Chapter 6 Notes Lesson 1 Earth’s Atmosphere



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Chapter 6 Notes

Lesson 1 Earth’s Atmosphere

The thin protective blanket of air that surrounds Earth is called the atmosphere. We couldn’t exist without it. It contains primarily nitrogen (78%) and oxygen (21%). The atmosphere protects life on Earth by:



  • Helping trap heat energy absorbed from the Sun which helps maintain the temperature range that is suitable for life.

  • Shielding Earth from dangerous levels of ultraviolet rays.

  • Reducing most meteors to dust and gas before they reach Earth’s surface.

  • Helping retain gases that most living organisms need for life (like oxygen and nitrogen).


Air has properties:

  • It takes up space.

  • It has weight.

  • It exerts pressure.


Q: What makes a balloon firmer as you blow it up?

A: Air pressure!
Air pressure changes as you go higher. There is greater air pressure closer to Earth (air particles are packed closer together) and it decreases the higher above the ground you go (air particles grow farther apart). Barometers are used to measure air pressure.
Earth’s atmosphere is divided into four layers:

1. Troposphere – (the closest one to Earth) We live in it and breath its air. Almost all weather

happens here. Here, air temperature and air pressure decrease as you go higher.

2. Stratosphere – Some planes fly here. Air is colder and dryer here. It contains most of the atmosphere’s ozone. This is where ultraviolet radiation is absorbed.

3. Mesosphere - the coldest layer of the atmosphere and where meteors burn up.

4. Thermosphere – the hot, outermost layer of the atmosphere.


A Change in Air Pressure

Q: Why do my ears pop?

A: If you've ever been to the top of a tall mountain, you may have noticed that your ears pop and you need to breathe more often than when you're at sea level. As the number of molecules of air around you decreases, the air pressure decreases. This causes your ears to pop in order to balance the pressure between the outside and inside of your ear. Since you are breathing fewer molecules of oxygen, you need to breathe faster to bring the few molecules there are into your lungs to make up for the deficit. As you climb higher, air temperature decreases. Typically, air temperatures decrease about 3.6° F per 1,000 feet of elevation.

Q: What happens to the energy from the Sun’s rays that reach the Earth?

A: Part of the sun’s energy is reflected back into space, part is absorbed by the atmosphere, and part is absorbed by the Earth’s surface (50%). Land absorbs the sun’s energy more quickly and heats up faster than bodies of water, such as lakes, rivers, and oceans. Land also releases heat and cools off faster when the sun goes down than bodies of water do.

Because the Earth’s surface is heated unevenly, the air above it is in constant motion causing changes in air pressure. This in turn causes wind to blow. Winds can be local, affecting small areas, or global, affecting large parts of the Earth. Local winds depend on local changes in temperature. Prevailing, or global, winds are caused by the sun’s uneven heating of large parts of the atmosphere and by Earth’s rotation on its axis. Prevailing winds blow constantly in the same direction. In the United States prevailing winds are from the west, so weather systems tend to move from west to east.




The Sun hits the polar regions at angles much less than 90 degrees. The energy from these rays is spread over a wider area.
The Sun hits the equator at a 90 degree angle. The energy from these rays is easily absorbed.







Air Pressure and Weather

Low-pressure systems are generally associated with stormy weather. High-pressure systems are generally associated with fair weather. Air pressure is just ONE factor used by weather forecasters to predict weather. In addition to air pressure, forecasters also use humidity; wind speed and direction; and air temperature.
Lesson 2 Moving Air

Because the Earth’s surface is heated unevenly, the air above it is in constant motion causing changes in air pressure. This in turn causes wind to blow. So the SUN is the source of energy that drives the winds. Winds usually blow faster at higher altitudes (no trees, mountains, or tall buildings to slow the winds down). Also, winds blow faster over smooth oceans than hilly lands. Remember convection currents from the last chapter? We talked about warm air rising and cold air falling in the water cycle. We also talked about the loops of convections currents in the ocean. Well, guess what? Winds are also examples of convection currents!


Q: What are local winds?

A: Mountain breezes and valley breezes are examples of local winds.
In areas where there are mountains and valleys we see a type of wind pattern known as mountain breezes and valley breezes.



