th.
The exhalation of water is vapour: air condensing into water is cloud. Mist is what Naisten Englanti Pelipaidat is left over when a cloud condenses into water, and is therefore rather a sign of fine weather than of rain; for mist might be called a barren cloud. So we get a circular process that follows the course of the sun. For according as the sun moves to this side or that, the moisture in this process rises or falls. We must think of it as a river flowing up Philippe Coutinho Pelipaidat and down in a circle and made up partly of air, partly of water. When the sun is near, the stream of vapour flows upwards; when it recedes, the Dortmund Børn Fodboldtrøjer stream of water flows down: and the order of sequence, at all events, in this process always remains the same. So if ‘Oceanus’ had some secret Jalkapalloseurat 2017/18 meaning in early writers, perhaps PJS Naiset Light Long Bear they may have meant this river that flows in a circle about the earth.
So the moisture is always raised by the heat and descends to the earth again when it gets cold. These processes and, in some cases, their varieties are distinguished by special names. When the water falls in small drops it is called a drizzle; when the drops Chelsea Dame are larger it is rain.
10
Some of the vapour that is formed by day does not rise high because the ratio of the fire that is raising it to the water that is being raised is small. When this cools and descends at night it is called dew and hoar-frost. When the vapour is frozen before it has condensed to water again it is hoar-frost; and this appears in winter and is commoner in cold places. It is dew when the vapour has Albania Fodboldtrøjer condensed into water and the heat is not so great as to dry up the moisture that has been raised nor the cold sufficient (owing to the warmth of the climate or season) for the vapour itself Suomi to freeze. For dew is more commonly found when the season or the place is warm, whereas the opposite, as has been said, is AS Roma the case with hoar-frost. For obviously vapour is warmer than water, having still the fire that raised it: consequently more cold is needed to freeze it.
Both dew and hoar-frost are found when the sky is clear and there is no wind. For the vapour could not be raised unless the sky were clear, and if a wind were blowing it could not condense.
The fact that hoar-frost is not found Yhdysvallat on mountains contributes to prove that these phenomena occur because the vapour does not rise high. One reason for this is that it rises from hollow and watery places, so that the heat that is raising it, bearing as it were too heavy a burden cannot lift it to a great height but soon lets it fall Albanien Fodboldtrøjer again. A second reason is that the motion of the air is more pronounced at a height, and this dissolves a gathering of this kind.
Everywhere, except in Pontus, dew is found with south winds and not with north winds. There the opposite is the case and it is found with north winds and not with south. The reason is the same as that which explains why dew is found in warm weather and not in cold. For the south Sergio Ramos Pelipaidat wind brings warm, and the north, wintry weather. For the north wind is cold and so quenches the heat of the evaporation. But in Pontus the slinks:
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