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Aurora - Wikipedia. Aurora australis from the ISS, 2. Video of this encounter: [2]An aurora (plural: auroras),[a] sometimes referred to as polar lights, northern lights (aurora borealis) or southern lights (aurora australis), is a natural light display in the Earth's sky, predominantly seen in the high latitude (Arctic and Antarctic) regions. Auroras are produced when the magnetosphere is sufficiently disturbed by the solar wind that the trajectories of charged particles in both solar wind and magnetospheric plasma, mainly in the form of electrons and protons, precipitate them into the upper atmosphere (thermosphere/exosphere) due to Earth's magnetic field, where their energy is lost. The resulting ionization and excitation of atmospheric constituents emits light of varying color and complexity.

The form of the aurora, occurring within bands around both polar regions, is also dependent on the amount of acceleration imparted to the precipitating particles. Precipitating protons generally produce optical emissions as incident hydrogen atoms after gaining electrons from the atmosphere.

Proton auroras are usually observed at lower latitudes.[2]Occurrence of terrestrial auroras[edit]Most auroras occur in a band known as the auroral zone,[3] which is typically 3° to 6° wide in latitude and between 1. A region that currently displays an aurora is called the auroral oval, a band displaced towards the nightside of the Earth.[4] Early evidence for a geomagnetic connection comes from the statistics of auroral observations. Elias Loomis (1. 86. Hermann Fritz (1.

S. Tromholt (1. 88. Day- to- day positions of the auroral ovals are posted on the internet.[7]In northern latitudes, the effect is known as the Aurora Borealis or the Northern Lights. The former term was coined by Galileo in 1. Romangoddess of the dawn and the Greek name for the north wind.[8] The southern counterpart, the Aurora Australis or the Southern Lights, has features that are almost identical to the Aurora Borealis and changes simultaneously with changes in the northern auroral zone.[9] The Aurora Australis is visible from high southern latitudes in Antarctica, Chile, Argentina, New Zealand, and Australia. A geomagnetic storm causes the auroral ovals (north and south) to expand, and bring the aurora to lower latitudes.

It was hardly ever seen near the geographic pole, which is about 2. The instantaneous distribution of auroras ("auroral oval")[3] is slightly different, being centered about 3–5 degrees nightward of the magnetic pole, so that auroral arcs reach furthest toward the equator when the magnetic pole in question is in between the observer and the Sun. The aurora can be seen best at this time, which is called magnetic midnight. Auroras seen within the auroral oval may be directly overhead, but from farther away they illuminate the poleward horizon as a greenish glow, or sometimes a faint red, as if the Sun were rising from an unusual direction. Auroras also occur poleward of the auroral zone as either diffuse patches or arcs,[1. Video of the aurora australis taken by the crew of Expedition 2. International Space Station, its sequence of shots was taken 1.

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September 2. 01. 1 from 1. GMT, on an ascending pass from south of Madagascar to just north of Australia over the Indian Ocean. Video of the aurora australis taken by the crew of Expedition 2.

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International Space Station, its sequence of shots was taken 7 September 2. GMT, from the French Southern and Antarctic Lands in the South Indian Ocean to southern Australia.

Video of the aurora australis taken by the crew of Expedition 2. International Space Station, its sequence of shots was taken 1. September 2. 01. 1 from 1. GMT, from a descending pass near eastern Australia, rounding about to an ascending pass to the east of New Zealand. North America. Eurasia. These NOAA maps of North America and Eurasia show the local midnight equatorward boundary of the aurora at different levels of geomagnetic activity; a Kp=3 corresponds to low levels of geomagnetic activity, while Kp=9 represents high levels. Auroras are occasionally seen in latitudes below the auroral zone, when a geomagnetic storm temporarily enlarges the auroral oval.

Large geomagnetic storms are most common during the peak of the eleven- year sunspot cycle or during the three years after the peak.[1. Watch Alienated Online Free 2016. An aurora may appear overhead as a "corona" of rays, radiating from a distant and apparent central location, which results from perspective. An electron spirals (gyrates) about a field line at an angle that is determined by its velocity vectors, parallel and perpendicular, respectively, to the local geomagnetic field vector B. This angle is known as the "pitch angle" of the particle.

The distance, or radius, of the electron from the field line at any time is known as its Larmor radius. The pitch angle increases as the electron travels to a region of greater field strength nearer to the atmosphere.

Thus it is possible for some particles to return, or mirror, if the angle becomes 9. Other particles that do not mirror enter the atmosphere and contribute to the auroral display over a range of altitudes. Other types of auroras have been observed from space, e. These are relatively infrequent and poorly understood. There are other interesting effects such as flickering aurora, "black aurora" and sub- visual red arcs.

In addition to all these, a weak glow (often deep red) observed around the two polar cusps, the field lines separating the ones that close through the Earth from those that are swept into the tail and close remotely. The altitudes where auroral emissions occur were revealed by Carl Størmer and his colleagues who used cameras to triangulate more than 1.

They discovered that most of the light is produced between 9. Images of auroras are significantly more common today than in the past due to the increase in use of digital cameras that have high enough sensitivities.[1.

Film and digital exposure to auroral displays is fraught with difficulties. Due to the different color spectrum present, and the temporal changes occurring during the exposure, the results are somewhat unpredictable.

Different layers of the film emulsion respond differently to lower light levels, and choice of film can be very important. Longer exposures superimpose rapidly changing features, and often blanket the dynamic attribute of a display. Watch Pixel Perfect Megavideo. Higher sensitivity creates issues with graininess.