Weather Chp. 27
I. Atmospheric Moisture
- Phase changes of water are accompanied by a change in thermal energy of water
- Humidity- A measure of the amount of water vapor in the air
- Relative Humidity- the ratio of the amount of water vapor currently in the air at a given temperature to the largest amount of water vapor the air can contain at that temp.
- Water vapor in air
Possible water vapor at that temp
- Ex. 50% relative humidity - means the water content in the air is half the amount it could be.
- Warm air can hold more water than cold air
- As air rises it expands because of lower pressure
- Expanding air cools
- As air cools it slows down and begins to condense (water is polar)- occurs at the dew point
- As the water droplets grow they fall as rain, sleet, hail or snow -precipitation
II. Air Behavior
- Temperature changes in air is due only to pressure changes
b. Upper regions of air are warmer than lower regions leads to a temperature inversion
Ex. Denver’s smog problem
Air rises as long as it is less dense than the air above it.
III. Air Masses- (fig 27.8)
- Convectional lifting-warming air rises from “hot spots” followed by sinking cooler air
- Visualize a lava lamp
- Orographic lifting-air that is pushed up by a land mass
- Warm dry air sinks on opposite side creating a rain shadow
- Frontal lifting-(Figs. 27-11 and 27-12)
- Front- the contact zone between two air masses
- Differences in temp., moisture and pressure cause movement of air masses
- Cold front-cold into warm air mass
- Warm front-warm into cold
IV. The Atmosphere
a. Atmospheric Pressure
- Pressure exerted by air molecules because they have weight
- Decreases with increasing elevation
- Composed of primarily Nitrogen and Oxygen
- Layers of the Atmosphere
i. Thermosphere
- 90- 500 km
ii. Mesosphere
- 50-90 km
iii. Stratosphere
- 16-50 km
- contains the ozone layer
- 99% of atmosphere is below 35 km
iv. Troposphere
- 16 km at the equator
- 8 km at poles
- commercial jets fly at the top of troposphere to avoid weather
- 90% of atmosphere’s air mass
- all water vapor and clouds
V. Violent Weather
- Thunderstorms-
- Humid air rises cools and condenses
- Lightning-
- falling water droplets bump into and rub against one another
- cloud becomes electrically charged and release as lightning
- Thunder- lightning heats air up and it expands so fast it breaks the sound barrier
- Fun Facts
- ~1800 thunderstorms in progress in earth’s atmos.
- lightning strikes ~100 times every sec.
- Claims more than 200 people/ yr.
- Tornadoes-funnel cloud that has touched the ground
- Hurricanes-
- Winds up to 300 km/hr.
- Caused by a long supply of warm, moist air
VI. Clouds (table 27.1)
- High Clouds- (cirro)
- Cirrus-wispy
- Cirrostratus-sheet like
- Cirrocumulus-fish scales
- Middle Clouds- (alto)
- Altostratus-prevent shadows
- Altocumulus-long puffy strips or blotches
- Low clouds
- Stratus- gray and cover entire sky
- Statocumulus-wide gray, puffy clouds
- Nimbostratus- Cover sky, wet looking, “fog”
- Vertical Clouds
- Cumulus- pillowy
- Cumulonimbus- anvil shaped, tall clouds, produce tornadoes