Title: The Atmosphere
1The Atmosphere
2- Warm-Up Questions
- CPS Questions 1-2
3Chapter Overview
- Lesson 1 The Atmosphere
- Lesson 2 Weather Elements
- Lesson 3 Aviation Weather
- Lesson 4 Weather Forecasting
- Lesson 5 The Effects of Weather on
- Aircraft
4Lesson Overview
- The atmospheres regions
- The roles of water and particulate matter in the
atmosphere - The primary causes of atmospheric motion
- The types of clouds
- How the atmospheric layers impact flight
5Quick Write
- What are some of the advantages to
- using low-tech equipment? What are some of the
disadvantages? -
- (Note to teacher Use Pick a Student button in
CPS)
Courtesy of NOAA
6The Atmospheres Regions
- Extends more than 350 miles from Earths surface
- Life on earth is supported by atmosphere, solar
energy, and magnetic fields - Nitrogen 78 of the atmospheres gases, oxygen
21 and argon, carbon dioxide, and traces of
other gases 1
Reproduced from US Department of
Transportation/Federal Aviation Administration
7Five Distinct Layers Troposphere
- Lowest layer reaches from sea level to about
four to nine miles - Dense stretch of atmosphere where most weather
takes place - Boundary layer called tropopause traps moisture
and weather
8Stratosphere
- Above the troposphere and extends about 30 miles
- Drier and less dense than troposphere
- Temperature begins to rise again to about 26.6
- Stratopause boundary layer separates it from next
layer
Reproduced from US Department of
Transportation/Federal Aviation Administration
9Mesosphere
- Above the stratosphere to about 53 miles
- Temperatures dip as low as -135.4 F
- Chemicals exist in an excited state, they absorb
energy from sun - The boundary layer at the top is the mesopause
Courtesy of NASA
10Thermosphere Exosphere
- Thermosphere starts above the mesosphere and
extends about 350 miles - Temperature goes as high as 3,140.6 F
- Chemical reactions occur faster here than on
Earths surface - Boundary layer is the thermopause
- ExosphereStretches to the edges of space at
around 6,200 miles
11Activity 1 Atmospheric Regions
-
- Match the atmospheric region to its appropriate
place on the illustration provided - Add additional features about each region
12Roles of Water in the Atmosphere
- Evaporationtransformation of liquid to gaseous
state - Sublimationsolid changes to gas without going
through liquid state
13Roles of Water in the Atmosphere, cont.
- Condensationchange of water from gaswater
vaporto a liquid - Depositiongas changes to solid without going
through liquid state - Melting
- Freezing
Courtesy of NASA
14Evaporation
- Oceans are source of 86 of
- evaporation
- Evaporation requires heat
- Air loses heat when water changes to vapor
- Condensing water forms clouds
- Water in clouds can fall as rain, snow, some
other form - Moisture falling seeps into soil and groundwater
through infiltration
Courtesy of NOAA/Historic NWS Collection
15Sublimation
- Sublimation takes place in colder climates
- Temperatures can be too cold on a mountaintop to
melt snow and ice to liquid - Intense sunlight with strong winds can transform
snow and ice into water vapor
Courtesy of NASA/Goddard/Sarah DeWitt
16Humidity and Relative Humidity
- Humidity - amount of water in atmosphere at a
given time - Relative humidity - amount of moisture in air
compared amount of moisture the air could hold at
that temperature
17Dew Point
- Temperature at which air can hold no more
moisture - Air becomes saturated, water condenses as fog,
dew, frost, clouds, rain, hail, or snow
Courtesy of NASA/Ben Smegelsky
18Particulate Matter
- Water vapor and cloud droplets make up a cloud
- Water vapor clings to particulate matter to
condense into cloud droplets - Bits of particulate matter act as nucleusor
coreof the raindrop
Courtesy of Sean Waugh NOAA/NSSL
19- Learning Check Questions
-
- CPS Questions 3-4
20The Primary Causes of Atmospheric Motion
- Heat causes air to circulate around Earths
surface - Rising warm air and heavy, sinking cool air
results in atmospheres circular motion - Tilted axis affects atmospheric circulation
Modified from US Department of Transportation/Fede
ral Aviation Administration.
21Coriolis Force
- How Earths rotation affects the motion of air
- Deflects air to the right in Northern Hemisphere
and left in Southern Hemisphere - Breaks up flow of air into three cells at
different latitudes in each hemisphere
Reproduced from US Department of
Transportation/Federal Aviation Administration
22Activity 2 Atmospheric Motion
- Read the information in Part 1 and Part 2, and
answer the questions - Conduct the experiment outlined in Part 3
23Types of CloudsLow Clouds
- Near Earths surface up to about 6,500 feet
- Low clouds are stratus, stratocumulus,
nimbostratus, and fog - Can make visibility difficult, pilots rely on
instruments to fly through them
Courtesy of NOAA Photo Library, National Weather
Service (NWS) Collection. Photographer Ralph F.
Kresge.
24Middle Clouds
- Around 6,500 feet and reach up to about 20,000
feet - Made of water, ice crystals, and supercooled
water droplets - Middle clouds are altostratus and altocumulus
Courtesy of NOAA Photo Library, National Weather
Service (NWS) Collection. Photographer Ralph F.
Kresge.
25High Clouds
- Above 20,000 feet, usually form only in stable
air - Contain ice crystals, pose no real risk of
turbulence or icing - High clouds are cirrus, cirrostratus, and
cirrocumulus
Courtesy of NOAA Photo Library, National Weather
Service (NWS) Collection, Photographer Captain
Albert E. Theberge Jr.,
26Cumulus Clouds
- Lots of vertical development
- Flat base that forms in low or middle cloud
regions - Cumulus, particularly cumulonimbus clouds, can
mean turbulent weather ahead - Can be most dangerous cloud to encounter in
flight
Courtesy of NOAA Photo Library
27Activity 3 All About Clouds
- Name and describe some of the features of the
clouds pictured
28- Learning Check Questions
-
- CPS Questions 5-6
29Atmospheric Layers Impact FlightDensity
- Lower altitudes, density of air increases, higher
altitudes, density decreases - Air that is less dense engines and propellers
are less efficient, take in less air
Courtesy of NASA
30Pressure
- Increasing altitude affects atmospheric pressure
- Means to measure pressure is standard conditions
- Atmospheres weight at 18,000 feet is half what
it is at sea level - Regulations require cabin altitude of 8,000 feet
Reproduced from US Department of
Transportation/Federal Aviation Administration
31Temperature
- Temperatures drop dramatically with altitude
drop continues until around 36,000 feet - Airplanes have systems that regulate temperature
and heat cabins
Reproduced from US Department of
Transportation/Federal Aviation Administration
32- Learning Check Questions
-
- CPS Questions 7-8
33Activity 4 Atmospheric Factors
- Write a short paper about how aircraft today
address the effects of air density, pressure,
and/or temperature - Conduct and investigate research using the
sources identified
34Summary
- The atmospheres regions
- The roles of water and particulate matter in the
atmosphere - The primary causes of atmospheric motion
- The types of clouds
- How the atmospheric layers impact flight
35- Review Questions
-
- CPS Questions 9-10
36Next.
- Done the atmosphere
- Next weather elements
Courtesy of Robert Schwemmer/NOAA/NOS/CINMS