100%
depends on where you live. could be moisture content in the air, or the size of your aunt
humidity
Water will begin to condense onto solid objects. These can be very small, like bits of dust or sand. Get enough of these and the result is a cloud or fog.
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Humidity is the amount of moisture in the air. Clouds are formed by condensation, which is when these water molecules in the form of water vapor condense. When it is too dense, it releases the extra water. So when humidity is high, rain clouds or fog are more likely to form.
When the relative humidity and dew point temperature are the same they form clouds.
Because it the humidity is in the cloud it makes the cloud warm so the cloud rises. So then the cloud is higher up.
depends on where you live. could be moisture content in the air, or the size of your aunt
humidity
Increase in humidity, and decrease in temperature.
No.
Base usually below 2,000 m (below 6,500 ft) but may be higher (mid-level altitude) during conditions of very low relative humidity. (tops vary)
Stuck Inside a Cloud was created in 2002.
First, warm air, heated by the surface, rises. As it rises, the temperature drops, which increases the relative humidity. Once the relative humidity passes 100%, water vapor in the air begins to condense. The formation of a cumulus cloud occurs when the water vapor condenses on various nuclei in the air. This creates the puffy cotton-like look of cumulus clouds.
Water will begin to condense onto solid objects. These can be very small, like bits of dust or sand. Get enough of these and the result is a cloud or fog.
the humidity levels in San Diego have risen drastically from their near "perfect"levels of 15-20 years ago. The relative humidity today, July1, 2013 is 84%...not perfect by any means. Thank God the sun has not come out; the mean temperature is only about 76. We'll pray for continued cloud cover...
The ground is heated up differently due to receiving different amount of insolation and air over warmer parts will rise first. Rising air expand with low pressure at high altitude. Air mass cool and relative humidity increase and saturation humidity decreases. Air force upwards, surrounding air is not as warm as rising air. When air reach dew point, water vapour starts to condense on atmospheric particles which acts as a condensation nuclei. Relative humidity reaches 100% saturation. Cloud formation continues as high as air rises. When air stop rising, cloud development stops. More uplift means the clouds will be taller and deeper. HOPE IT HELPS! :):)