Assuming the depth of the layer is restricted to between 1000mb and 500mb, and increasing with time, it is almost certain that the surface temperature will remain constant, thus not increasing or descreasing.
increasing temperature and increasing precipitation
The standard temperature lapse rate or environmental lapse rate as it is more commonly known is basically the temperature difference between the tropopause surface divided by height. This uses the formula -dT/dz and essentially shows the temperature decreasing as the height above the tropopause increases.
The sun!
Due to the phenomenon known as global warming, the surface temperature of the earth is increasing every year. It is warming in some areas more than others and over the last century, the temperature has increased an average of 13 degrees.
Due to the increasing temperature from morning to afternoon, causes presure gradient force (PGF) to occur.
as the temperature increase the molecular interaction between the liquids molecules are weaker, since hydrogen bond is the main factor for association between two molecules which are very weak bond, so it can be break easily when the temperature increase leading to decrease in surface tension
increasing of temperature >> increasing concentration
28 degrees on surface and gradually decreasing towards depth.
there is no effect of either
Water is condensed on a cool surface.
surface tension of water is affected by temperature as it starts to evaporate when there is hot temperature but due to unnatural medium its surface starts to freeze when the temperature outside is cold,so this gives the reason that surface tension of water is affected by temperature.
increasing temperature and increasing precipitation
Will increase the rate of dissolution and hence how fast the solute is dissolved.
it's the problem of surface area -to- volume ratio that mean there is no fitting between increasing of surface area and increasing of volume
The standard temperature lapse rate or environmental lapse rate as it is more commonly known is basically the temperature difference between the tropopause surface divided by height. This uses the formula -dT/dz and essentially shows the temperature decreasing as the height above the tropopause increases.
That's normally accomplished by raising the liquid's temperature, and sometimes decreasing the pressure on its surface, which also helps, but is not as easy to do.
as we know the relation between surface tension and temperature is inverse, and that of temperature and density also has inverse proportion, then it is clear that the '''surface tension is directly proportion to the density'''.