operators using high frequencies
rely upon solar and geomagnetic alerts to keep their communication circuits up
and running. Some military detection or early-warning systems are also affected
by solar activity. The Over-the-Horizon Radar bounces signals off the ionosphere
in order to monitor the launch of aircraft and missiles from long distances.
During geomagnetic storms, this system can be severely hampered by radio
clutter. Some submarine detection systems use the magnetic signatures of
submarines as one input to their locating schemes. Geomagnetic storms can mask
and distort these signals. The Federal Aviation Administration routinely
receives alerts of solar radio bursts so that they can recognize communication
problems and forego unnecessary maintenance. When an aircraft and a ground
station are aligned with the Sun, jamming of air-control radio frequencies can
occur. This can also happen when an Earth station, a satellite, and the Sun are
in alignment.
Navigation Systems

Systems such as LORAN and OMEGA are adversely affected when
solar activity disrupts their signal propagation. The OMEGA system consists of
eight transmitters located through out the world. Airplanes and ships use the
very low frequency signals from these transmitters to determine their positions.
During solar events and geomagnetic storms, the system can give navigators
information that is inaccurate by as much as several miles. If navigators are
alerted that a proton event or geomagnetic storm is in progress, they can switch
to a backup system. GPS signals are affected when solar activity causes sudden
variations in the density of the ionosphere.
Satellites

Geomagnetic storms and increased solar ultraviolet emission
heat Earth’s upper atmosphere, causing it to expand. The heated air rises, and
the density at the orbit of satellites up to about 1000 km increases
significantly. This results in increased drag on satellites in space, causing
them to slow and change orbit slightly. Unless low-Earth-orbit satellites are
routinely boosted to higher orbits, they slowly fall, and eventually burn up in
Earth’s atmosphere.
Skylab is an example of a spacecraft re-entering Earth’s
atmosphere prematurely as a result of higher-than-expected solar activity.
During the great geomagnetic storm of March 1989, four of the Navy’s
navigational satellites had to be taken out of service for up to a week.
As technology has allowed spacecraft components to become
smaller, their miniaturized systems have become increasingly vulnerable to the
more energetic solar particles. These particles can cause physical damage to
microchips and can change software commands in satellite- borne computers.
Differential Charging. Another problem for satellite
operators is differential charging. During geomagnetic storms, the number and
energy of electrons and ions increase. When a satellite travels through this
energized environment, the charged particles striking the spacecraft cause
different portions of the spacecraft to be differentially charged. Eventually,
electrical discharges can arc across spacecraft components, harming and possibly
disabling them. Bulk Charging. Bulk charging (also called deep charging) occurs
when energetic particles, primarily electrons, penetrate the outer covering of a
satellite and deposit their charge in its internal parts. If sufficient charge
accumulates in any one component, it may attempt to neutralize by discharging to
other components. This discharge is potentially hazardous to the satellite’s
electronic systems.
Radiation Hazards to Humans

Intense solar flares release very-high-energy particles that
can be as injurious to humans as the low-energy radiation from nuclear blasts.
Earth’s atmosphere and magnetosphere allow adequate protection for us on the
ground, but astronauts in space are subject to potentially lethal dosages of
radiation. The penetration of high-energy particles into living cells, measured
as radiation dose, leads to chromosome damage and, potentially, cancer. Large
doses can be fatal immediately. Solar protons with energies greater than 30 MeV
are particularly hazardous. In October 1989, the Sun produced enough energetic
particles that an astronaut on the Moon, wearing only a space suit and caught
out in the brunt of the storm, would probably have died. (Astronauts who had
time to gain safety in a shelter beneath moon soil would have absorbed only
slight amounts of radiation.)
Solar proton events can also produce elevated radiation
aboard aircraft flying at high altitudes. Although these risks are small,
monitoring of solar proton events by satellite instrumentation allows the occasional
exposure to be monitored and evaluated.
Geologic Exploration
Earth’s magnetic field is used by geologists to determine
subterranean rock structures. For the most part, these geodetic surveyors are
searching for oil, gas, or mineral deposits. They can accomplish this only when
Earth’s field is quiet, so that true magnetic signatures can be detected.
Other surveyors prefer to work during geomagnetic storms, when the variations to
Earth’s normal subsurface electric currents help them to see subsurface oil or
mineral structures. For these reasons, many surveyors use geomagnetic alerts and
predictions to schedule their mapping activities.
Electric Power

