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This question is actually more complicated than it sounds. Water freezes at 0 degrees celcius. From 1° to 99° you'll have liquid water. So if the air temperature is 2° C you might expect liquid precipitation. But you might get a surprise when step out and see snow falling. Here's why. Precipitation falls through several thousand feet of air before you actually see it. If the air temp. near you is 2° C but the air from say above 1000 feet up to 9000 is -5° C you might get ice.
Precipitation is the solid or liquid form of water falling from clouds. Fog is a type of stratus cloud near the ground that forms when water vapor cools and condenses near the ground.
If dew point and the air temperature are the same, condensation may occur but all the given conditions guarantee is that any liquid water that might be present will be in equilibrium with the moisture in the air so any evaporation that might occur will be matched with some condensation somewhere and any condensation that might occur would have to be matched by some evaporation elsewhere.
Precipitation
At 30 0F this liquid become a solid (this is water).
This question is actually more complicated than it sounds. Water freezes at 0 degrees celcius. From 1° to 99° you'll have liquid water. So if the air temperature is 2° C you might expect liquid precipitation. But you might get a surprise when step out and see snow falling. Here's why. Precipitation falls through several thousand feet of air before you actually see it. If the air temp. near you is 2° C but the air from say above 1000 feet up to 9000 is -5° C you might get ice.
Precipitation is the solid or liquid form of water falling from clouds. Fog is a type of stratus cloud near the ground that forms when water vapor cools and condenses near the ground.
A benchmark is the minimum level of quality a product must reach. Any product falling below the benchmark is considered to be of poorer quality.
If we had no precipitation plants might not grow.
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At its outer edge, where it meets the atmosphere, the temperature of the crust of the Earth is the same temperature as the air. So, it might be as hot as 35 °C in the desert and below freezing in Antarctica.
increased precipitation
Water evaporates from the surface of the earth. It then condenses into clouds. When the water particles get too big to be held in the clouds, they fall to earth in rain. If its cold enough, they form ice crystals and it turns into snow. If they get held aloft in high winds during a thunderstorm, they might freeze into larger ice chunks called hail. Precipitation is water falling from a cloud to the earth.
If dew point and the air temperature are the same, condensation may occur but all the given conditions guarantee is that any liquid water that might be present will be in equilibrium with the moisture in the air so any evaporation that might occur will be matched with some condensation somewhere and any condensation that might occur would have to be matched by some evaporation elsewhere.
i think i might know
i guess it's united states , it also might be New York. by the way what's ur ame .
The dry bulb temperature is your average everyday straight-up temperature, the ones the weather reports discuss.The wet bulb temperature is the temperature that would be reached if exposed water were allowed to evaporate into a parcel of air until it were saturated. It's not the dew point, which is just the temperature at which the current moisture content of the air would be saturated. It measures the resulting temperature after the air loses enough heat to evaporate water until it is saturated.It is between the dry bulb and the dew point, and is useful for determining (among other things) how far the temperature might drop once precipitation starts (the precipitation will evaporate until the air is nearly saturated, using heat from the air to do so).