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Chapter 8 Objectives: Geography 12 Worksheet 8.7 Key 8.7 Climatic Controls: Altitude Read pages 152 – 153 of Planet Earth: A Physical Geography. Answer the following questions: Vocabulary (1 mark each) /17 Environmental Lapse Rate: The rate at which air temperatures decrease with altitude. In stable air, the lapse rate is 6.4 C per 1000 meters. Sensible Heat Flux: The movement of heat in the atmosphere by convection currents in the air. Short Answer (2 marks each) 1. Since solar radiation does not convert into heat until it is absorbed by a body, how does the atmosphere heat up? Understand the relationship between weather and climate Understand important terms that are associated with the study of climate Appreciate the importance of classifying climatic conditions in various ways Recognize that the climatic patterns on earth are complex and that they result from a wide variety of interacting forces which include the earth’s basic motions, the earth’s surface features, and the arrangement of the earth’s land masses and water bodies Identify the importance of the sun in powering climatic systems Appreciate that our understanding of climate and weather is still developing and that many theories have yet to be proven to be true Appreciate the extreme variability and complexity of the earth’s climates Examine ways that humans both influence and are influenced by climate an weather The land heats up and warms the atmosphere from below by radiating longwave radiation to the atmosphere. Heat is distributed upwards to the atmosphere by warm convection currents of air generated at the surface…called sensible heat flux. 2. Why is the air warmer at lower elevations than at higher elevations? (1 mark) At lower elevations the air is more dense and contains more molecules of air, water vapor, dust, pollen etc than it does at higher elevations. Atmosphere at sea level is able to absorb more solar radiation and longwave radiation. 3. How high must a mountain at the equator be in order to have snow year round if the average maximum temperature in the hot month is 31C? 4900 m (use the spreadsheet) 4. Graph the temperatures in the following chart to illustrate the influence altitude has on temperature. (10 marks) Station Latitude Altitude Above Sea Level (m) Average Annual Daily Maximum Temperature (C) Average Annual Daily Minimum Temperature (C) Guayaquil, Ecuador Pandang, Indonesia Douala, Cameroon Mogadishu, Somalia Manaus, Brazil Kisangani, Zaire Kisumu, Kenya Rubona, Rwanda Kabale, Uganda Quito, Ecuador 2S 6 31 20 0 7 31 23 4N 8 29 23 2N 12 30 24 3S 0 44 418 32 30 24 20 0 2S 1148 1706 28 25 18 14 1S 0 1871 2879 23 22 10 8 3500 30 3000 25 2500 20 Altitude 2000 15 1500 10 1000 5 500 0 G ua y Pa aq u nd il, E a Do ng, cua d u I M ala nd o or og , n a d Ca es ish me ia u r M , S oon an o Ki a u mal ia sa s, n g Br Ki an az su i, il Ru mu Za bo , K ire e n Ka a , ny R ba w a a l Q e , U nd a ui to ga , E nd cu a ad or 0 Altitude Place Guayaquil, Ecuador 6 Pandang, Indonesia Douala, Cameroon Mogadishu, Somalia Manaus, Brazil Kisangani, Zaire Kisumu, Kenya Rubona, Rwanda 7 8 12 44 418 1148 1706 Kabale, Uganda Quito, Ecuador 1871 2879 Average Daily Temperature Max 25.5 27 26 27 28 25 23 31 20 31 29 30 32 30 28 25 23 23 24 24 20 18 14 23 22 10 8 19.5 16.5 15 Min Average Daily Temperature