Period 6, Connor and Asad, Understanding the Air and Sky Around us

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d n a r i A e

h t g n i d n a t s r e d n U s U d n u o r A y k S ll e r r a F r o n n o C d Asad Lakhani an


s t n e t n o C f o Table P. 4-11 P. 12-14 P. 15, 16 P. 17, 18 P. 19 - 23 P. 24 P. 25 P. 26

The Atmosphere Convection Currents Air Pressure Fronts Hurricanes Tornados Sun's Energy


d e u n i t n o C s t n e t n o C f o Table P. 27 P. 28 P. 29 P. 30 P. 31 P. 32 P. 33 - 36 P. 37

Weather Maps Isotherm and Isobar Precipitation Cloud Dew Point Scientist and Images Meteorological Instruments Contributions


e r e h p Atmos ● The atmosphere is like a big blanket made up of many layers ● It helps keep the Earth warm by absorbing heat and holding it in ● Protects us from the Sun's radiation with the ozone layer ● It causes weather and climate ● It is made up of many different gasses ○ 78% Nitrogen ○ 21% Oxygen ○ Small amounts of Argon, C02, Neon, Helium, Hydrogen, etc.


e r e h p s o m t A e h t f o m a r g Dia The Thermosphere is the layer of the atmosphere where the space station orbits. This is also where auras like the northern lights are.

This layer, the Mesosphere, is where rocks and meteors burn up. This is like the Earth's shield that protects us from space junk

This is the Exosphere. The Exosphere is the thinnest and outermost layer of our atmosphere.

This is the Stratosphere. This is where many planes fly, and it contains the ozone layer which protects us from harmful rays from the sun.

This is the this is Troposphere. It is where the weather is, and is the first layer above the earth


e r e h p s o p o r T ●

The Troposphere makes up about 80% of the atmosphere's mass The Troposphere is mainly heated by the Earth's surface The Troposphere is warmest closest to the Earth, and cools down from there


e r e h p s o t Stra ●

The Stratosphere is the second layer of the atmosphere The Stratosphere contains the ozone layer The Stratosphere gets warmer further up due to absorption of the sun's rays in the ozone layer


e r e h p s o s e M ●

The Mesosphere is where most meteors burn up when entering the atmosphere The Mesosphere gets warmer the further out Ice clouds form in the Mesosphere


e r e h p s o m r The ●

The Thermosphere is the second to last layer of the atmosphere The Thermosphere gets warmer further out, then stays at the same temperature The Thermosphere can reach 1,500°C or 2,700°F


e r e h p s o x

E

● The Exosphere is the outermost layer of the atmosphere ● It is mainly composed of hydrogen and helium. ● The particles are so far apart that they can travel hundreds of kilometers without colliding with one another. ● The Exosphere no longer behaves like a fluid.


s h t g n e L Layer ● The Exosphere reaches about 800 km around the earth ● The Thermosphere reaches to 410 km ● The Mesosphere reaches out to about 80 km ● The Stratosphere reaches out to 50 km ● The Troposphere reaches 12 km


n o i t c e v n o C ● Common in the atmosphere and the ocean ● Convection is an ongoing cycle made up of different things happening ● Convection makes the air rise and fall, creating clouds and rain.


r i A n o i t c Conve ● ●

First, air gets heated and raises

After this, Cool air rushes up to take the warm air's place

Finally, the warm air starts to cool down and fall

This cycle repeats endlessly

Next, the air starts to expand and become less dense


r e t a W n o Convecti

● Water starts to warm ● The warm water becomes less dense and rises up ● The cool water at the top falls down being less dense ● The movement of this water causes convection currents that continue forever


s t n e r r u C d Win â—? Wind currents are caused by differences in the temperature of the atmosphere â—? When part of the atmosphere has a lower pressure, the air from the higher pressure section moves over to the low pressure section to balance out â—? Areas with higher temperatures have high pressure. Lower temperature areas have lower pressure


s t n e r r u C Ocean ● Ocean currents are like rivers inside of an ocean ● Remember water convection from two pages ago? This same thing is what causes these ocean currents ● Currents are caused by differences in temperature, salinity, and wind.


e r u s s e r P r i A ● Have you ever been on an airplane when your ears popped? This is because of a change in air pressure ● Air pressure is how much force the atmosphere is pressing down with ● The higher you go, the lower the air pressure gets. This is why it can be harder to breathe when you're up high hiking or skiing


e r u s s e r P w o L d n a h g i H ● Low pressure usually signals that there are storms coming ● Low pressure also usually comes with warmer temperatures because when air heats up, it expands

● High pressure usually brings clear weather ● When air cools, it shrinks down and takes up less space which leads to a higher air pressure