Valley Breeze Mountain Breeze
Valley Breeze Explained: During the day, the surface of the mountain heats the air high up in the atmosphere, quicker than the valley floor can. As the warmer air expands a low pressure is created near the top of the mountain. This attracts the air from the valley, creating a breeze that blows from the valley floor up towards the top of the mountain. Often birds known as raptors such as eagles, hawks, condors, and vultures float on these breezes to preserve their energy. This wind pattern is known as a valley breeze.
Mountain Breeze Explained: In the evening, the mountain slopes cool the surrounding air more quickly than the air found lower in the atmosphere. This creates a high pressure as air becomes more densely packed. The resulting high pressure causes winds to blow down the mountain towards the valley floor. This type of wind pattern is known as a mountain breeze.
Thus, in the daytime we typically see valley breezes, as winds blow from the valley up towards the mountains. In the night we often see mountain breezes, as winds travel from the mountains, down towards the valleys. The cycle of mountain and valley breezes is strongest during the summer, when skies are clear.

Sea Breeze Explained: During the day, land gets heated by the Sun much quicker than water. As the land becomes warmer, it heats the air in the atmosphere above it. This causes the air to expand, becoming less dense, and thus creating a low pressure. Because water heats up much less quickly, air above the ocean also takes longer to increase in temperature. The result is that a higher pressure is maintained. With a high pressure above the water, and a lower pressure above the land, conditions are perfect for a small breeze to develop. Wind blows from the sea, towards the land along the pressure gradient, in an attempt to equalize pressure. This is known as a sea breeze.
Land Breeze Explained: In the night, land cools down much quicker than does the waters of the ocean. As the land becomes cooler, so does the air above it. This results in air becoming more dense, forming a high pressure, causing winds to blow outward towards the sea. This is known as a land breeze.

LAND BREEZE



Sea Breeze and Land Breeze

Thus, in the day we often see sea breezes, while in the evening we see land breezes in coastal regions.




Mountain Effect



Windward Side Leeward Side
Windward Side of the Mountain Explained: Mountains make a barrier for moving air. The wind pushes air and water vapor up the mountain slope. Recall that at higher elevations, temperatures are colder and water vapor condenses to form clouds. As the cloud continues to rise, droplets grow and grow, eventually becoming too heavy to float in the air. The clouds dump rain, and/or snow, on ONE side of the mountain slope called the windward side. Some of the wettest places on Earth are on the windward sides of mountains. The windward side of the mountain faces the ocean.

Leeward Side of the Mountain Explained: After topping the crest of the mountain, however, the clouds may have no more moisture to deliver on the other side of the mountain (leeward side), which then becomes arid. The leeward side of the mountain receives very little or no precipitation. These dry areas on the leeward mountain slopes are called rain shadows.

Example: This rain shadow is best illustrated in the Sierra Nevada Mountains of California, where tall redwood forests cover the ocean-facing side of the mountains (windward side) and Death Valley lies in the rain shadow (leeward side).

Q: What are the global wind patterns?
A: The equator receives the Sun's direct rays. Here, air is heated and rises, leaving low pressure areas behind. Moving to about thirty degrees north and south of the equator, the warm air from the equator begins to cool and sink. Between thirty degrees latitude and the equator, most of the cooling sinking air moves back to the equator. The rest of the air flows toward the poles.

Q: What is the jet stream?
The jet stream is a fast flowing, river of air found in the upper troposphere. Winds in these narrow belts can blow as fast as 149 mph. They form at the boundaries of adjacent air masses with significant differences in temperature, such as of the polar region and the warmer air to the south. Because of the effect of the Earth's rotation the streams flow west to east, moving in a snake-like or wave-like manner at lower speeds than that of the actual wind within the flow. Jet streams “steer” weather systems from place to place, affecting both their speed and direction.

Jet Stream (moving like a snake)





Lesson 3 Predicting Weather

As we said, most of Earth’s weather takes place in the troposphere, the lowest layer of the atmosphere. Weather conditions such as temperature, air pressure, humidity, wind speed and direction, and the amount of precipitation can be observed and measured. Warm air weighs less than cold air. Weather changes because high and low pressure areas move. Changing air pressure, meaning that a different air mass is moving into the area, can be used to predict weather.


Instrument used Weather condition measured

1) Thermometer Measures air temperature

2) Barometer Measures air pressure

3) Rain gauge Measures precipitation

4) Wind vane Measures wind direction

5) Anemometer Measures wind speed


Q: What is an air mass?

