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In 1938, light pulses were used to determine the heights of clouds.
They found that on average, the heights of clouds around the world had dropped by about 1 percent over the decade ending in 2010.
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Ceilometer, device for measuring the height of cloud bases and overall cloud thickness.
At that height, shoals of clouds breeze past.
The amount of radiation emitted by the lake surface is proportional to the fourth power of the surface temperature, whereas the radiation emitted by the clouds and atmosphere overlying the lake depends primarily upon the amount and height of the clouds and the temperature and moisture content of the atmosphere near the lake surface.
A position of the upper boundary of the clouds depends on local time in such a way that the lowest height of the clouds is observed in the morning at all selected latitude ranges.
The thickening of the cloud layer, the splitting of a cloud layer, the changing height of a cloud layer are all ascribed to the presence of waves with rather long wavelengths in the cloud layer.
The ratios of hydrogen isotopes in rainfall vary according to the height of rain clouds.
For the forecast of volcanic ash by the JMA Global Atmospheric Transport Model (JMA-GATM) in the Tokyo VAAC of the JMA, the top height of ash clouds is an essential parameter.
We compare the noctilucent cloud time series, which indicate a strong upward trend in the 1964 1986 period, with changes expected of atmospheric water vapor at the mean height of the clouds (83 km).
In this case, a simulation result using realistic top and bottom height of SO2 clouds for the initial conditions of the model should be consistent with the Ash RGB images.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com