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The Solar Wind
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The Sun makes itself known throughout much of
the Solar System by the influence the
solar wind of high-speed charged particles constantly blowing off the Sun.
The solar wind may be viewed as an extension of the outer atmosphere of the Sun
(the corona) into interplanetary space.
Components of the Solar Wind
The solar wind contains roughly equal number of electrons and
protons, along with a few
heavier ions, and blows continously
from the
surface of the Sun at an average velocity of about 400 km/second. This is a
remarkable velocity: particles in the solar wind from the Sun's surface travel
at a speed that would allow them to go from Knoxville to Memphis in
less than 2 seconds!
This wind leads to a mass loss of more than 1 million tons of material per second,
which may seem like a large number, but is insignificant relative to the total mass
of the Sun.
The Role of the Coronal Magnetic Field
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Magnetic field lines in the solar corona
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The solar wind escapes primarily through
coronal holes, which are found predominantly near the
Sun's poles; in
the equatorial plane the
magnetic field lines of the Sun are more likely to close on themselves,
particularly in periods of low solar activity. These closed field lines trap the
hot coronal gases, leading to enhanced X-ray emissions from these hotter regions,
but suppressing contributions to the solar wind.
The adjacent image shows an enhanced image of the solar corona. In this image
the magnetic field lines of the corona correspond approximately to the boundaries
between regions of different color
(more info). Notice that in the equatorial regions the field
lines traced by these color boundaries tend to form closed loops, indicating the
trapping of coronal gas.
Influence of the Solar Wind on the Earth
As we have already discussed in the section on the
Earth,
the solar wind can have a large influence on our planet, particularly in times of
the active Sun (near sunspot maximum) when the wind is strong and can
contain bursts corresponding to flares and coronal mass ejections from the Sun.
The solar wind has a significant influence on our
ionosphere,
the Earth's
magnetic field, on Earth's
auroras,
and on telecommunication systems. For example, there is reason to believe
that a burst of
particles from a coronal mass ejection detected 5 days earlier by SOHO
may have killed the Telstar 401
communications satellite on January 11, 1997
(News Story).
Earth's Ionosphere and the Sun
The level of activity on the Sun can have a large influence on the Earth's
ionosphere, as illustrated in the following animations.
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Electron Density
The adjacent animations simulate
the variation by month of the ionosphere for two different years:
1. The year 1990 (upper image), which was
a period of high solar activity with many (150) sunspots.
2. The year 1996 (lower image), which was
a period of low solar activity with few (10) sunspots.
The plots show electron density contours, which are an indication of the amount
of ionization in the atmosphere.
Yellows and reds indicate
larger ionization and blues and greens indicate smaller ionization.
Notice the
substantial differences in these two animations, with much stronger
atmospheric ionization in the upper image (the active Sun of 1990) than
the lower image (the quiet Sun of 1996).
The adjacent images are based on these
electron density
contour maps of the
ionosphere
for months in the year 1957 to the present. Additional animations
may be found in this
NOAA directory.
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The level of solar activity has similar effects on related phenomena such as
Earth's auroras.
The "Space Weather" Report
One can monitor
solar data for the last 30 days.
This data gives information on
solar flares, sunspots, X-ray and radio-frequency fluxes.
One can even tune into
Today's Space
Weather, which gives a "weather report" of current and predicted
conditions in space with respect to the solar wind, solar activity, X-ray
activity, and related phenomena.
For example, here is the space weather outlook that was reported
on January 27, 1998:
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Space Weather Outlook
SOLAR ACTIVITY IS EXPECTED TO REMAIN
LOW. REGIONS 8142 AND 8143 COULD PRODUCE ISOLATED C-CLASS FLARES.
THERE IS ALSO A SLIGHT CHANCE FOR AN M-CLASS FLARE FROM EITHER
REGION.
THE GEOMAGNETIC FIELD IS
EXPECTED TO BE MOSTLY QUIET THROUGH 28 JANUARY. A DISTURBANCE IS
EXPECTED DURING 29 - 30 JANUARY IN RESPONSE TO THE PARTIAL-HALO CME
THAT OCCURRED ON 25 JANUARY. UNSETTLED TO MINOR STORM LEVELS ARE
EXPECTED DURING THE DISTURBANCE.
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In this report, the region numbers refer to active areas on the Sun, C and M
are classifications of solar flares, and CME stands for a coronal mass ejection.
As noted above in conjuction with the ill-fated Telstar 401 satellite, "space
weather" may have non-trivial practical consequences.
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