APOD: Noctilucent Cloud Storm Panorama (2009 July 11)
Posted: Sat Jul 11, 2009 6:17 am
http://apod.nasa.gov/apod/ap090711.html
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1) Are noctilucent clouds partially responsible for Volcanic modulation of summertime sub polar solar irradiation?
2) Do noctilucent clouds produce a Sunspot Cycle modulation of summertime sub polar solar irradiation?
(Note: The lack of sunspot activity in 1816 and 2009 and during the Maunder Minimum
should have resulted in more noctilucent clouds & less summertime sub polar solar irradiation.)
3) Can artificially generated noctilucent clouds be used to help reduce rampant summertime sub polar global warming?
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1) Are noctilucent clouds partially responsible for Volcanic modulation of summertime sub polar solar irradiation?
2) Do noctilucent clouds produce a Sunspot Cycle modulation of summertime sub polar solar irradiation?
(Note: The lack of sunspot activity in 1816 and 2009 and during the Maunder Minimum
should have resulted in more noctilucent clouds & less summertime sub polar solar irradiation.)
3) Can artificially generated noctilucent clouds be used to help reduce rampant summertime sub polar global warming?
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-------------------------------------http://en.wikipedia.org/wiki/Noctilucent_cloud wrote:
<<Noctilucent clouds were first observed in 1885, two years after the 1883 eruption of Krakatoa. It remains unclear whether their appearance had anything to do with the volcano, or whether their discovery was due to more people observing the spectacular sunsets caused by the volcanic debris in the atmosphere. Studies have shown that noctilucent clouds are not caused solely by volcanic activity, although dust and water vapour could be injected into the upper atmosphere by eruptions and contribute to their formation. Scientists at the time assumed the clouds were another manifestation of volcanic ash but, after the ash had settled out of the atmosphere, the noctilucent clouds persisted.
Noctilucent clouds are composed of tiny crystals of water ice 40 to 100 nanometers in diameter and exist at a height of about 76 to 85 kilometers (47 to 53 mi),higher than any other clouds in Earth's atmosphere. Much like the more familiar lower altitude clouds, the noctilucent clouds are formed from water collecting on the surface of dust particles. The sources of both the dust and the water vapour in the upper atmosphere are not known with certainty. The dust is believed to come from micrometeors, although volcanoes and dust from the troposphere are also possibilities. The moisture could be lifted through gaps in the tropopause, as well as forming from the reaction of methane with hydroxyl radicals in the stratosphere.
The exhaust from Space Shuttles, which is almost entirely water vapour, has been found to generate individual clouds. About half of the vapor is released into the thermosphere, usually at altitudes of 103 to 114 kilometers (64 to 71 mi). This exhaust can be transported to the Arctic region in little over a day, although the exact mechanism of this very high-speed transport is unknown. As the water migrates northward, it falls from the thermosphere down into the colder mesosphere, which occupies the region of the atmosphere just below. Although this mechanism is the cause of individual noctilucent clouds, it is not thought to be a major contributor to the phenomenon as a whole.
As the mesosphere contains very little moisture, approximately one hundred millionth that of air from the Sahara desert, and is extremely thin, the ice crystals can only form at temperatures below about −120 °C (−184.0 °F). This means that noctilucent clouds form predominantly during summer when, counterintuitively, the mesosphere is coldest. noctilucent clouds form mostly near the polar regions, because the mesosphere is coldest there. Clouds in the southern hemisphere are about 1 km higher up than those in the northern hemisphere.
Ultraviolet radiation from the Sun breaks water molecules apart, reducing the amount of water available to form noctilucent clouds. The radiation is known to vary cyclically with the solar cycle and satellites have been tracking the decrease in brightness of the clouds with the increase of ultraviolet radiation for the last two solar cycles. It has been found that changes in the clouds follow changes in the intensity of ultraviolet rays by about a year, but the reason for this long lag is not yet known.
Noctilucent clouds are known to exhibit high radar reflectivity, in a frequency range of 50 MHz to 1.3 GHz. This behavior is not well understood but Caltech's Prof. Paul Bellan has proposed a possible explanation: that the ice grains become coated with a thin metal film composed of sodium and iron, which makes the cloud far more reflective to radar. Sodium and iron atoms are stripped from incoming micrometeors and settle into a layer just above the altitude of noctilucent clouds, and measurements have shown that these elements are severely depleted when the clouds are present. Other experiments have demonstrated that, at the extremely cold temperatures of a noctilucent cloud, sodium vapor can rapidly be deposited onto an ice surface.>>