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Bellringer-Day 01 What do you think of when you hear the word “atmosphere?” What events do you think take place within the atmosphere? Do you know any layers/parts of the atmosphere? If so, what?

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Page 1: What events do you think take place within the atmosphere ...msfarrisscience.weebly.com/uploads/2/6/3/9/26394241/atmosphere_part_1.pdfBellringer-Day 01 What do you think of when you

Bellringer-Day 01

What do you think of when you hear the word

“atmosphere?”

What events do you think take place within

the atmosphere?

Do you know any layers/parts of the

atmosphere? If so, what?

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Introduction to the

Atmosphere: Structure and

Composition

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Our atmosphere

Earth’s atmosphere = the layer of gases that surround the planetVery thin layer, relative to size of planet Atmosphere:

Absorbs solar radiation

Burns up meteors

Transports and recycles water, and other chemicals

Moderates climate

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Composition of the Atmosphere

Main Components

◦ 78% nitrogen

◦ 21% oxygen

◦ 1% argon

◦ Traces of other gases:

water vapor

carbon dioxide

Methane

pollutants

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Layers of the Atmosphere

The atmosphere is divided into four layers based on temperature:1. Troposphere

2. Stratosphere

3. Mesosphere

4. Thermosphere

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As we continue…

Fill out your Layers of the Atmosphere Chart in your notes

•Be sure to include• Temperature change according to elevation

• Special characteristic of that layer

• Drawing which helps you remember the layer name with its characteristics

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The Troposphere

The bottom layer, at Earth’s surface

11 km high.

Temperature decreases with altitude.

Where weather occurs

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The Stratosphere

◦ Next layer up (11–50 km).

◦ Temperature increases with altitude.

◦ Contains “ozone layer.”

◦ Why do you think planes fly in the stratosphere?

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The Mesosphere

Third layer up

(50–90 km).

Temperature

decreases with

altitude.

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The Thermosphere

Top layer (90–500

km).

Very thin air;

mostly lightweight

elements.

Very hot.

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Atmospheric layersTemperature and other characteristics vary with altitude.

Figure 11.3

Tropopause

marks boundary

between

troposphere and

stratosphere.

Layers don’t

mix.

Ozone layer

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Ozone layer

Not really a layer (it’s part of the stratosphere), but a region of higher-than-normal ozone concentrations (which are still very low)

~17–30 km altitude

Ozone = O3—molecule of 3 oxygen atoms

Absorbs ultraviolet (UV) radiation from sun, protecting organisms on surface from radiation damage

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Exit Ticket

Create a diagram of the atmospheric layers, from the Earth up.

In each layer, write the defining characteristic of that layer

Create a pie chart that describes the amount of each atmospheric gas

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Bellringer: Day 021. What are the 4 layers of the

atmosphere, from the layer closest to Earth up?

2. Which layer is where weather occurs?

3. In which layer is the ozone layer located?

4. What does the ozone layer do? In other words, why is it important to us on Earth?

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What is Meteorology?

The study of weather, climate, and atmosphere processes

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How Does Weather

differ from Climate?

Weather is constantly changing and it refers to the state of the atmosphere at any given time and place

Climate is based on observations of weather that have been collected over many years to help describe a place or region

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Weather Vs. Climate

Weather Examples

Temperature

Pressure

Cloudiness

Humidity

Climate Examples

Seasons

Weather patterns over time/years

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First, we’re going to talk about weather.

Later, we’ll talk about climate and

climate change!

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Air Density Like most substances, cold air is more dense than warm air

Cold air will sink, hot air will rise….sound familiar??

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Air Pressure Demo!

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Pressure Systems

Low pressure –warm air rises

Poor Weather-Clouds and

precipitation

High pressure – cool air sinks and

spreads

Fair weather

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Wind is caused by the movement of air

molecules

Cool dense air sinks, forcing warm, less

dense air upward

Wind

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Global Winds

The atmosphere balances itself

by acting as a giant heat-

transferring system

It moves warm air to the poles

and cool air towards the

equator

Jet Streams –

High altitude, westerly winds

Responsible for most of our

weather in our country!

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Air Masses

Air masses are large bodies of air that take on characteristics of area they

cover (land and water)

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Four Basic Types of Air Masses

cP – Continental Polar

•dry and cool

•cold and dry in winter

and summer

cT – Continental Tropical

•dry and hot

•hot, drought-like

conditions

mT – Maritime Tropical

•wet and warm

•source of precipitation in

the United States

mP – Maritime Polar

•wet and cold

•mild, humid, unstable

cold air from Canada

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Fronts

Fronts are the

narrow regions

separating two air

masses

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Warm Front

Warm air displaces cold

air

Weather Conditions:

Light to moderate rain

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Cold Front

Cold air displaces

warm air

Weather Conditions:

Thunderstorms

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Stationary Fronts

The surface position

of the front does not

move

Do not displace

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Occluded Front

• Warm squeezed

between cold

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Can you name the fronts?

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Exit Ticket-Did the information “stick?”1. What would be the primary reason that planes fly in the stratosphere, the

second-lowest layer of the atmosphere? a) To avoid storms and other weather events b) To receive better radio communication c) To fly at supersonic speeds without air resistance d) To avoid changes in air pressure

2. The earth’s atmosphere is mainly composed of which three gases?a) Argon, nitrogen and oxygenb) Carbon dioxide, helium and nitrogenc) Argon, methane and oxygend) Helium, oxygen and radon

3. In which atmospheric layer do thunderstorms occur?a) Thermosphereb) Mesospherec) Stratosphered) troposphere

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Bellringer: Day 03

▪ Identify the states in which the fronts are

occurring. What types of fronts are they?

