Earth’s magnetosphere allows solar wind to leak into it
Data from European Space Agency’s Cluster mission has revealed that it is easier for the solar wind to penetrate Earth’s magnetic environment, the magnetosphere.
Washington: Data from European Space Agency’s Cluster mission has revealed that it is easier for the solar wind to penetrate Earth’s magnetic environment, the magnetosphere, than had previously been thought.
Scientists from NASA’s Goddard Space Flight Center in Greenbelt, Md. have, for the first time, directly observed the presence of certain waves in the solar wind -- called Kelvin-Helmholtz waves that can help transfer energy into near-Earth space -- under circumstances when previous theories predicted they were not expected.
The study showed that the presence of these waves help the incoming charged particles of the solar wind breach the magnetopause -- the outer region of the magnetic “shield” around our planet. As a result, the boundary of Earth’s magnetic bubble behaves less like a continuous barrier and more like a sieve allowing entry to the continuous onslaught of energetic electrons and protons.
This latest discovery was made possible by the unique configuration of the four identical Cluster spacecraft, which fly in a closely controlled formation through near-Earth space. As they sweep from the magnetosphere into interplanetary space and back again, the flotilla provides unique three-dimensional insights on the processes that connect the Sun to Earth.
Previous discoveries derived from Cluster measurements have shown that the magnetopause is commonly subject to Kelvin-Helmholtz waves. These waves have a distinctive shape that is quite familiar: they look like large amplitude ocean waves that are whipped up by strong winds. Such waves generate turbulence as they crest and break.
In the case of the solar wind, the waves are made of huge swirls of electrified gas called plasma, up to 25,000 miles across, which develop along the outer edge of the magnetosphere. Moving plasma, and therefore the Kelvin-Helmholtz waves, trap magnetic fields along with them, which turn out to be crucial in trying to determine how the solar wind can enter the magnetosphere.
As the magnetic field becomes wrapped up in the Kelvin-Helmholtz waves, oppositely directed fields can “reconnect”, allowing plasma to move from the solar wind into the magnetosphere.
“The space weather community pays considerable attention to Kelvin-Helmholtz waves because they have global influence on Earth’s magnetic system and are important for understanding Earth’s response to changes on the Sun,” said Kyoung-Joo Hwang, a research scientist at Goddard and the University of Maryland Baltimore County and lead author of the paper.
In general, the solar wind’s ability to penetrate into near-Earth space is thought to rely on the magnetic alignment of the interplanetary magnetic fields, often shortened to IMF. As the solar wind streams from the Sun toward the day side of Earth, its magnetic fields connect up to those of Earth, resulting in a sudden and dramatic reconfiguration or reconnection of the field lines.
This is most efficient when the IMF is aligned southward -- opposite to the northward alignment of Earth’s magnetic field. The temporary tangling of the field lines creates ideal conditions for magnetic reconnection, allowing large amounts of plasma and magnetic energy to be transferred from the solar wind to the magnetosphere.
Magnetic reconnection also occurs more weakly with a northward orientation of the IMF, generally only seen at higher latitudes. Spacecraft observations have indicated that Kelvin-Helmholtz waves may play an important role in the transfer of solar wind material into the magnetosphere during a northward IMF -- a hypothesis bolstered by the fact that the waves can facilitate magnetic reconnection. However, previous identification of Kelvin-Helmholtz waves during northward IMF were limited to the low latitude flanks of the magnetosphere.
The team of scientists has now directly observed these Kelvin-Helmholtz waves at high latitudes under other orientations of the IMF. Instead of pointing north or south, the IMF was pointing west, towards the dawn side of Earth.
Under these conditions, the Cluster data showed the waves on the dusk side of the high-latitude magnetopause. The magnetopause is the boundary between the relatively undisturbed magnetosphere and the magnetosheath, the region containing solar wind plasma that has come across the bow shock that protects Earth from the direct onslaught of solar wind plasma.
The scientists were also able to characterize how differences in IMF orientation greatly influenced the Kelvin-Helmholtz waves as a result of variations in the thickness and other characteristics of the boundary layer.
While the paper reports on only one case study, similar conditions are frequently found in the magnetosphere, said Melvyn Goldstein, a geospace scientist at Goddard and an author on the paper.
“Since this and similar geometrical orientations of the IMF are common, the process we describe might act as a fairly continuous mechanism of solar wind transport into the magnetosphere,” Goldstein added.
The paper was recently published in the Journal of Geophysical Research.