A: An air mass is a large body of air that has temperature and moisture similar to that of the

area (land or water) over which it formed. Air masses can cover thousands of kilometers. They



form over continents and oceans. Moist air masses form over water. Air masses that form over land are generally dry. Air masses that form near Earth’s poles are cold. Air masses that form in the tropics, or areas near the equator, are warm. When two air masses meet, they usually don’t mix but form a front. Fronts are the areas where most weather happens. When a front stops moving it is called a stationary front.
Types of air masses that affect North America

  • mP-Maritime Polar. This is very cold air that resided over a cold body of water for some time, allowing it to also be moist.




  • cP-Continental Polar. This is a very frigid air mass that originates over land and thus is dry. It often forms over landmasses covered in snow.




  • cT-Continental Tropical. This air mass is a very warm air mass, but is dry due to it forming over land.




  • mT-Maritime Tropical. This is a very warm, very moist air mass.



Q: How do meteorologists forecast the weather?
A: Weather forecasting is a prediction of what the weather will be like in an hour, tomorrow, or next week. Weather forecasting involves a combination of computer models, observations, and a knowledge of trends and patterns. By using these methods, reasonable accurate forecasts can be made up to seven days in advance.

Q: What are weather station symbols? (EXTRA INFORMATION )
A: Weather symbols are used on my weather maps as shorthand for the conditions at weather observing stations.


Q: What is a High Pressure System?
A: A high pressure system is a whirling mass of cool, dry air that generally brings fair weather and light winds. When viewed from above, winds spiral out of a high-pressure center in a clockwise rotation in the Northern Hemisphere. These bring sunny skies. A high pressure system is represented as a big, blue H.
H

Q: What is a Low Pressure System?
A: A low pressure system is a whirling mass of warm, moist air that generally brings stormy weather with strong winds. When viewed from above, winds spiral into a low-pressure center in a counterclockwise rotation in the Northern Hemisphere. A low pressure system is represented as a big, red L.
L

Q: What is a front?
A: A front is a boundary between two different air masses, resulting in stormy weather. A front usually is a line of separation between warm and cold air masses.

Q: What is a cold front?
A: A cold front is a boundary between two air masses, one cold and the other warm, moving so that the colder air replaces the warmer air. A cold front is represented as a blue line with the teeth pointing toward the direction on movement.


Q: What is a warm front?
A: A warm front is a boundary between two air masses, one cool and the other warm, moving so that the warmer air replaces the cooler air. A warm front is represented as a red line with half circles pointing toward the direction on movement.









Compare warm and cold air fronts

Q: What is a stationary front?
A: A stationary front is a boundary between two air masses that more or less doesn’t move, but some stationary fronts can wobble back and forth for several hundred miles a day. A stationary front is represented as an alternating warm and cold front symbol.


Q: What is a weather satellite?
A: A weather satellite is a type of satellite that is primarily used to monitor the weather and climate of the Earth. Satellites can be either polar orbiting, seeing the same path of the Earth every 12 hours, or geostationary, hovering over the same spot on Earth by orbiting over the equator while moving at the speed of the Earth's rotation. These meteorological satellites see more than clouds and cloud systems. City lights, fires, effects of pollution, auroras, sand and dust storms, snow cover, ice mapping, boundaries of ocean currents, energy flows, etc., are other types of environmental information collected using weather satellites.


Q: What is radar?
A: Radar is an electronic instrument, which determines the direction and distance of objects that reflect radio energy back to the radar site. It stands for Radio Detection and Ranging. This is what meteorologists use to see rain or snow.


Q: What is Doppler Radar?
A: Doppler Radar detects precipitation intensity, wind direction and speed, and provides estimates of hail size and rainfall amounts. Doppler Radar gives forecasters the capability of providing early detection of severe thunderstorms that may bring strong damaging winds, large hail, heavy rain, and possibly tornadoes. Combined with satellites, radar gives forecasters the ultimate tools to provide accurate forecasts and advanced severe weather warnings.

Q: How does Doppler Radar work?
A: Doppler Radar gets its name from the Doppler Effect. Have you ever listened to a train whistle as it was coming toward you? You probably noticed that the pitch of the whistle changed as the train passed you and moved away. This change in the frequency of sound is called the Doppler Effect. Doppler Radar measures the changes in the frequency of the signal it receives to determine the wind.


Q: What is NEXRAD Radar?
A: The National Weather Service has installed a new type of Doppler Radar called NEXRAD Radar. NEXRAD stands for Next Generation Radar. This radar produces many different views of storms and rain that allows meteorologists to determine if a storm could be severe.