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Water in the Atmosphere

Precipitation is any form of water that falls from a cloud.When it comes to understanding atmospheric processes, water vapor is the most important gas in the atmosphere

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Humidityamount of water vapor in air.

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Relative Humidity

Water vapor in the

air compared to how

much water vapor

the air is capable of

holding

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Saturation

▪ The state when air contains the maximum quantity of water vapor that it can hold at any given temperature and pressure.

▪ Saturated warm air contains more water vapor than saturated cold air

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Dew PointDew point is the temperature to which air would need to be cooled to reach saturation.

http://www.youtube.com/watch?v=S8W-

xl4mcJ8

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Dew on a Spider Web

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Measuring Humidity

▪ Instrument: Hygrometer▪ Psychrometer : a type of

hygrometer consisting of two identical thermometers mounted side by side

▪ Dry bulb: give the present air temperature

▪ Wet bulb: has thin wet wick tied around the end

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Cloud Formation

▪ Condensation Nuclei – small particles in atmosphere

which water condenses around

– Millions = cloud

▪ Coalescence – droplets collide, become bigger

▪ Precipitation – droplets become too big and fall

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http://www.youtube.com/watch?v=32uFVssBs6E

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Exit Ticket-Did the information “stick?”

1. What about the cloud in the jar is similar to real cloud

formation?

2. How is relative humidity different from humidity? Why is it

that warmer seasons tend to be more humid than colder

seasons?

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Bellringer: Day 041. Explain how clouds form in 3 steps.

2. What is the difference between humidity and relative humidity? Relate relative humidity to cold vs. warm air.

3. Explain what’s happening in the morning when dew drops are forming on the grass.

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Practice: Reading Fronts

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Weather Models In reading weather data, we can find all of the following through reading a

weather model

Temperature

Dew Point

Cloud Cover

Present Weather

Wind Speed

Wind Direction

Location

Atmospheric Pressure (mb)

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Using Weather Models

Temperature

on the model

is measured

in degrees

Fahrenheit

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Using Weather ModelsCurrent weather

is represented

by any number

of symbols:

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Using Weather ModelsDew point is in

Fahrenheit

Cloud cover is

represented by the

amount of the circle

that is blacked out

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Using Weather ModelsPressure measured in

millibars- also measured

by isobars on the map

For the pressure,

remember to add the

decimal point

between the 2nd & 3rd

digit, then put a 9 or

10 in front of it. The

acceptable range of

pressures is 960mb

to 1040mb.

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Using Weather Models

Wind speed is measured

by lines

-Long lines are 10 knots

-Short lines are 5 knots

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Using Weather ModelsWind direction is

designated as the

area the wind is

blowing from!

The arrow is pointing NE,

so the wind direction is

“from the NE”

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What’s Taking Place?

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Pressure Differences Isobars

lines on a map that connect places of equal air pressure

A pressure gradient

The spacing of isobars

indicates the amount

of pressure change

over a given time

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Isobars Closely spaced isobars:

indicate a steep pressure

gradient and high winds.

Widely spaced isobars:

indicate a weak pressure

gradient and light winds.

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High and Low Pressure SystemLow Pressure Centers High Pressure Centers

Centers of Low Pressure High Pressure

AKA Cyclones Anti-cyclones

Pressure

Behavior

Pressure drops Pressure increase

Wind Behavior Winds blow

counterclockwise

Winds blow outward and

clockwise

Weather

Associated

Severe and stormy Fair and Sunny

Symbol “L” that is RED “H” that is BLUE

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What’s Taking Place?

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Seasonal Weather Why do we have different weather in different seasons?

Why do we even have the seasons? What is the cause?

Weather?

Climate?

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Bellringer-Day 05• Using the station below, answer the following:

– In what direction is the wind blowing?

– Is the wind strong or weak? How do you know?

– Is it clear, partly cloudy, or cloudy?

– What is the current temperature? And dew point?

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SEVERE STORMS

THUNDERSTORMS, TORNADOS, AND HURRICANES

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Thunderstorms• Generates lightning and thunder

• Frequently produce gusty winds, heavy rains, and hail

– 45,000 a day across the world

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• Lightning: results from the build up and discharge of electric energy between positively charged ground and negatively clouds.

• Thunder: the sound of rapidly expanding gases usually associated with lightning

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Development of Thunderstorms

• Warm, humid air rises in unstable environment

• Uplift carries warm, moist air into cooler part of atmosphere

• 3 Stages

–Cumulus Stage

–Mature Stage

–Dissipating Stage

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Thunderstorm Development• 1. Cumulus Stage-Precipitation will stay

uplifted until heavier than uplift force

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Thunderstorm Development

• 2. Mature Stage-Downdrafts throughout the cloud (cold air)

• 3.Dissapating Stage-Storm dies

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Thunderstorm Development

https://www.youtube.com/watch?v=NxWbR60tFlg

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Tornados• Take form of rotating column of air called

vortex

• Uplift turns vortex vertical

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https://www.youtube.com/watch?v=2ajShQpzBus

https://www.youtube.com/watch?v=006guBgSf14

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Tornado Intensity

• Pressure inside lower than outside

– Air rushes in to equalize pressure

– Winds may reach 480 km/h (300 mph)

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Watch vs. Warning

• Tornado Watch-The conditions are favorable for a tornado to form. People in the area should remain cautious and listen for updates.

• Tornado Warning-A tornado is imminent and has either been sighted or picked up on radar. People in the area should take cover immediately.

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When finished…

• http://cimss.ssec.wisc.edu/wxfest/Tornado/tornado.html

– Create a tornado

• http://www.nssl.noaa.gov/education/svrwx101/tornadoes/

– Read about tornados