Fronts ● There are four different types of fronts ○ ○ ○ ○

● ● ● ●

Cold Fronts Warm Fronts Stationary Fronts Occluded Fronts

Warm fronts bring warm air Cold fronts bring cool air Stationary fronts are where Occluded fronts


s t n o r F d l o C ● Forms when cold air pushes under warmer air ● Thunderheads can form when the moisture from the warm air cools and condenses ● As the front moves through an area, cool air is likely to follow it


s t n o r F m r Wa ● Forms when a moist warm air mass pushes up and over a cooler air mass ● Condenses into a wide area of clouds ● Brings gentle rain or snow followed by warmer weather


s t n o r F y r a n Statio ● Forms when cold and warm air masses meet each other but neither has enough force to move on ● Can form clouds and fog at the point where cold and warm air meet ● Capable of bringing many days of clouds and precipitation


s t n o r F d e Occlud ● Forms when a warm air mass is caught between two cold air masses ● Causes the temperature to drop ● Capable of bringing strong winds and heavy precipitation


s e n a c i r r u H ● Hurricanes form in really warm water ● In order to form a hurricane, the winds must blow in the same direction ● Hurricanes cannot form too close to the equator ● Hurricane seasons are from July 1st to November 30th and May 15th to November 30th for the Atlantic and Pacific oceans


Tornadoes ● Most tornadoes are formed from thunderstorms ● A tornado needs to have moist air from the Gulf of Mexico and dry air from Canada ● Changes in wind direction and speed with an increase in height creates a spinning in the lower atmosphere known as a tornado


y g r e n E s ' n u S ● The sun is the closest star to earth at 93 million miles away ● The sun's energy reaches earth as heat, ultraviolet light, and electromagnetic radiation ● Nearly all energy comes from the sun! ● Earth receives 1/2,000,000 of the Sun's energy


s p a M r e h t a We Fog

Occluded Front

High pressure zone

Heavy Snow

Cold Front Thunderstorm with hail

Low pressure zone

Stationary Front

Isotherm

Warm front


Isotherm ● Isotherms are lines of equal temperature regions that are drawn in on weather maps ● Pictured on the map in green and red

Isobar ● Isotherms are atmospheric pressure regions that are drawn into weather maps ● On the map in yellow


n o i t a t i p i c Pre ● Precipitation is when there is enough condensed water in the air that it can group together and fall ● Precipitation always comes from clouds ● Not all clouds always form precipitation ● There are a few different kinds of precipitation ● Rain

● Snow

● Sleet

● Hail


Clouds ● Clouds are large water droplets or ice crystals ● Clouds are made when water vapor condenses ● Four different types of clouds - Cumulus, Stratus, and Cirrus ○ Cumulus clouds are White and puffy or dark and grey ○ Stratus clouds look like a huge grey blanket ○ Cirrus clouds look like pieces of a cloud that was pulled apart


t n i o P w e D ● What is dew point? ○ Dew point is the temperature when water in the air turns into water and condenses

● What causes frost? ○ Frost is caused when the temperature of the dew point falls below 0°C (32°F)

● Does this relate to humidity? ○ Dew point is associated with relative humidity. The higher the relative humidity is, the closer to the current air temperature the dew point is


s e g a m I d n a s t s i t n e i c S ● Scientists have many different ways of getting images ● Scientists can use satellites to get images of clouds and predict weather ● Scientists can use radars to get information about precipitation and weather ● Scientists can also look at past storms and weather patterns to predict what is going to happen


s t n e m u r t s n I l a c i g o l o r o

Mete

● Scientists use many different instruments to gather information about weather. These include ○ ○ ○ ○ ○ ○

Thermometers Barometers Psychrometers Rain Guages Anemometers Wind Vanes


s r e t e m o r a B d n a s r e t e m

Thermo

● Thermometers ● Barometers measure air measure air temperature pressure ● Most thermometers ● A rising barometer are glass tubes with means sunny and alcohol or mercury dry weather ● A falling barometer means stormy, wet weather


s e g u a G n i a R d n a s r e t e Psychrom ● A Sling Psychrometer measures relative humidity by using evaporation ● A Psychrometer uses two different thermometers

● Rain gauges measure the amount of rain that has fallen over time ● Rain gauges are usually tubes that collect rainwater and have markings


s e n a V d n i W d n a s r e t e Anemom ● Anemometers measure wind speed ● Cups catch wind and turn a dial attached to the instrument ● The dial shows the wind speed

● Wind vanes determine the direction in which wind blows ● Wind vanes have a fin or some sorts that points with the wind showing wind direction


s n o i t u b i r t Con Asad ● ● ● ● ● ● ● ● ● ● ●

Covection Ocean Currents Low Pressure Hurricane Tornados Weather Map Isotherm and Isobar Clouds How Scientists get images Formatting Graphics

Connor ● ● ● ● ● ● ● ● ● ● ● ●

Title Table of Contents Atmosphere Wind Currents High Pressure Fronts Sun and Sun's Energy Types of Precipitation Dew Point Meteorological Instruments Graphics Global Patterns of Atmospheric movements


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