Lesson 4 Severe Weather

Severe storms are associated with low pressure systems. In these systems, warm, moist air rises and cools. Water vapor in the cooling air condenses, forming clouds followed by precipitation.


Q: What is a thunderstorm?
A: A thunderstorm is a storm with lightning and thunder. It’s produced by a cumulonimbus cloud, usually producing gusty winds, heavy rain and sometimes hail.


Q: What causes a thunderstorm?
A: The basic ingredients used to make a thunderstorm are moisture, unstable air and lift. You need moisture to form clouds and rain. You need unstable air that is relatively warm and can rise rapidly. Finally, you need lift. This can form from fronts, sea breezes or mountains.

Q: Are thunderstorms dangerous?
A: Yes, despite their small size, all thunderstorms are dangerous. Every thunderstorm produces lightning, which kills more people each year than tornadoes.


Q: What is lightning?
A: Lightning is a bright flash of electricity produced by a thunderstorm. All thunderstorms produce lightning and are very dangerous. If you hear the sound of thunder, then you are in danger from lightning.



Q: What causes lightning?
A: Lightning is an electric current. Within a thundercloud way up in the sky, many small bits of ice (frozen raindrops) bump into each other as they move around in the air. All of those collisions create an electric charge. After a while, the whole cloud fills up with electrical charges. The positive charges or protons form at the top of the cloud and the negative charges or electrons form at the bottom of the cloud. Since opposites attract, that causes a positive charge to build up on the ground beneath the cloud. The grounds electrical charge concentrates around anything that sticks up, such as mountains, people, or single trees. The charge coming up from these points eventually connects with a charge reaching down from the clouds and - zap - lightning strikes!

Have you ever rubbed your feet across carpet and then touched a metal door handle? If so, then you know that you can get shocked! Lightning works in the same way.


Q: What causes thunder? (EXTRA INFORMATION )
A: Thunder is caused by lightning. When a lightning bolt travels from the cloud to the ground it actually opens up a little hole in the air, called a channel. Once then light is gone the air collapses back in and creates a sound wave that we hear as thunder. The reason we see lightning before we hear thunder is because light travels faster than sound!

Q: How do you know if lightning is nearby? (EXTRA INFORMATION )
A: If you see dark clouds, then lightning could be present, but the best thing you can do is to listen for thunder. If you hear thunder, then you need to go indoors or get in a car. Don't be outside, where lightning could strike! If your hair stands on end or your skin starts to tingle, lightning maybe about to strike. Get down on your hands and knees and keep your head tucked in. Do not lay flat, because it can give lightning a better chance of strike you.


Q: How far away can you see lightning and hear thunder? (EXTRA INFORMATION )
A: Within those distant thunderstorms, the lightning bolts can be seen as much as 100 miles from us, depending on the height of the bolt, the clarity of the air, and our elevation. Thunder, in comparison, has a much shorter range of detection - usually less than 15 miles in a quiet rural setting and under 5 miles in a noisy city environment.

Q: Can you tell how far away a storm is? (EXTRA INFORMATION )
A: Yes, you can use thunder to tell how far away a storm is. Next time you see a storm, count the number of seconds between when you see the lightning and hear the thunder. Take the number of seconds and divide by 5 and that will tell you how far away the storm is in miles. For example: If you counted 10 seconds between the lightning and the thunder, the lightning is 2 miles away!


Q: What is hail? (REVIEW)
A: Hail is created when small water droplets are caught in the updraft of a thunderstorm. These water droplets are lifted higher and higher into the sky until they freeze into ice. Once they become heavy, they will start to fall. If the smaller hailstones get caught in the updraft again, they will get more water on them and get lifted higher in the sky and get bigger. Once they get lifted again, they freeze and fall. This happens over and over again until the hailstone is too heavy and then falls to the ground.



Q: What is the largest hailstone recorded in the United States? (EXTRA INFORMATION )
A: According to the National Weather Service, the largest hailstone is 8 inches in diameter and weights approximately 2 pounds. It fell in Vivian, South Dakota on July 23, 2010.


Q: What causes the wind to blow?
A: As the sun warms the Earth's surface, the atmosphere warms too. Some parts of the Earth receive direct rays from the sun all year and are always warm. Other places receive indirect rays, so the climate is colder. Warm air, which weighs less than cold air, rises. Then cool air moves in and replaces the rising warm air. This movement of air is what makes the wind blow.

