Как известно, воздухе имеется невид

Как известно, воздухе имеется невидимый газ – водяной пар.
Поскольку при различной температуре воздуха в нём может содержаться разное количество пара (при большей температуре - большее, при меньшей - меньшее) то если имеющийся "сухой" воздух с находящемся в нём водяным паром охлаждать, то получится что при определённой температуре, пар станет насыщающим пространство! Но для достижения такого состояния температуру воздуха нужно понижать! Вот именно эта температура, при которой при понижении её значения, воздух начинает насыщаться имеющимся водяным паром, и будет называться ТОЧКОЙ РОСЫ. Это значение можно рассчитать по специальным формулам, таблицам и графику зависимости максимального количества водяного пара в зависимости от температуры. Соответственно, в обычном, "сухом" и ненасыщенном состоянии точка росы ниже температуры и поэтому конденсации не происходит, а когда температура воздуха достигает, понижаясь, значения точки росы, воздух насыщается водяным паром и происходит конденсация воды в виде капелек (при положительной температуре) или сублимация в виде кристаллов (при отрицательной) . Это и является причиной образования множества атмосферных явлений, таких как роса и иней на поверхностях, а в воздухе - туманы и облачность, атмосферные осадки, на окнах - узоры:

Результаты (английский) 1:

As you know, air has an invisible gas is water vapor. Since the air at different temperatures it may contain a different number of couple (in larger temperature-more with less-less) if available "dry" air with water vapor in it which is cool, you get that at a certain temperature, the steam will be oxygenating space! But to achieve such a State need to temperature! It is the temperature at which in its value, the air begins to become saturated with water vapour available, and will be called the DEW POINT. This value can be calculated by means of special formulas, tables, and graphics of the dependence of the maximum amount of water vapour depending on temperature. Accordingly, normal, dry and nenasyŝennom State of the dew point temperature is lower and therefore condensation will not occur, and when the air temperature reaches the dew point values falling, the air is saturated with water vapour and condensation of water in the form of droplets (when positive temperature) or sublimation in the form of crystals (if negative). This is the cause of education many atmospheric phenomena, such as dew and frost on surfaces and in the air, fogs and clouds, precipitation, on Windows-patterns:

Результаты (английский) 2:

As you know, air has an invisible gas - water vapor.
Since the different air temperature in it can contain different amounts of steam (at higher temperatures - more with less - less), then if the current "dry" air is placed in it by steam cooling, you get that at a certain temperature, the steam will be saturating the space! But to achieve such a state need to lower the temperature of the air! That's just the temperature at which its value is lowered, the air begins to saturate the available steam, and will be called the dew point. This value can be calculated according to special formulas, tables and graphics depending on the maximum amount of water vapor depending on the temperature. Accordingly, in a conventional "dry" and an unsaturated condition dew point below the temperature and therefore no condensation occurs, and when the temperature reaches, dropping, dew point, air saturated with water vapor occurs condensation of water in the form of droplets (with a positive temperature) or sublimation as crystals (negative). This is the reason for the formation of the set of atmospheric phenomena, such as dew and frost on surfaces and in the air - the fog and cloud cover, precipitation, on the windows - patterns:

Результаты (английский) 3:

as is well known, the air is the invisible gas is water vapor.as with the varying temperature it can contain different numbers of the couple (with higher temperature and more with less and less), if the dry air is cooled with the water vapor in it, that can work in a certain temperature, the steam will be насыщающим space! but to achieve such a state of the temperature should be lower. this is the temperature at which the lowering her values, the air begins to насыщаться available water vapor, and is called the dew point. this value can be calculated by the formulas, tables and the time dependence of the maximum amount of water vapour in dependence on temperature. accordingly, in the usual, "dry" and ненасыщенном state of dew point below the temperature and therefore the condensation does not occur, and when the air temperature reaches, понижаясь, meaning the dew point, the air is saturated with water vapor and condensation of water in the form of drops (with positive temperature) or sublimation, in the form of crystals (in the negative). it is responsible for the formation of multiple atmospheric phenomena, such as the dew and frost on the surfaces and in the air, mist or fog and cloud cover, precipitation, new designs: