Atmospheric Moisture. How does the moisture get in the atmosphere?? EVAPORATION TRANSPIRATION –...
-
Upload
mae-fleming -
Category
Documents
-
view
219 -
download
4
Transcript of Atmospheric Moisture. How does the moisture get in the atmosphere?? EVAPORATION TRANSPIRATION –...
How does the moisture get in the atmosphere??
• EVAPORATION
• TRANSPIRATION – water evaporated from trees
Factors that affect evaporation rates(adding water vapor to the atmosphere)
1. Temperature – warmer the temperature, evaporation increases
2. Surface Area – As surface area increase, the rate of evaporation increases
3. Relative Humidity – as relative humidity increases, the rate of evaporation decreases
Which will evaporate faster?
4. Surface area – more surface area of water available,the more evaporation
ABSOLUTE HUMIDITY
• Amount of Water Vapor in the atmosphere• Air that is full of water vapor is said to be
saturated• The higher the temperature, the greater
the capacity of the air can “hold” water• SO, • As the air temperature increases, the air can
hold (less or more) water
Relative Humidity (RH)
Percentage of air that is saturated at a given temperature
50% RH = air has ½ the water vapor needed to saturate the air
RH = 100% means Air is saturated, it cannot add any more water vaporor condensation will occur
Dew Point
Temperature at which condensation occurs
It’s a direct measure of the moisture content in the air.
Therefore, as the dew point temp increases the amount of moisture in the air increases
Air Temp = Dew Point, then RH= 100%, which equals and occurs
• As air temperature and dew point get closer together, the probability of clouds and precipitation increases
Relationships
A. If the moisture content remains the same:
As temperature increases, RH
As temperature decreases, RH
decreases
Indirect relationship
increases
Indirect relationship
Measuring Dew Point
Instrument:
Psychrometer has 2 thermometers,
- dry bulb –
- Wet Bulb – a piece of moist cloth wrapped around the bulb
Sling Psychrometer
Air temperature
Psychrometer
• The psychrometer is swung around, the wet bulb temperature drops because of the cooling effect when being
• Wet bulb depression - difference between the dry and wet bulbs
evaporated
ESRT Page 12
• To Find Dew Point (see ESRT p. 12)• Find the wet bulb depression along the top of the chart• Find the air temperature along the left side of the chart• Where the two meet is the dew point (You may have to
estimate)
• Ex:• Dry bulb = 20°C Wet bulb = 17°C •Difference between Wet bulb and Dry Bulb =•• Dew point =
3°C
• Dry Bulb = 11 oC
• Wet Bulb = 4 oC
• Difference between wet bulb and dry bulb = ______
• Dew Point = __________
7 oC
-7 oC