Weblesson: Atmosphere Name: _______________________ Date: _____________ Class period: ________ Student Worksheet Directions: Type in www.windows2unvierse.org in the address bar of your internet search engine. Lesson: Temperature and the Earth's Atmosphere Directions: Go to the following website and complete the data table below. http://www.windows2universe.org/earth/Atmosphere/layers.html Data Table #1 Atmospheric Layer Based on the background information, list important characteristics of each layer. Click on the blue hyperlink to find the characteristics of each layer. Troposphere First layer Contains half of the atmosphere Weather occurs here All water vapor and dust particles Low altitude, but high pressure Stratosphere Very stable Contains the ozone layer Where commercial airplanes fly Very dry, little water vapor High temperature because of ozone Mesosphere Middle layer Meteors burn up in this layer Temperature decreases as you increase altitude Contain sprites - lightning Thermosphere Contains the auroras High temperatures Very low air density Beginnings of space, space orbits Earth in this layer Exosphere Very thin Where atmosphere merges into space Directions: Refer to the graph, “The Average Temperature Profile of the Earth’s Atmosphere” found on Windows to the Universe, and complete the data tables. Data Table #2 Exists between which altitudes (km) Thickness (km) (Hint: subtract) Troposphere 0 - 10 10 Stratosphere 10 - 50 40 Atmospheric Layer Mesosphere Thermosphere 50 - 87 87 - 500 Thickness (miles) (Formula: divide by 1.61) Maximum Temperature (°C) °C x 9/5 + 32 = °F 25 - -50 - 50 - 0 0 - -100 37 413 - 100 - 1500 Ionosphere Exosphere 500 - Space Maximum Temperature (°F) Formula: 500 - 1500 Directions: Study and analyze the graph, “The Average Temperature Profile of the Earth’s Atmosphere” as you complete Table 3: Data Table #3 Atmospheric Layer Describe what happens to the temperature as altitude increases. Be sure to note specific altitudes where abrupt changes occur and how each layer is heated. Troposphere The temperature decreases with altitude Stratosphere Temperature increases abruptly at 20 km and levels off at around 47 km Mesosphere Temperature gradually decreases starting at 50 km and ending at 80 km Thermosphere Temperature increases sharply from 90 km to 100 km It increases slightly from 100 km – 110 km but increases dramatically from 110 km and up Exosphere Temperature increases dramatically starting at 500 km Analysis Questions: 1. Study the graph, "The Average Temperature Profile of the Earth's Atmosphere". Does information there help you to explain why scientists decided where one layer of atmosphere ended and the next one began? Explain your answer. The information in the graph definitely helps explain why or how scientists decided where the different layers of the atmosphere begin. The changes in temperature of the atmosphere as the altitude increases is a good indication of the different layers, and is probably what scientists used to determine where the different layers begin and end. 2. What important layer exists within the stratosphere? The ozone layer 3. What is the importance of this layer within the stratosphere? The ozone layer is important because is filters harmful ultraviolet rays (uv rays) from the Sun. Click on the blue hyperlink, stratosphere, then click on ozone and answer the questions below. 4. After reviewing the effects of both “good” and “bad” ozone, how do you think our lives would be different if the “good” ozone were destroyed? (at least three sentences). In the troposphere, you find "bad" ozone is an air pollutant that damages human health, vegetation, and many common materials. In the stratosphere, we find the "good" ozone that protects life on Earth from the harmful effects of the Sun's ultraviolet rays. If the good ozone was destroyed, there would most likely be an increase health issues for many people. Click on Does the ionosphere count as another layer? and answer the questions below. 5. What important layer exists within the thermosphere? ionosphere 6. What is the importance of this layer within the thermosphere? The ionosphere contains electrons and molecules that have gained or lost electrons that are floating around to help reflect radio waves. Different regions of the ionosphere make long distance radio communication possible by reflecting the radio waves back to Earth. 7. After reading the section, “Regions of the Ionosphere”, summarize the differences between the D, E, and F layers. Be sure to pay close attention to which wavelengths of sunlight are absorbed and which wavelengths are reflected. Does the ionosphere count as a layer different regions of the ionosphere Ionospheric Layer Characteristics F It is the highest of all of the regions. Extreme ultra-violet radiation (EUV) is absorbed there. E absorbs soft x-rays. D lowest in altitude, though it absorbs the most energetic radiation, hard x-rays 8. If the ionosphere did not exist, what do you think might be some possible consequences to humans? Think about which wavelengths the ionosphere blocks and what would happen if these wavelengths were allowed through the atmosphere to the Earth’s surface. If the ionosphere didn’t exist, satellite communication would be next to impossible. Also, many things such human health and the health of animals would be in danger because of the lack of ultra-violet radiation being absorbed. Extension Questions: 1. Give a possible explanation as to why the density of the ionosphere is greater at low latitudes (30°S to 30°N) than at high latitudes (polar regions). (HINT: Think about the effect of the Sun on the ionosphere and where on the Earth the most direct rays of sunlight are received.) 2. The density of the atmosphere decreases as altitude increases. Give a possible explanation for this relationship. 3. Give a possible explanation as to why the density of the ionosphere increases during the day or during higher solar activity. (HINT: Think about when the Sun’s effect reaches a maximum during the day and what happens during solar flares.)
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