Earth’s magnetosphere extends about 65,000 km on the dayside but more than 10 times further (beyond the Moon’s orbit) on the nightside.
MOONDUST IN THE WIND:
Unlike Earth, the Moon has no magnetic field to ward off charged particles from the Sun. Solar wind blows directly onto the lunar surface. Researchers have long suspected that electrons in the solar wind become embedded in moondust, causing the dust to "charge up" and giving the Moon a very bad case of static cling.
http://science.nasa.gov/headlines/y2008 ... edmoon.jpg
Strange things can happen when moondust gathers charge. For one, the dust might rise up and, propelled by electrostatic repulsion, rush in a diaphanous wind across the lunar surface. Imagine, dust storms on an airless world with no weather!
But it could be even stranger than that. NASA researchers have discovered that moondust peppered with solar wind electrons gain not a negative but a positive charge. This unexpected and counterintuitive reaction makes it hard to predict what is really happening to dust on moon.
Get the full story from Science@NASA.
http://science.nasa.gov/headlines/y2008 ... hewind.htm
The Moon and the Magnetotail
April 17, 2008: Behold the full Moon. Ancient craters and frozen lava seas lie motionless under an airless sky of profound quiet. It's a slow-motion world where even a human footprint may last millions of years. Nothing ever seems to happen there.
Right?
Wrong. NASA-supported scientists have realized that something does happen every month when the Moon gets a lashing from Earth's magnetic tail.
"Earth's magnetotail extends well beyond the orbit of the Moon and, once a month, the Moon orbits through it," says Tim Stubbs, a University of Maryland scientist working at the Goddard Space Flight Center. "This can have consequences ranging from lunar 'dust storms' to electrostatic discharges."
Yes, Earth does have a magnetic tail. It is an extension of the same familiar magnetic field we experience when using a Boy Scout compass. Our entire planet is enveloped in a bubble of magnetism, which springs from a molten dynamo in Earth's core. Out in space, the solar wind presses against this bubble and stretches it, creating a long "magnetotail" in the downwind direction:
Anyone can tell when the Moon is inside the magnetotail. Just look: "If the Moon is full, it is inside the magnetotail," says Stubbs. "The Moon enters the magnetotail three days before it is full and takes about six days to cross and exit on the other side."
It is during those six days that strange things can happen.
During the crossing, the Moon comes in contact with a gigantic "plasma sheet" of hot charged particles trapped in the tail. The lightest and most mobile of these particles, electrons, pepper the Moon's surface and give the Moon a negative charge.
On the Moon's dayside this effect is counteracted to a degree by sunlight: UV photons knock electrons back off the surface, keeping the build-up of charge at relatively low levels. But on the nightside, in the cold lunar dark, electrons accumulate and voltages can climb to hundreds or thousands of volts.
Walking across the dusty charged-up lunar terrain, astronauts may find themselves crackling with electricity like a sock pulled out of a hot dryer. Touching another astronaut, a doorknob, a piece of sensitive electronics—any of these simple actions could produce an unwelcome zap. "Proper grounding is strongly recommended," advises Stubbs.
The ground, meanwhile, may leap into the sky. There is compelling evidence (see, e.g., the Surveyor 7 image below) that fine particles of moondust, when sufficiently charged-up, actually float above the lunar surface. This could create a temporary nighttime atmosphere of dust ready to blacken spacesuits, clog machinery, scratch faceplates (moondust is very abrasive) and generally make life difficult for astronauts.
Stranger still, moondust might gather itself into a sort of diaphanous wind. Drawn by differences in global charge accumulation, floating dust would naturally fly from the strongly-negative nightside to the weakly-negative dayside. This "dust storm" effect would be strongest at the Moon's terminator, the dividing line between day and night.
Much of this is pure speculation, Stubbs cautions. No one can say for sure what happens on the Moon when the magnetotail hits, because no one has been there at the crucial time. "Apollo astronauts never landed on a full Moon and they never experienced the magnetotail."
The best direct evidence comes from NASA's Lunar Prospector spacecraft, which orbited the Moon in 1998-99 and monitored many magnetotail crossings. During some crossings, the spacecraft sensed big changes in the lunar nightside voltage, jumping "typically from -200 V to -1000 V," says Jasper Halekas of UC Berkeley who has been studying the decade-old data.
