Humidity and Clouds
Moisture
in the Air
Evaporation
·
Moisture enters the
atmosphere through the process called evaporation of water
·
Evaporation is the
process by which water molecules escape into the air
·
Evaporation uses the
sun’s energy to turn water into gas
water vapor!
·
Water vapor, or
moisture, in the air is called humidity
·
Amount of humidity
always changes
Amount depends on the temp. of air
o
more water can
evaporate into warm air then cold air
·
Relative Humidity
o
Percentage of
moisture air holds relative to the amount it can hold at a particular
temperature
§
Ex:
Can hold 12g of water vapor, only holding 9g
9/12= .75
to convert to % just x by 100
100 x .75= 75%
RH
§
Changes with temp.
and pressure
Warmer air holds more water vapor and will also have
a higher relative humidity
·
Dew Point
o
Point at which air is
saturated (100% humidity)
o
Dew happens when air
contains all water vapor possible and temp. cools so water vapor changes into
liquid when
temp. is below freezing: frost (ice crystals) can form
·
Psychrometer
o
Uses 2 thermometers,
one with cloth over bulb; other one uncovered
o
cloth is dipped in
water and the 2 thermometers are twirled
o
As air passes over
thermometers, wet cloth cools to give wet bulb temp; dry bulb temp. is given
to dry thermometer
o
To determine relative
humidity using table
§
Calculate difference
in wet and dry bulbs temp.; using difference and dry bulb temp you can find RH