Q: What is a tornado?
A: A tornado is a violent rotating column of air extending from a thunderstorm to the ground. The most violent tornadoes are capable of tremendous destruction with wind speeds of up to 300 mph. They can destroy large buildings, uproot trees and hurl vehicles hundreds of yards. They can also drive straw into trees. Damage paths can be in excess of one mile wide to 50 miles long. In an average year, 1000 tornadoes are reported nationwide.

Q: How do tornadoes form?
A: Most tornadoes form from thunderstorms. You need warm, moist air from the Gulf of Mexico and cool, dry air from Canada. When these two air masses meet, they create instability in the atmosphere. A change in wind direction and an increase in wind speed with increasing height creates an invisible, horizontal spinning effect in the lower atmosphere. Rising air within the updraft tilts the rotating air from horizontal to vertical. An area of rotation, 2-6 miles wide, now extends through much of the storm. Most strong and violent tornadoes form within this area of strong rotation.











Q: What is a funnel cloud?
A: A funnel cloud is a rotating cone-shaped column of air extending downward from the base of a thunderstorm, but not touching the ground. When it reaches the ground it is called a tornado.
 
 
Q: How do tornadoes stop? (EXTRA INFORMATION)
A: It is not fully understood about how exactly tornadoes form, grow and die. Tornado researchers are still trying to solve the tornado puzzle, but for every piece that seems to fit they often uncover new pieces that need to be studied.
 
Q: What is a super cell thunderstorm? (EXTRA INFORMATION)
A: A super cell thunderstorm is a long-lived thunderstorm whose updrafts and downdrafts are in near balance. These storms have the greatest tendency to produce tornadoes that stay on the ground for long periods of time. Super cell thunderstorms can produce violent tornadoes with winds exceeding 200 mph.

Q: What is a waterspout? (EXTRA INFORMATION)
A: A waterspout is just a weak tornado that forms over water. They are most common along the Gulf Coast. Waterspouts can sometimes move inland, becoming tornadoes causing damage and injuries.


Q: When are tornadoes most likely to occur?
A: Tornadoes can happen at any time of the year and at any time of the day. In the southern states, peak tornado season is from March through May. Peak times for tornadoes in the northern states are during the summer. A few southern states have a second peak time for tornado outbreaks in the fall. Tornadoes are most likely to occur between 3 p.m. and 9 p.m.

Q: Where are tornadoes most likely to occur?
A: The geography of the central part of the United States, known as the Great Plains, is suited to bring all of the ingredients together to forms tornadoes. More than 500 tornadoes typically occur in this area every year and is why it is commonly known as "Tornado Alley".


Fujita Scale of Tornado Intensity (FYI ONLY)

SCALE

WIND SPEED

POSSIBLE DAMAGE

Enhanced,
Operational
Fujita Scale

F0

 40-72 mph

Light damage: Branches broken off trees; minor roof damage

EFO
65-85 mph

F1

73-112 mph

Moderate damage: Trees snapped; mobile home pushed off foundations; roofs damaged

EF1
86-110 mph

F2

113-157 mph

Considerable damage: Mobile homes demolished; trees uprooted; strong built homes unroofed

EF2
111-135 mph

F3

158-206 mph

Severe damage: Trains overturned; cars lifted off the ground; strong built homes have outside walls blown away

EF3
136-165 mph

F4

207-260 mph

Devastating damage: Houses leveled leaving piles of debris; cars thrown 300 yards or more in the air

EF4
166-200 mph

F5

261-318 mph

Incredible damage: Strongly built homes completely blown away; automobile-sized missiles generated

EF5
over 200 mph


Q: What is a flood?
A: A flood results from days of heavy rain and/or melting snows, when rivers rise and go over their banks.

Q: What is a flash flood?
A: A flash flood is sudden flooding that occurs when floodwaters rise rapidly with no warning within several hours of an intense rain. They often occur after intense rainfall from slow moving thunderstorms. In narrow canyons and valleys, floodwaters flow faster than on flatter ground and can be quite destructive.

Q: Do flash floods hurt people? (FYI ONLY)
A: Flash floods are the #1 weather-related killer in the U.S. Nearly 80% of flash flood deaths are auto related. Know beforehand if your area is a flood risk.


Q: How much water is needed for your car to float away? (FYI ONLY)
A: A mere 2 feet of water can float a large vehicle or even a bus. This is why you should never drive through flooded roads. Just 6 inches of rapidly moving flood water can knock a person down.
Q: What is the opposite of an extreme flood?

