1. Airglow Ripples over Tibet Explanation: Why would the sky look like a giant target? Airglow

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5. Team Airglow is a group of Gossamer Aviators with the Human Powered Aircraft Airglow that maintain & fly the aircraft when

6. Airglow is the natural “glowing” of the Earth’s atmosphere.

7. Airglow is strongest over low and middle latitudes.

8. Airglow is the natural “glowing” of the Earth’s atmosphere

9. Airglow occurs all around the Earth, all the time.

10. Airglow carries information on the upper atmosphere’s temperature, density, and

11. Airglow is the natural “glowing” of the Earth’s atmosphere

12. There are three types of Airglow: dayglow, twilightglow and nightglow.

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14. There are three types of Airglow: dayglow, twilightglow and nightglow

15. Unlike the aurora, the Airglow is visible all over the globe

16. Airglow is caused by sunlight exciting ions in the atmosphere of Earth

17. Airglow interferes with optical and infrared observations of faint celestial bodies.

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19. The Airglow is brightest on Earth's day side where the original excitation occurs

20. Airglow, faint diffuse illumination of the night sky originating in the upper atmosphere

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23. According to a University of Albany website, the brightest source region for Airglow …

24. The airglow phenomenon was first identified in 1868 by Swedish physicist Anders Ångström.

25. Molecules that produce Airglow include sodium (Na), hydroxyl radicals (OH), and atomic oxygen (O)

26. Worked for the ECE Airglow project at UIUC, with goals of studying the ionosphere to

27. The night Airglow is (fortunately!) only one thousandth as bright and varies through the night

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29. ‘The orangish arc extending to the left from the aurora is Airglow viewed edgewise on the limb of the Earth.’ ‘There should not be any city lights or other light pollution: the Airglow is a faint glow.’ ‘Like its brighter and fast-moving relative the aurora, night Airglow has strong emissions at specific wavelengths.’

30. Airglow is defined as a luminosity or "glowing" given off by the Earth's own atmosphere

31. On a much longer timescale the Airglow varies with the 11 year cycle of solar activity.

32. Airglow is typically too faint to fire up the cone cells in our retinas responsible for color vision

33. Easily confused with the aurora borealis, or northern lights, the sightings were of another phenomena called “Airglow”.

34. Definition of Airglow : light that is observed especially during the night, that originates in the high atmosphere of a planet (such as the earth), and that is associated with photochemical reactions of gases caused by solar radiation Examples of Airglow in a Sentence

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36. According to Gordon Shepherd, an Aeronomer involved in the study, “Bright nights do exist, and they’re part of the variability of airglow that can be observed with satellite instruments.” Airglow is an atmospheric condition caused by chemicals in the upper layers of the Earth’s atmosphere.

37. ‘Click here to view a movie and narrative by Don Pettit describing some of the Airglow he has seen.’

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39. Airglow occurs when atoms and molecules in the upper atmosphere, excited by sunlight, emit light in order to shed their excess energy

40. Airglow definition: the faint light from the upper atmosphere in the night sky , esp in low latitudes Meaning, pronunciation, translations and examples

41. This causes faint light to be emitted is called Airglow. Humans have been exploring space in different forms for over 50 years now

42. Airglow, faint luminescence of Earth’s upper atmosphere that is caused by air molecules’ and atoms’ selective absorption of solar ultraviolet and X-radiation

43. Bright swaths of red in the upper atmosphere, known as Airglow, can be seen in this image taken from the International Space Station

44. Rainier National Park for a few hours, I captured this massive panorama of the Northern Lights and green Airglow over a beautiful lake.

45. Airglow is a visual depiction of the interaction between the upper boundaries of Earth's atmosphere and space beyond, an area of ongoing research at NASA

46. The enveloping orange hue is known as Airglow — a mesmerizing luminescence caused by chemical reactions high in Earth's atmosphere, NASA reported.This ghostly glow usually happens when

47. Airglow is a photochemical reaction in the Earth’s atmosphere caused by electronically excited atoms, molecules and ions that react to ultraviolet radiation from the Sun

48. Airglow comes from "the emission of light from chemical interactions between oxygen, nitrogen, and other molecules in the upper atmosphere." Auroras are the result of …

49. Nighttime Airglow (or nightglow) is a type of chemiluminescence —the emission of light from chemical interactions between oxygen, nitrogen, and other molecules in the upper atmosphere

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51. Designed for continuous and long-term use, the Airglow is constructed out of corrosion-resistant stainless steel and uses UV-C bulbs with a lifespan of 13,000 hours (approx

52. The phenomenon is similar to auroras, but where auroras are driven by high-energy particles originating from the solar wind, Airglow is sparked by day-to-day solar radiation

53. A photochemical reaction that occurs high in the atmosphere, Airglow is the result of various atoms, molecules and ions that get excited (chemistry-excited, that is… not “whee!”-excited) by

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58. Most of the Airglow emanates from the region about 50 to 300 km (31 to 180 miles) above the surface of Earth, with the brightest area concentrated at altitudes around 97 km (60 miles).

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60. Airglow [ âr ′glō′ ] A faint photochemical luminescence in the upper atmosphere caused by the collision of x-rays and charged particles from the Sun with atoms and molecules, especially of oxygen, sodium, and the hydroxyl radical (OH)

61. The amount of airglow and zodiacal light is quite variable (depending, amongst other things on sunspot activity and the Solar cycle) but given optimal conditions the darkest possible sky has a brightness of about 22 magnitude/square arcsecond.

62. Airglow (air -gloh) (nightglow) The faint everpresent glow arising in the Earth's atmosphere that is light emitted (along with infrared radiation) during the recombination of ionized atoms and molecules following collisions with high-energy particles and radiation, mainly from the Sun

63. Their 52-page "Nikon Astronomical Instruments" catalog lists a weight-driven 8-inch apochromat refractor, a 6-inch achromat, 12 and 36-inch reflectors, coronographs, nebular, airglow, auroral and grating spectrographs, 12-inch Coelostats, solar tower telescopes for museums and all sorts of plate measuring and photometric equipment.

64. Airglow is caused by various processes in the upper atmosphere, such as the recombination of atoms, which were photoionized by the sun during the day, luminescence caused by cosmic rays striking the upper atmosphere and chemiluminescence caused mainly by oxygen and nitrogen reacting with hydroxyl ions at heights of a few hundred kilometres