"It is important to note," says Halekas, "that the plasma sheet (where all the electrons come from) is a very dynamic structure. The plasma sheet is in a constant state of motion, flapping up and down all the time. So as the Moon orbits through the magnetotail, the plasma sheet can sweep across it over and over again. Depending on how dynamic things are, we can encounter the plasma sheet many times during a single pass through the magnetotail with encounters lasting anywhere from minutes to hours or even days."
"As a result, you can imagine how dynamic the charging environment on the Moon is. The Moon can be just sitting there in a quiet region of the magnetotail and then suddenly all this hot plasma goes sweeping by causing the nightside potential to spike to a kilovolt. Then it drops back again just as quickly."
The roller coaster of charge would be at its most dizzying during solar and geomagnetic storms. "That is a very dynamic time for the plasma sheet and we need to study what happens then," he says.
What happens then? Next-generation astronauts are going to find out. NASA is returning to the Moon in the decades ahead and plans to establish an outpost for long-term lunar exploration. It turns out they'll be exploring the magnetotail, too.
Solar Wind vs. Magnetotail: Earth's magnetotail isn't the only source of plasma to charge the Moon. Solar wind can provide charged particles, too; indeed, most of the time, the solar wind is the primary source. But when the Moon enters the magnetotail, the solar wind is pushed back and the plasma sheet takes over. The plasma sheet is about 10 times hotter than the solar wind and that gives it more "punch" when it comes to altering the charge balance of the Moon's surface. Two million degree electrons in the plasma sheet race around like crazy and many of them hit the Moon's surface. Solar wind electrons are relatively cool at only 140 thousand degrees, and fewer of them zip all the way down to the shadowed surface of the Moon's nightside.
http://science.nasa.gov/headlines/y2008 ... totail.htm

Solar Wind vs. Magnetotail: Earth's magnetotail isn't the only source of plasma to charge the Moon. Solar wind can provide charged particles, too; indeed, most of the time, the solar wind is the primary source. But when the Moon enters the magnetotail, the solar wind is pushed back and the plasma sheet takes over. The plasma sheet is about 10 times hotter than the solar wind and that gives it more "punch" when it comes to altering the charge balance of the Moon's surface. Two million degree electrons in the plasma sheet race around like crazy and many of them hit the Moon's surface. Solar wind electrons are relatively cool at only 140 thousand degrees, and fewer of them zip all the way down to the shadowed surface of the Moon's nightside.
Subject: (7) There's no dust on the lander footpads
Rebuttal
The Moon has no atmosphere in which eddies and such can cause
the dust to swirl and "float around". Dust is "shot" away when
there is no atmosphere. Therefore it is difficult to say
whether the foot pads would have been covered in dust with any
certainty. The chances are that some hollows and crevices will
contain trapped dust but all of the images I have seen look
remarkably clean. Nothing conclusive here in my opinion though.
Ion01 wrote:Hey! It looks like they are finally starting to get it. No if they can just apply that same knowledge elsewhere, such as the winds and storms on earth, then we can really get somewhere!
junglelord wrote:
MGmirkin wrote:I might, once again, add to that the "prior art" listed below.
(Moon Fountains)
http://science.nasa.gov/headlines/y2005 ... ntains.htm
(A DYNAMIC FOUNTAIN MODEL FOR LUNAR DUST.)
http://www.lpi.usra.edu/meetings/lpsc2005/pdf/1899.pdf
&
(Moon Storms)
http://science.nasa.gov/headlines/y2005 ... storms.htm
I think I'd mentioned these somewhere on "Thunderbolts Forum 1.0," which is sadly lost, but not forgotten, nor completely gone (still working on that, as time permits!)...
The long slow slog continues. Nature will inevitably force them to RECOGNIZE!
Granted they're still calling it the "magnetic tail" or the "magnetotail." But they're not acknowledging that currents are required to sustain a dynamic magnetic field in a plasma.
Should really be calling it the plasma sheath or plasma tail.
Likewise, they're still calling Birkeland currents "magnetic ropes," "flux ropes," "flux tubes," anything and everything to not directly say "electric current" or credit Birkeland's contribution.
Ion01 wrote:True, it is extremely frustrating that they discover "new" things, which are not new at all, and don't give people like Birkeland credit. However, articles like this, and some of the others you referenced, make it easier for us to educate the public about people like Birkeland.
True, it is extremely frustrating that they discover "new" things, which are not new at all, and don't give people like Birkeland credit.
"Is it not the case that at first a new idea is regarded as not true, and later, when accepted, as not being new?" I.Velikovsky 1952
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