about the ice crystals and due point not the cold tyres
Originally posted by nsxtasy:
Moisture doesn't condense out of the atmosphere onto solid surfaces unless the humidity is close to 100 percent - whether the temperature is below freezing or above freezing
Depends how you look at it. For example: If you pull a cold bottle out of your fridge and place it in a room, moisture will condense onto the bottle regardless of the relative humidity in the room (assuming it is not 0). Reason: although the room is not at 100% "relative humidity", the air around the bottle cools down to the temperature where there is 100% saturation and droplets form on the chilled bottle. The point: for ice crystals to form on pavement, the pavement must be cold enough to lower the temperature of the air, flowing over it, to the point where it's relative humidity reaches 100% and ofcourse below freezing for ice crystals.
Originally posted by nsxtasy:
One way of determining whether humidity will condense on the ground is to look at the difference between the temperature and the dewpoint. The dewpoint is the temperature at which the humidity would be 100 percent with the then-current amount of humidity in the air. If the temperature is close to the dewpoint, then moisture will condense on the ground (as dew if it's above freezing) and, if it's below freezing, in the air as snow. If the temperature is not close to the dewpoint, then moisture won't condense.
Kinda confusing but some truth. key is the difference in temperature of the air and the surface not air and dew point and the air has to drop its temperature where it cannot hold the moisture it onced carried. Hot air has the pontential to hold more moisture. And,its relative humidity.
That said, who knows exactly all the conditions that day.
Originally posted by nsxtasy:
Moisture doesn't condense out of the atmosphere onto solid surfaces unless the humidity is close to 100 percent - whether the temperature is below freezing or above freezing
Depends how you look at it. For example: If you pull a cold bottle out of your fridge and place it in a room, moisture will condense onto the bottle regardless of the relative humidity in the room (assuming it is not 0). Reason: although the room is not at 100% "relative humidity", the air around the bottle cools down to the temperature where there is 100% saturation and droplets form on the chilled bottle. The point: for ice crystals to form on pavement, the pavement must be cold enough to lower the temperature of the air, flowing over it, to the point where it's relative humidity reaches 100% and ofcourse below freezing for ice crystals.
Originally posted by nsxtasy:
One way of determining whether humidity will condense on the ground is to look at the difference between the temperature and the dewpoint. The dewpoint is the temperature at which the humidity would be 100 percent with the then-current amount of humidity in the air. If the temperature is close to the dewpoint, then moisture will condense on the ground (as dew if it's above freezing) and, if it's below freezing, in the air as snow. If the temperature is not close to the dewpoint, then moisture won't condense.
Kinda confusing but some truth. key is the difference in temperature of the air and the surface not air and dew point and the air has to drop its temperature where it cannot hold the moisture it onced carried. Hot air has the pontential to hold more moisture. And,its relative humidity.
That said, who knows exactly all the conditions that day.