Watts Up With That? 
Wednesday, Dec 17, 2008
I know. This sounds like a plot of a 1950’s scifi movie. But it is real. From my view, our localized corner of the solar system is now different than it used to be and changes in the magnetic interactions are evident everywhere. First we have the interplanetary magnetic field that took an abrupt dive in October 2005 and has not recovered since and remains at very low level:
Then we have the recent discovery that the ionosphere has dropped in altitude  to unexpected and unexplained low levels.
We have a solar cycle 24 (driven by the solar magnetic dynamo) which can’t seem to get out of the starting gate , being a year late with forecasts for activity from it being revised again and again.
And finally we have this, this discovery that Earth’s magnetic field can be ripped open and our atmosphere laid bare to the solar wind, much like Mars.
Magnetism is underrated in the grand scheme of things, in my opinion. We’d do well to pay more attention to magnetic trends in our corner of the universe and what effects it has on Earthly climate. – Anthony
(ARTICLE CONTINUES BELOW)
From NASA News  (h/t to Geoff Sharp)
Dec. 16, 2008: NASA’s five THEMIS spacecraft have discovered a breach in Earth’s magnetic field ten times larger than anything previously thought to exist. Solar wind can flow in through the opening to “load up” the magnetosphere for powerful geomagnetic storms. But the breach itself is not the biggest surprise. Researchers are even more amazed at the strange and unexpected way it forms, overturning long-held ideas of space physics.
“At first I didn’t believe it,” says THEMIS project scientist David Sibeck of the Goddard Space Flight Center. “This finding fundamentally alters our understanding of the solar wind-magnetosphere interaction.”
The magnetosphere is a bubble of magnetism that surrounds Earth and protects us from solar wind. Exploring the bubble is a key goal of the THEMIS mission, launched in February 2007. The big discovery came on June 3, 2007, when the five probes serendipitously flew through the breach just as it was opening. Onboard sensors recorded a torrent of solar wind particles streaming into the magnetosphere, signaling an event of unexpected size and importance.
Right: One of the THEMIS probes exploring the space around Earth, an artist’s concept. [more ]
“The opening was huge—four times wider than Earth itself,” says Wenhui Li, a space physicist at the University of New Hampshire who has been analyzing the data. Li’s colleague Jimmy Raeder, also of New Hampshire, says “1027 particles per second were flowing into the magnetosphere—that’s a 1 followed by 27 zeros. This kind of influx is an order of magnitude greater than what we thought was possible.”
The event began with little warning when a gentle gust of solar wind delivered a bundle of magnetic fields from the Sun to Earth. Like an octopus wrapping its tentacles around a big clam, solar magnetic fields draped themselves around the magnetosphere and cracked it open. The cracking was accomplished by means of a process called “magnetic reconnection.” High above Earth’s poles, solar and terrestrial magnetic fields linked up (reconnected) to form conduits for solar wind. Conduits over the Arctic and Antarctic quickly expanded; within minutes they overlapped over Earth’s equator to create the biggest magnetic breach ever recorded by Earth-orbiting spacecraft.
Above: A computer model of solar wind flowing around Earth’s magnetic field on June 3, 2007. Background colors represent solar wind density; red is high density, blue is low. Solid black lines trace the outer boundaries of Earth’s magnetic field. Note the layer of relatively dense material beneath the tips of the white arrows; that is solar wind entering Earth’s magnetic field through the breach. Credit: Jimmy Raeder/UNH. [larger image ]
The size of the breach took researchers by surprise. “We’ve seen things like this before,” says Raeder, “but never on such a large scale. The entire day-side of the magnetosphere was open to the solar wind.”
The circumstances were even more surprising. Space physicists have long believed that holes in Earth’s magnetosphere open only in response to solar magnetic fields that point south. The great breach of June 2007, however, opened in response to a solar magnetic field that pointed north.
“To the lay person, this may sound like a quibble, but to a space physicist, it is almost seismic,” says Sibeck. “When I tell my colleagues, most react with skepticism, as if I’m trying to convince them that the sun rises in the west.”
Here is why they can’t believe their ears: The solar wind presses against Earth’s magnetosphere almost directly above the equator where our planet’s magnetic field points north. Suppose a bundle of solar magnetism comes along, and it points north, too. The two fields should reinforce one another, strengthening Earth’s magnetic defenses and slamming the door shut on the solar wind. In the language of space physics, a north-pointing solar magnetic field is called a “northern IMF” and it is synonymous with shields up!
“So, you can imagine our surprise when a northern IMF came along and shields went down instead,” says Sibeck. “This completely overturns our understanding of things.”
Northern IMF events don’t actually trigger geomagnetic storms, notes Raeder, but they do set the stage for storms by loading the magnetosphere with plasma. A loaded magnetosphere is primed for auroras, power outages, and other disturbances that can result when, say, a CME (coronal mass ejection) hits.
The years ahead could be especially lively. Raeder explains: “We’re entering Solar Cycle 24. For reasons not fully understood, CMEs in even-numbered solar cycles (like 24) tend to hit Earth with a leading edge that is magnetized north. Such a CME should open a breach and load the magnetosphere with plasma just before the storm gets underway. It’s the perfect sequence for a really big event.”
Sibeck agrees. “This could result in stronger geomagnetic storms than we have seen in many years.”
For more information about the THEMIS mission, visit http://nasa.gov/themis