Want this question answered?
Your question is meaningless, there is either an absolute logation (x/y point) or an approximate location(near the house on the corner), there can not be an "approximate absolute" location.
600
Boiling point: the temperature when a material become a gas phase.
Boiling point is the temperature at which a liquid changes into a gas. Freezing point is the temperature at which a liquid changes into a solid.
The dew point is a measure of the amount of water vapor in the atmosphere. As the temperature gets closer to the dew point, the humidity rises. When the temperature finally drops to the dew point (100% humidity), the the atmosphere is completely saturated with water, and it will start to rain (or snow, if the dew point is below freezing). Since the atmosphere is completely saturated when the temperature is at the dew point, it cannot go below the dew point.
The approximate dew point at sea level is dependent on more than just the sea level itself. Calculating dew point requires the air temperature as well as relative humidity. So in a general sense, there is no difference in dew point based on elevation if the temperature is the same.
The temperature is 286 oC.
Your question is meaningless, there is either an absolute logation (x/y point) or an approximate location(near the house on the corner), there can not be an "approximate absolute" location.
That's an approximate definition of saturation. And the temperature at which the current amount of water vapor in the air would be the saturation point is called the dew point. The dew point is a measure of absolute humidity.
An approximate answer is that 0 degrees is the temperature at which pure ice melts, and 100 degrees is the temperature at which pure water boils - both processes at standard one atmosphere. The temperature unit is one hundredth of that range. A more precise, but complicated, answer involves the absolute scale (Kelvin) and the triple point of water.
It is the approximate boiling temperature of water.
-400c
21C
6,000
85-90
If the temperature were lowered gradually enough for the substances to be in (approximate) thermal equilibrium, then nitrogen would freeze first. Nitrogen has an observed normal freezing point of 63.05 K, and oxygen has a freezing point of 54.85 K. As the temperature is lowered, nitrogen's higher freezing temperature occurs first.
The approximate height of the stratopause is between 50 to 55 km. The temperature is about negative15 degrees Celsius or 5 degrees Fahrenheit.