by APOD Robot » Sun May 30, 2021 4:06 am
Aurora over Clouds
Explanation: Auroras usually occur high above the clouds. The
auroral glow is created when fast-moving particles ejected from the Sun impact the
Earth's magnetosphere, from which charged particles spiral along the
Earth's magnetic field to strike atoms and molecules high in the
Earth's atmosphere. An
oxygen atom, for example, will glow in the green light commonly emitted by an
aurora after being energized by such a collision. The lowest part of an
aurora will typically occur about 100 kilometers up, while most clouds exist only below about 10 kilometers. The relative heights of clouds and
auroras are shown clearly in the
featured picture in 2015 from
Dyrholaey,
Iceland. There, a determined astrophotographer withstood
high winds and initially overcast skies in an attempt to capture aurora over a
picturesque lighthouse, only to take, by chance, the featured picture including elongated
lenticular clouds,
along the way.
[url=https://apod.nasa.gov/apod/ap210530.html] [img]https://apod.nasa.gov/apod/calendar/S_210530.jpg[/img] [size=150]Aurora over Clouds[/size][/url]
[b] Explanation: [/b] Auroras usually occur high above the clouds. The [url=http://www.atoptics.co.uk/highsky/auror3.htm]auroral glow[/url] is created when fast-moving particles ejected from the Sun impact the [url=http://science.nasa.gov/heliophysics/focus-areas/magnetosphere-ionosphere/]Earth's magnetosphere[/url], from which charged particles spiral along the [url=http://www.nasa.gov/mission_pages/sunearth/news/gallery/Earths-magneticfieldlines-dipole.html]Earth's magnetic field[/url] to strike atoms and molecules high in the [url=http://www.nasa.gov/mission_pages/sunearth/science/atmosphere-layers2.html]Earth's atmosphere[/url]. An [url=http://periodic.lanl.gov/8.shtml]oxygen[/url] atom, for example, will glow in the green light commonly emitted by an [url=https://apod.nasa.gov/apod/ap141103.html]aurora[/url] after being energized by such a collision. The lowest part of an [url=https://apod.nasa.gov/apod/ap130609.html]aurora[/url] will typically occur about 100 kilometers up, while most clouds exist only below about 10 kilometers. The relative heights of clouds and [url=http://www.gi.alaska.edu/AuroraForecast]auroras[/url] are shown clearly in the [url=https://www.facebook.com/NikonItalia/photos/a.380376239661.158168.147466084661/10153716437154662/]featured picture[/url] in 2015 from [url=https://youtu.be/_Om267wp-h4]Dyrholaey[/url], [url=https://en.wikipedia.org/wiki/Iceland]Iceland[/url]. There, a determined astrophotographer withstood [url=https://i2.wp.com/puppytoob.com/wp-content/uploads/2013/04/Dogs_In_Wind_9.jpg?resize=619%2C411&ssl=1]high winds[/url] and initially overcast skies in an attempt to capture aurora over a [url=https://apod.nasa.gov/apod/image/1511/DSC_6447.jpg]picturesque lighthouse[/url], only to take, by chance, the featured picture including elongated [url=https://apod.nasa.gov/apod/ap090203.html]lenticular clouds[/url], [url=https://quoteinvestigator.com/2012/05/06/other-plans/]along the way[/url].
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