The aim of our studies was to examine turbulent, wavy structures innoctilucentclouds taking into account the clouds dusty plasma nature.
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However, the dusty plasma nature ofnoctilucentclouds has been neglected.
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A specific feature observed innoctilucentclouds is wavy, turbulent structure.
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However, although being an interesting point by itself, we emphasize that our simulations are not sufficiently appropriate regarding the vertical dynamics innoctilucentclouds.
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Thus, our simulations offer new insight into the dynamics ofnoctilucentclouds.
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The occurrence ofnoctilucentclouds appears to be increasing in frequency, brightness and extent.
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The possibility that small particles left behind on the orbital pathalmost one hundred days after the nucleus has passedcould formnoctilucentclouds is also slim.
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Noctilucentclouds may be confused with cirrus clouds, but appear sharper under magnification.
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Noctilucentclouds may be seen by observers at a latitude of 50 to 65.
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The connecting of global warming andnoctilucentclouds however, remains controversial.
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At still higher altitudes up in the mesospere,noctilucentclouds made of ice crystals are sometimes seen in polar regions in the summer.
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The clouds thus generated are intended to simulate naturally occurring phenomena callednoctilucentclouds, which are the highest clouds in the atmosphere.
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Noctilucentclouds are not fully understood and are a recently discovered meteorological phenomenon; there is no record of their observation before 1885.
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The characteristic blue colour comes from absorption by ozone in the path of the sunlight illuminating thenoctilucentcloud.
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There is also evidence that smoke particles from burnt-up meteors provide much of the condensation nuclei required for the formation ofnoctilucentcloud.
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