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average width of 20 feet may be loaded down with five tons of ice. Visibility in the air improves following a rainfall because precipitation has a cleansing effect on the air. Water droplets in the air form around condensation nuclei, tiny particles of dust and debris. When precipitation falls, it removes these particles from the air. Eventually the cloud and air temperatures become equal. The cloud isn’t buoyant at this point and begins to spread out. This creates the classic anvil‐shaped tops that are seen at cloud tops. The temperature at which water vapor condenses into liquid water is called the dew point. If the dew point is below 0°C, it is called the frost point. These are important numbers in helping to determine where to post frost and freeze warnings. The dew‐point temperature is found in a similar manner to that of relative humidity. The dry‐bulb and wet‐bulb temperatures are determined. The wet‐bulb Amazing book lover do not disturb all over printed tote bag in the air can be measured in different ways. The specific humidity of air is a measure of how much water is in the air. Warmer air can hold more water than colder air. When the air reaches its capacity, it is saturated. This capacity doubles for about every 11°C
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