When magnetic fields move about in the vicinity of a
conductor such as a wire, an electric current is induced into the conductor.
This happens on a grand scale during geomagnetic storms. Power companies
transmit alternating current to their customers via long transmission lines. The
nearly direct currents induced in these lines from geomagnetic storms are
harmful to electrical transmission equipment. On March 13, 1989, in Montreal,
Quebec, 6 million people were without commercial electric power for 9 hours as a
result of a huge geomagnetic storm. Some areas in the northeastern U.S. and in
Sweden also lost power. By receiving geomagnetic storm alerts and warnings,
power companies can minimize damage and power outages.
Pipelines

Rapidly fluctuating geomagnetic fields can induce currents
into pipelines. During these times, several problems can arise for pipeline
engineers. Flow meters in the pipeline can transmit erroneous flow information,
and the corrosion rate of the pipeline is dramatically increased. If engineers
unwittingly attempt to balance the current during a geomagnetic storm, corrosion
rates may increase even more. Pipeline managers routinely receive alerts and
warnings to help them provide an efficient and long-lived system.
Climate
The Sun is the heat engine that drives the circulation of our
atmosphere. Although it has long been assumed to be a constant source of energy,
recent measurements of this solar constant have shown that the base output of
the Sun can vary by up to two tenths of a percent over the 11-year solar cycle.
Temporary decreases of up to one-half percent have been observed. Atmospheric
scientists say that this variation is significant and that it can modify climate
over time. Plant growth has been shown to vary over the 11-year sunspot and
22-year magnetic cycles of the Sun, as evidenced in tree-ring records.
While the solar cycle has been nearly regular during the last
300 years, there was a period of 70 years during the 17th and 18th centuries
when very few sunspots were seen (even though telescopes were widely used). This
drop in sunspot number coincided with the timing of the little ice age in
Europe, implying a Sun- to-climate connection. Recently, a more direct link
between climate and solar variability has been speculated. Stratospheric winds
near the equator blow in different directions, depending on the time in the
solar cycle. Studies are under way to determine how this wind reversal affects
global circulation patterns and weather.
During proton events, many more energetic particles reach
Earth’s middle atmosphere. There they cause molecular ionization, creating
chemicals that destroy atmospheric ozone and allow increased amounts of harmful
solar ultraviolet radiation to reach Earth’s surface. A solar proton event in
1982 resulted in a temporary 70% decrease in ozone densities.
Biology
There is a growing body of evidence that changes in the
geomagnetic field affect biological systems. Studies indicate that physically
stressed human biological systems may respond to fluctuations in the geomagnetic
field. Interest and concern in this subject have led the Union of Radio Science
International to create a new commission entitled Electromagnetics in
Biology and Medicine.
Possibly the most closely studied of the variable Sun’s
biological effects has been the degradation of homing pigeons’ navigational
abilities during geomagnetic storms. Pigeons and other migratory animals, such
as dolphins and whales, have internal biological compasses composed of the
mineral magnetite wrapped in bundles of nerve cells. While this probably is not
their primarily method of navigation, there have been many pigeon race smashes,
a term used when only a small percentage of birds return home from a release
site. Because these losses have occurred during geomagnetic storms, pigeon
handlers have learned to ask for geomagnetic alerts and warnings as an aid to
scheduling races.
Conclusion
It has been realized and appreciated only in the last few
decades that solar flares, CMEs, and magnetic storms affect people and their
activities. The list of consequences grows in proportion to our dependence on
technological systems. The subtleties of the interactions between Sun and Earth,
and between solar particles and delicate instruments, have become factors that
affect our well being. Thus there will be continued and intensified need for
space environment services to address health, safety, and commercial needs.
Suggested Reading
Davies, K., 1990, Ionospheric Radio. Peter Peregrinus, London.
Eather, R. H., 1980, Majestic Lights. AGU, Washington,
D.C.
Garrett, H. B., and C. P. Pike, eds., 1980,
Space Systems and Their Interactions with Earth’s Space Environment. New York:
American Institute of Aeronautics and Astronautics.
Gauthreaux, S., Jr., 1980, Animal Migration:
Orientation and Navigation.,Chapter5. Academic Press, New
York.
Harding, R., 1989, Survival in Space. Routledge, New
York.
Joselyn, J. A., 1992, The impact of solar flares and magnetic storms on humans.
EOS, 73(7): 81,
84-85.
Johnson, N. L., and D. S. McKnight, 1987, Artificial Space Debris. Orbit Book
Co., Malabar,
Florida.
Lanzerotti, L. J., 1979, Impacts of ionospheric/magnetospheric process on
terrestrial science and technology. In Solar System Plasma Physics, III, L. J.
Lanzerotti, C. F. Kennel, and E. N. Parker, eds. North Holland Publishing Co.,
New
York.
Campbell, W. H., 2001, Earth Magnetism: A Guided Tour Through Magnetic Fields,
Harcourt Sci. and Tech. Co., New York