A: A drought! Droughts are associated with high pressure systems and a longer than normal period of time with below-normal rainfall. Droughts can kill crops, and drain away water reserves.

Q: How do blizzards form?
A: A blizzard is a long-lasting snowstorm with very strong winds and intense snowfall. You need three things to have a blizzard; cold air at the surface, lots of moisture, and lift. Warm air must rise over cold air. Blizzards form from low pressure systems. In the United States, blizzards occur in areas that experience cold winters such as the Northeast, the Great Plains, and mountainous regions, such as the Sierra Nevada region in California.

Blizzards can strand cars on highways for hours or even days. When you are traveling during the winter months, be sure to have an emergency car kit in the vehicle with you.


Q: What is a hurricane?
A hurricane is the most powerful storm on Earth! It begins as a low pressure system over warm, tropical waters. It can be up to 930 miles across and have strong winds spiraling inward and upward at speeds of 75 to 200 mph. Each hurricane usually lasts for over a week, moving 10-20 miles per hour over the open ocean. Hurricanes gather heat and energy through contact with warm ocean waters. Evaporation from the seawater increases their power. Hurricanes rotate in a counter-clockwise direction around an "eye." The center of the storm or "eye" is the calmest part. It has only light winds and fair weather. When they come onto land, the heavy rain, strong winds and large waves can damage buildings, trees and cars.


Q: How do hurricanes form?
A: Hurricanes only form over really warm ocean water of 80°F or warmer. The atmosphere (the air) must cool off very quickly the higher you go. Also, the wind must be blowing in the same direction and at the same speed to force air upward from the ocean surface. Winds flow outward above the storm allowing the air below to rise. Hurricanes typically form between 5 to 15 degrees latitude north and south of the equator.


Q: When does hurricane season start? (FYI ONLY)
A: The Atlantic hurricane season is from June 1 to November 30, but most hurricanes occur during the fall months. The Eastern Pacific hurricane season is from May 15 to November 30. (Below is a graphic that shows you when hurricanes are most active across parts of the world.)



Q: Who names hurricanes? (FYI ONLY)
A: From 1950 to 1952, tropical cyclones of the North Atlantic Ocean were identified by the phonetic alphabet (Able-Baker-Charlie-etc.), but in 1953 the US Weather Bureau switched to women's names. The rest of the world eventually caught on, and naming rights now go by the World Meteorological Organization, which uses different sets of names depending on the part of the world the storm is in. Around the U.S., only women's names were used until 1979, when it was decided that they should alternate a list that included men's names too. There's 6 different name lists that alternate each year. If a hurricane does significant damage, its name is retired and replaced with another.

Q: What is the difference between a hurricane and a typhoon? (FYI ONLY)
A: Nothing except geography. Tropical storms occur in several of the world's oceans, and except for their names, they are essentially the same type of storm. In the Atlantic Ocean, Gulf of Mexico, and the Eastern Pacific Ocean, they are called hurricanes. In the Western Pacific Ocean, they are called typhoons. In the Indian Ocean, the Bay of Bengal, and Australia, these types of storms are called cyclones.


Q: Who are the "Hurricane Hunters"? (FYI ONLY)
A: The brave "hurricane hunters" work for the National Oceanic and Atmospheric Administration (NOAA). Each mission lasts about ten hours, with the crews passing four to six times through the storm. The planes carry radar, sophisticated computers, and weather instruments that determine characteristics such as temperature, air pressure, wind speed, and wind direction inside the hurricane. The crews also release instruments that measure temperature, air pressure, and wind at different levels as the devices drop through the hurricane toward the ocean. By mission's end, NOAA can warn everyone in the hurricane's path.







Saffir-Simpson Hurricane Scale

Category

Winds (MPH)

Pressure (Millibars)

 Pressure (Inches)

Storm Surge
(Feet)

Damage

1

74-95

<980

<28.94

4'-5'

Minimal

2

96-110

979-965

28.91-28.50

6'-8'

Moderate

3

111-130

964-945

28.47-27.91

9'-12'

Extensive

4

131-155

944-920

27.88-27.17

13'-18'

Extreme

5

>155

<920

<27.17

>18'

Catastrophic


You do not need to memorize this scale. You should know, for example, that a category 3 hurricane is stronger than a category 1 hurricane and that a category 5 hurricane is the most severe.


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