when the temperature is decreased gas turns into ice therefore condensation happens
Condensation is a state change. Take water for example. To get liqud water to gas water, you boil it. When you boil it, you're increasing the temperature.
Now, condensation is the process from a gas state to a liquid state. It is the reverse of boiling. Therefore, instead of increasing the temperature, you decrease the temperature.
That's the role of temperature in regards to condensation.
The relationship between air temperature and its capacity to hold water vapor is governed by the principle that warmer air can hold more moisture than cooler air. As the temperature increases, the kinetic energy of air molecules rises, allowing them to accommodate more water vapor, leading to higher humidity levels. Conversely, cooler air has a lower capacity for water vapor, which can result in condensation when it reaches its saturation point. Thus, as temperature fluctuates, so does the amount of humidity the air can contain.
The correlation between temperature and humidity is typically inverse; as temperature increases, the air can hold more moisture, which can lead to lower relative humidity if the absolute moisture content doesn't increase. Conversely, when temperatures drop, the air's capacity to hold moisture decreases, which can lead to higher relative humidity if the moisture content remains constant. This relationship is crucial in weather patterns and impacts comfort levels, evaporation rates, and precipitation.
Generally, warmer temperatures can lead to increased evaporation, which can in turn lead to more moisture in the atmosphere. This increased moisture can result in more frequent or intense precipitation events, but the relationship between temperature and precipitation can be influenced by various factors, including geography and weather patterns.
The temperature determines the humidity.
The rate of condensation depends on the temperature difference between the object being cooled and the surrounding air, the humidity of the air, and the surface area and type of the object. Higher temperature differences and higher humidity levels typically result in faster condensation.
They are the same.
Condensation occurs when air reaches its dew point, which is the temperature at which air becomes saturated with moisture and can no longer hold it in gaseous form. When air cools to its dew point, water vapor in the air condenses into liquid water, forming dew or fog.
it is a relationship between moisture content & water activity in a constent temperature
People call it Rain
Humidity and temperature are closely related. As temperature increases, the air can hold more moisture, leading to higher humidity levels. Conversely, lower temperatures result in lower humidity levels as the air can hold less moisture. This relationship is important in understanding weather patterns and how our bodies perceive the environment.
Condensation can occur in any roof including insulated roof. If there is a difference in temperature between the tin roof and surrounding air (relative humidity) then condensation can occur. Relative humidity is the amount of moisture found in any measure relative to the temperature of the air. The warmer the air the more moisture it 'can' hold. With roofs if you have vented ridge or eaves it will allow air to escape and not form as condensation on the inside. Externally, moisture can form on the outside when the air reaches its dew point i.e. the air gives up the moisture it is holding when it comes into contact with cool surface.
The relationship between temperature and frequency is that as temperature increases, the frequency of a wave also increases. This is known as the temperature-frequency relationship.
The relationship between reflux temperature and distillation efficiency is that a higher reflux temperature typically leads to better separation of components in a distillation process. This is because higher reflux temperatures allow for more effective condensation and re-vaporization of the vaporized components, resulting in a purer distillate.
The relationship between air temperature and its capacity to hold water vapor is governed by the principle that warmer air can hold more moisture than cooler air. As the temperature increases, the kinetic energy of air molecules rises, allowing them to accommodate more water vapor, leading to higher humidity levels. Conversely, cooler air has a lower capacity for water vapor, which can result in condensation when it reaches its saturation point. Thus, as temperature fluctuates, so does the amount of humidity the air can contain.
humdidity and the temperature differental between the air and the surface on which the condensation collects.
The dew point is the temperature at which air becomes saturated with moisture. When the dew point is below freezing, frost can form on surfaces as the moisture in the air freezes.
When a cold can of Coke is taken out of the fridge, moisture in the air condenses on its surface due to the temperature difference between the can and the surroundings. This forms droplets of water on the can, making it wet.