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Chapter 17 The Atmosphere: Structure and Temperature.

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Presentation on theme: "Chapter 17 The Atmosphere: Structure and Temperature."— Presentation transcript:

1 Chapter 17 The Atmosphere: Structure and Temperature

2 Atmosphere Characteristics Earth is the only planet in our universe with an atmosphere that is able to sustain life. The state of the atmosphere at a given time and place is known as weather. The combination of Earth’s motions and energy from the sun produce a variety of weather. Climate is based on observations of weather that have been collected over many years. –Climate helps describe a place or region.

3 Question: Which of the following is an example of climate? A.A sudden snowstorm resulted in subzero temperatures and 30cm of new snow. B.In southern California, temperatures are generally mild and rainfall is low. C.Record-breaking low temperatures caused a sudden freeze one day in Des Moines. D.A week of rain caused widespread flooding in Seattle.

4 Atmosphere Characteristics Composition of the Atmosphere Major Components –The atmosphere is a mixture of different gases and particles, each with their own physical properties, and it varies from place to place. –If all the water vapor, dust, and other variable components were removed, its makeup would be very stable up to about 80 kilometers.

5 Atmosphere Characteristics Composition of the Atmosphere Variable Components –Important materials that vary in the air (water vapor, dust, ozone, etc.), have significant effects on weather and climate. –The amount of water vapor varies from almost none to about 4% by volume. –Water vapor is the source of all clouds and precipitation. –It also absorbs heat given off by the Earth and absorbs some solar energy, therefore it plays a significant role in heating the atmosphere.

6 Atmosphere Characteristics Composition of the Atmosphere Variable Components –The dust particles include sea salts from breaking waves, fine soil blown into the air, smoke and soot from fires, pollen and microorganisms lifted by the wind, and ash and dust from volcanic eruptions. –The ozone is a form of oxygen that combines three oxygen atoms into each molecule (O 3 ). Ozone is not the same as the oxygen we breathe. –The ozone is what protects us from harmful ultraviolet radiation (UV) from the sun. If ozone did not filter most UV radiation, our planet would be uninhabitable for many living organisms.

7 Atmosphere Characteristics

8 Composition of the Atmosphere Human Influence –Humans influence the atmosphere through pollutants (i.e. emissions from cars, factories, etc.) –There are two different types of air pollutants: Primary Pollutants: Emitted directly from identifiable sources (i.e. cars, factories, etc.). Secondary Pollutants: Not emitted directly into air (i.e. acid rain, smog, etc.). –Secondary pollutants form in the atmosphere when reactions take place between primary pollutants and other substances. »Acid Rain = Primary Pollutant SO 2 reacts with Oxygen in air to produce SO 3, which then combines with water to produce sulfuric acid (H 2 SO 4 ).

9 Atmosphere Characteristics

10 Question: Most of Earth’s dry air is made up of A.Carbon dioxide and oxygen. B.Nitrogen and argon. C.Nitrogen and oxygen. D.Oxygen and argon.

11 Question: What percentage of water vapor is found in the air? A.0-1 percent B.0-4 percent C.0-8 percent D.0-10 percent

12 Question: How is ozone produced? A.One molecule of oxygen is split into two atoms. B.Two atoms of oxygen combine to form one oxygen molecule. C.Two molecules of oxygen are split simultaneously into four atoms. D.One atom of oxygen collides with the one molecule of oxygen.

13 Atmosphere Characteristics Height and Structure of the Atmosphere As the atmosphere gets higher and higher in altitude it gets thinner and thinner, until there is no more atmosphere (space). Also as the atmosphere gets higher, the pressure drops (atmospheric pressure). –Atmospheric pressure at sea level = 14.6 psi. Also as the atmosphere gets higher, the temperature drops, but this trend is not the same in all the layers of the atmosphere.

14 Atmosphere Characteristics

15 Height and Structure of the Atmosphere Temperature Changes –The atmosphere can be divided vertically into four layers based on temperature. Troposphere, Stratosphere, Mesosphere, ad Thermosphere. –The troposphere is the bottom layer where all important weather phenomena occur. On average the temperature drops as altitude rises in the troposphere. –In the stratosphere, the temperature remains constant to a height of 20 km, then it begins to increase in temperature until nearly 50 km. The increase in temperature is due to the ozone being located in this region, absorbing UV radiation.

16 Atmosphere Characteristics Height and Structure of the Atmosphere Temperature Changes –The mesosphere is the layer of the atmosphere immediately above the stratosphere and is characterized by decreasing temperatures with height. –The thermosphere is the region of the atmosphere immediately above the mesosphere and is characterized by increasing temperatures due to the absorption of very short-wave solar energy by oxygen.

17 Atmosphere Characteristics Snowy Mountaintops Contrast with Warmer Snow-Free Lowlands

18 Question: In which level of the atmosphere is ozone concentrated? A.Troposphere B.Stratosphere C.Mesosphere D.thermosphere

19 Question: In which layer of the atmosphere does our weather occur? A.Thermosphere B.Mesosphere C.Stratosphere D.Troposphere

20 Atmosphere Characteristics Earth-Sun Relationships Nearly all of the energy that drives Earth’s variable weather and climate comes from the sun. The amount of energy received varies with latitude, time of day, and season of the year. The variations in solar heating are caused by the motions of Earth relative to the sun and variations in Earth’s land and ocean surface. –Unequal heating of Earth results in wind and drives the ocean currents.

21 Atmosphere Characteristics Earth-Sun Relationships Earth has two principle motions: –Rotation: Spinning about Earth’s axis. 1 rotation of Earth takes 24 hours. –Revolution: The movement of Earth in its orbit around the sun. 1 revolution of Earth around the sun takes 1 year. Season changes occur because Earth’s position relative to the sun continually changes as it travels along its orbit. Earth is tilted at an angle of 23.5° from the perpendicular, therefore causing the change in seasons as we move around the sun.

22 Length of Daylight The length of daylight compared to the length of darkness also is determined by Earth’s position in orbit.

23 Atmosphere Characteristics Solstices & Equinoxes The four seasons we experience on Earth are Fall, Winter, Spring, and Summer. There are four important dates to remember (Northern Hemisphere): –June 21 st or 22 nd each year is known as the summer solstice (first day of summer). –December 21 st or 22 nd each year is known as the winter solstice (first day of winter). –September 22 nd or 23 rd each year is known as the autumnal equinox (first day of fall). –March 21 st or 22 nd each year is known as the spring equinox (first day of spring).

24 Question: Seasonal changes occur because of A.Earth’s tilt. B.Earth’s shape. C.The distance between Earth and the moon. D.The time of year.


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